t Digitized by the Internet Archive in 2016 https://archive.org/details/influenceofbluerOOplea Sketch of Gen. A. J. Pleasonton’s Grapery, in the 24th Ward of the City of Philadelphia, displaying the arrangement of the Blue and Transparent Glasses THE INFLUENCE OF THE Blue Eat of the Sunlight AMD OF THE BLUE COLOUR OF THE SKY, IN DEVELOPING ANIMAL AND VEGETABLE LIFE ; IN ARRESTING DISEASE, AND IN RESTORING HEALTH IN ACUTE AND CHROJHC DISORDERS TO HUMAN AND DOMESTIC ANIMALS, AS ILLUSTRATED BY THE EXPEBI2IEMT3 OF GEN. A. J. PLEASONTON, AND OTHERS. Between the years i86i and i8j6. AJtefflJ to llie Pladslsliia Society fir ProMiii AAiiciiltaie. “ Error may he tolerated, •what reason is left free to combat it." — Thomas yeffersott. “ If this theory he true, it upsets all other theories." — Richmond Whig. PHILADELPHIA: CT.AXTON, KEMSEN & HAFFELFINGER, PUBLISHERS. - 1876. '1 -" i.- -v^^^.'i^'''-.-i '.j y '1 fv Entered accqrding to Act. of Congress in the year 1876, _^By gen. AUGUSTUS J. PLEASONTON, In the Office of the Librarian of Congress, at Washington, D. C. P’l ■? PREFACE. TTating been much interested in the phenomena of the physics of the earth, llio aiit'iui., in offering to liis readers a second edition of his work, “Oh the luriueiic6. ,ee the Blue Color of the Sky in Developing Animal and Vegetable Life,” may be indulged in his introduction into this preface of some views that his observations have led him to entertain relative to the variations .of tempera- ture, and changes of our seasons, wliich are in harmony with the subjects treated by him in this work. The first edition of the following memoir was printed for distribution among scientific and literary institutions, and among persons of culture, for the purpose of attracting the attention of those for whom it was intended, to the subjects of which it treats. It was hoped that its publication would invite investigaiion into the nature, composition, and influences of those great forces which, in the poverty of our language, we call imponderables, that is to say, not to be w"cighed in the balance, and consequently never to be found wanting. This expectation is likely to be realized, if we may judge from the general interest that appears to be taken in the memoir, w'hich has been manifested in the. numerous apirlications that have been made to the author, from various parts of our country, for copies, of it. The edition has now been distributed, yet .so many persons who liave applied for copies of the memoir are still without it, that it has been deemed advisable to issue another edition. If, by a course of study, and observation of the great forces of nature, as they are exliibited, not in the laboratory, upon the minutest scale, but in those grand operations by which physical changes are at every moment developed before our eyes, we can succeed in penetrating the mysteries of their origin, of their evolution, of their application, and of their reciprocal conversions into each other, we shall become indeed wise in our generation, and mankind in the future will be able to rejoice in a development never yet reached in any pre- ceding age. J>y \vny of illustration of this idea, we may suggest that this planet is surrouudeii, at variable altitudes above its surface, by a canopy of cold, increas- ing in jhtensity with its distance above the earth. 'Kow, w'e may ask, what produces the changes of our seasons? We answer, simply the descent or ascent of columns of tliis canopy of cold 1 It has been observed, for any years, that the first frost of the autumn appears in Texas or Louisiana, or some othef of the Gulf States, while at :h.- same time no frost is observable in other localities situated much farther to the north— the commonly supposed place of departure of our winters. This frost, therefore, must come from the descent of the cold of the higher atmosphere immediately over the locality where it prevails. Following the valley of the Mississippi and those of its tributaries, frost appears successively in various idaces along those routes, till it reaches the vallies of the Northern Lakes, running along which it is felt in Northern New York and the NewJEngland States, and subsequently in the Middle and Southern Atlantic States. It does, not reach the vicinity of Philadelphia until some fifteen or twenty days after it has shown itself on the Gulf of Mexico. Now would it not seem that the influences producing this frost are telluric; and not exclusively solar, as hitlierto they have been supposed to he '* • V We know that in the ocean there are columns of fresh water which differ in temperature from the. surrounding sea water, and with which they do not mingle for a long time. So is it for a himdred or more miles at sea, distant from the mouths of the great rivers Amazon, Orinoco, Mississippi, etc., whose fresh waters do not mix w'ith the salt waters surrounding them, owing to the difference of their densities. In like manner the cold air of the. tipper atmosphere descends in columns of various extent over particular localities, to vary the temperature and change the seasons, on the surface of our earth, without mixing with the warmer and more expanded air beneath, which it displaces. • The spring and summer seasons arc produced by increased radiations from tlie interior heat of the earth, forcing upwards the dense cold of winter, whose particles are so close together as to prevent the intrusion among them of tbe e^panded warm air in its ascent. ■ Much of the heat of the lower atmospliere is also developcxl in the conversion of vapor into clouds by condensation from cold. It is in this way that our seasons arc changed. Let our savans discover how and why tlicse effects are produced. Until they do, it may be. suggested that they arc owing to electrical atmospherical disturbances in the upper atmos- phere, repelling the negative electricity of those regions, and forcing the cold iii air to the surface of the earth, where it displaces the warnier and nrore rarehed and expanded air, and condenses in rain, snow and hail, the vapors it contains, driving tlie displaced g amier air totlvo tropics, and the heat from the. tropics attracted to the cohdensed vapor in the clouds in the temperate zones to liquefy them in rain, producing winter. ' :r Tn the opposite manner the warm seasons of spring and summer are pro- duced hy the positive elcclricity of the suxfaee-air .of the earth becoming wai .ued by increased radiation of heat from the interior of the earth, repelling itself, and displacing the upper strata of cold ah, till by induction of electricity the temperature of the season is established. • ■ f . . geologists tell us that in the early existence of this planet, the greater part f)f tlve earth’s surface was covered with ice, and that this period of time is Cidled the G-lacial Period. ' Let us imagine that the igneous action, of the elementary substances of the interior of the earth’s ermst, just before that period, might have been so iidense as by the radiation of its heat to the surface of the earth to rarefy the lower _ atmosphere, converting into vapor the water it contained, and forcing it upward till the whole surface of the eartH was almost incandescent. To restore' the equilibrium, the canopy of cold repelled by its own negative electricity from above, whiclr has been increased by the currents of polar elec- . trikty, largely dcyeldped by this central and interior igi^ous action— and attracted by the positive electricity in the heated atmosphere below— descended to the surface of the earth, condcsi.sing the vapors of- the atmosphere into rain, and afterwards into hail and snow, driving the remainder of the warmer air at what wo call, now, the temperate zones, to the tropics,'" and covering the' surfaces of the earth, from the poles to the tropics, with a dense mantle of ice, freezing the rivei-s, hays, iTnd seas of those latitudes. -The internal central fires "thus eoncerdTated, in due season increased their radiation of heat, and melted the .superjacent ice, whidx, breaking from- the' sides of glaciers in large masses, - slid aiid rolled to the. ocean, there becounng'lcshergs, and carrying- with them 'those immense boulders ■which, iorn from the mountain sides by the adhesion • of the ice, have left the traces of their furrows on the slopes of the mountains, and have marked their courses till, by the melting of the bergs, they have been dropped in the ocean, which subsequently, by its subsidence, have left them dry on the land. If such was the cause of the glacial period, it would rc,quire no grout stretch of fancy to coniprehcnd tlie deluge of Deucalion or that of our great ancestor; iN'oah, wiien tlie rain descended for forty days ; occasioned no doubt by a lessCr descent of the canopy of cold (limiting its . effect to the condensation of five vapors of the atmosphere into rain) than that vvliich produced tire glacial lauioiL' If such effects follow from ,sueh causes, wfe need not be at a loss to account • for the changes of our seasons, or the daily variations of temperature in every locality. This edition of our memoir has been printed upon tinted paper with blue ■ ink, as an experiment, in an attempt to relieve the eyes of the reader from the. great glare, occasioned by the reflection of gas light at night from the white paper usually employed in ' the juinting of hooks. If it '.shall succeed we may hope to see the tinted paper introiiuced for all books and periodicals. rmLADELPHIA, July 29, 1871. " i. PREFACE TO THE LAST EDITION. r In the previous editions of my memoir “ On the Influence of the Blue Colour of the Sky in Developing Animal and Yegetahle Life,” an erroneous, imjjres- Sion has been created by the ambiguity of - the language Employed in describing the- results of my experiments -with light. From the tints reflected from the outside of the coloured glass, upon centain localities in my terraced garden, I fancied that the glass itself -was of ayiolet tint, and so attributed the remarkable results -within the grape^ to violet rays. Upon my attention having been called to this apparent discrepancy, I investigated the matter, and found that the glass -was of a dark mazarine blue — o-sving its colour to a preparation of cobalt, \vhlch had been fused -with the materials composing the glass during its manu- fueturo— and* hat the reflection of the violet ray on the outside -was due to the irregular surface of the glass itself upon -which the light of the firmament, as well as of the sunlight had fallen, and had been thus reflected. Wliatever effect may he produced by the use of violet coloured glass is to be attributed to. the ■ proportion of the blue ray which enters into the composition of the -violet rays of light, and not to those composite raj’s themselves. This edition, begun in the summer of the year 1373, has been prepared at intervals snatched from the occupations of a busy life, which will account for any incoherences that may appear in the subject? as they are treated herein. Tlie following memoir was read by Gen, A. J. Pleasonton. before tbe Pbiladelpbia Society tor Promoting Agriculture, on Wediiesday, tbe 3d of May, 1871, at their room, S. W. corner ot 9th and "Walnut Streets, in the City ot Philadelphia, upon the following recpiest ; 1309 Walnxtt St., mii, 1871. Mk Dear General: Will it suit you, and will you do us the favor to explain your process of using glass in improving stock to the' Philadelphia So- ciety for Promoting Agriculture, on Wednesday next, the 3d of May, at eleven o’clock, A.M., at their Eoom, S. W. corner of Ninth and Walnut Streets, (entrance on Ninth street) ?■ You were kind enough to express to me. in conversation, j'our willingness to give u.s, the result of your experiments. ■ Yours, very truly, W. H. DEAYTON, President General Pleasonton. Ifr. President and Gentlemen of The Philadelphia Society for Promoting Agriculture. At the request of my old friend'and yoiir respected Presi- dent, I have attended your meeting this morning to impart to you tlie results of certain experiments that I have mjide within the last ten years in attempts to utilize the blue color of the sky in the development of vegetable and animal life. I may prernise that for a long time I have thought that the blue color of the sky, so permane!-' and so alKpervading- and yet so varying in intensity of color, according to season and latitude, must have some abiding relation and intimate con- nection with the living organisms on this planet. Deeply impressed with this idea, in the autumn of the year 1800, 1 commenced the erection of a cold grapery on my farm in the western part of this city. I remembered that while a student of chemistry I was taught that in the analysis of the ray of the sun by the prism, in the year 1666, by Sir Isaac New- ton, he had resolved it into the seven primary rays, viz : red, orange, yellow, green, blue, indigo and violet, and had disco- vered that these elementary rays had different indices of refrac- tion ; that for the red ray at one side of the solar spectrum being the least, while that of the violet at the opposite side thex'eof was the greatest, from which he deduced his celebrated doctrine of the different refrangibility of the rays of light and further, that- Sir John Herschel in his subsequent investigation of the pro- perties of light had shown that- the cherin^l power of the solar ray is greatest in the blue rays, which give the least light of any of the Imiinoiis prismatic radiations, but the largest quantity of so- lar heat,^ and that later experiments established the fact of the stimulating influence of the blue rays upon vegetation. Haviuo- - concluded to make a practical application of"the properties of the blue and violet rays of light just refeiTed to in stimulating ve- getable life, I began to inquire in.every accessible direction if this stimulating quality of the blue or violet ray had ever re- ceived any practical useful application. My inquiries developed the facts that various experiments had been made in England and on the European continent with glass colored with eimh of c the several primary rays, hut that they wore so iinshiishietory ill their results tliat nothiiia; useful came cf Uiem so far as auy iin}ir()vemeiit in the process of devehapiriy’ ve/rcia.iion was con- cerned. Finding no beaten track, I was left to grop-'. iny way as best I ci)uld under the guidance of the violet ras* alone. My grapery was finished in ]\Iarch, 1861. Its dimensions were, 84 feet long, 26 feet wide, 16 feet higirat the ridge, with a dou- ble-pitc.heil roof. It was built at the foot of a tet raced .garden, in the direction of H. E. 1)y E. to S. W. by W. On three sides of it there was a border 12 feet wide, .and on the fourth or N. E. by E, side the border was only five feet wide, bcirig a walk of the garden. The borders inside and outside were excavaicd 3 feet 6 inches deep, and w'oro fillcfl up with the usual nutritive jnat- tcr, carefully'proparcd for growing vines. I do not think they diffcrc(l ossenliail}'- from thousand.^ of other borders wbieh have been made in man.y parts of the world. The first ques- , tion to be solved on the completion of the frame of the grapery, was the proportion of blue or violet glass to he used on the z’oof. Shuuld too much he used, it would reduce the temperature 'too much, and cause a foilure of the experiment; if too little, it would not afford a fair test. At a venture I adopted every eighth row of glas.s on the roof to he violet colored, alternating the rows oti opposite .sides of the roof, so that the sun in its duilj'- course should cast a beam of violet light on every leaf in the grapeiy. Cuttings of ^■inc8 of some twenty variciies of grapes, each one year old, of the thickness of a ])ipe-stem, and cut close to the pots containing them, were planted in the borders inside and outside of the grapery, in. the. early part of April, 1801. Soon after being planted thg growth of- the vines began. Those on the outside were trained through earthen pipes in the walls to the inside,, and as they grew they were tied up to the wires like_ those wliich had been planted within. A^ery soon the vines began to at- tract great notice of all who saw them, from the rapid growth they Avere making. ' Every day disclosed some new extension, and the gardener was kept busy in tying up the new wood which the day before he had not observed. In a few Aveeks after tbe vines had been planted, the walls and inside of the roof were closely cov'ered Avith the most luxurious-and healthy development of foliage and Avood. In the early part of September, 1861, Mr. Eobert Buist, Sr., a noted seedsman and distinguished horticulturist from whom I had procured, the vines, haAung heard of their Avonderful growth, visited the grapery. * On entering it he seemed to be' t lost in amazement at "wliat he saw; after examining it very care- fully? tiirning to me, he said, “ General! I have been cultivating plants and vines of various kinds for the last forty years; I have seen some of the best vineries and conservatories in England and Scotland, but I have never seen anything like this growth.”’ He then measured some of the vines and found them forty- five feet in length, and an inch in diameter at the distance of one foot above the ground ; and these dimensions were the growth of only five months I He then . remarked, “I visited last week a new grapery near Darby, the vines in which I fur- nished at the same time I did- yours ; they were of the same varieties, of like age and size, when they were planted as yours ; they were planted at the same time with yours. When I saw them last week, they were puny spindling plants not more than five feet long, and scarcely increased in diameter since ■ they were planted — and yet they have had the best possible care and attendance ! ” The vines continued healthy and to grow, making an abun- dance of young wood during the remainder of the season of 1861. In March of 1862 they were started to grow, having been pi'uned and cleaned in January of that year. The growth in this second season was, if anything, more remarkable than it had been in the previous year. Besides the formation of new wood and the display of the most luxuiriant foliage, there was a wonderful number of bunches of grapes, which soon assumed the most remarkable proportions — the bunches being of extra- ordinary magnitude, and the grapes of unusual siz"e and de- velopment. In September of 1862 the same gentleman Mr, EobertBuist, Sr,, WHO had visited the grapery the year before came again — this time accompa nied by his foreman. The grapes were then beginni ng to color and to ripen rapidly. On entering the grapery, astonished at the wonderful display of foliage and fruit which it presented, he stood for a while in silent amazement; he then slowly walked around the grapery several times, critically ex- amining its wonders ; when taking from his pocket paper and pencil, he noted on the paper each bunch of grapes, and esti- mated its weight, after which aggregating the whole, he came to me and said, “ General ! do you know that you have 1200 pounds of grapes in this grapery ?” On my saying that I had no idea of the quantity it contained, he continued, “ you have indeed that weight of fruit, but I would not dare to publish it, for no 8 one ‘.voiild believe me.” "We well conceive of bis astnn- isbmont at this product wlicn we are reminded that iii grape- groving countrio,s where grapes have been grown for centu- ries. that a period of time of from tive to six years will elapse ‘before a single bunch of grapes can be produced from a young vine — while before him in the second year of the growth of' wnes wbich he himself had furnished only seventeen mouths before, he saw this remarkable yield of the finest and clioicest varieties of grapes. He might well say that an account of it would be incredible. During the next season (1863) the vines again fruited and matured a crop of grapes estimated by compai'ison with the yield of the previous year to weigh about two tons ; the vines were yjerfectly healthy and -free from the usual maladies which affect the grape. By this time the grapery and its products had become partially known among cultivators, who said that such excessive crops would exhaust the vines, and that the follovring year there would be no fruit, as it was well known that all plants required I’est after yielding large crops ; notwith- standing, new wood was formed this year for the next year’s crop, which turned out to be quite as large as it had been in the season of 1863, and so on year by year the vines have con- tinued to bear large ci'ops of fine fruit without iutcriuission- for the last nine years. They are now healthy and strong, and as yet show no signs of decrepitude or exhaustion; The success of the grapery induced me to make an experi- ment with animal life. In the autumn of 1869 I built a pig- gery and inti’oduced into the roof and three sides of it violet- colored and white glass in equal proportions — half of each kind. Separating a recent litter of Chester county pigs into two parties, I placed three sows and one barrow pig in the ordinary pen, and three other sows and one other barrow pig in the- pen under the violet glass. The pigs w'ere all about two months old. The weight of the pigs was as follows, viz : Under the violet glass, No. 1 sow, 42 lbs.. No. 2, a barrow pig, 45J lbs,, No, 3, a sow, 38 lbs., No. 4, a sow 42, lbs., their ag- gregate weight 167-J lbs. The weight of the others in the common pen was as follows, viz No. 1,, a sow, 60 lbs., No. 2, a sow, 48 lbs.. No. 3, a barrow big, 59 lbs.. No. 4, a sow, 46 lbs ; their aggregate weight was 203 lbs. ' It will be observed that each of the pigs under the violet glass was lighter in weight than the lightest in weight pig of those under the sun- light alone in the common pen. The two sets of pigs were treated exactly alike ; fed with the same kinds of food at 9 eq^ual intervals of time, and vritli equal quantities by measure at each meal, and. were attended by the same man. They were put in the pens on the 3d day of November, 1869, and kept there until the 4th day of March, 1870, when they were weighed again. By some misconception of my orders, the separate weight of each pig was not had. The aggregate weight of the three sows under the violet light on the 8d of November, 1869, was 122 lbs; on the 4th of March, 1870, it was 520 lbs., increasc^98 lbs. The aggregate weight of the three sows in the old pens , on the 3d of November, 1869, was 144 lbs,, and on the 4th of March, 1870, it was 530 lbs., increase 386 lbs., or 12 lbs. less than those under the violet glass had gained. The weight of thq barrow pig in the common pen on the 3d of November, 1869, was 59 lbs., and on the 4th of March, 1870, it was 210 lbs., increase 151 lbs. The weight of the barrow pig under the violet light, on the 3d of November, 1869, was 45 J lbs., and on the 4th of March, 1870, it was 170 lbs., increase 124| lbs. The large increase of the weight of the barrow pig in the common pen is to be attributed to his superior size and weight on being put in the same common pen with the three sows, and which enabled him to seize upon and appropriate to himself moi;e than his share of the com.- mon food. If the barrow pig under the violet light had increased at the rate of increase of the barrow pig in the common pen, his weight on the 4th March, 1870, would have been only Ihlfyl, Ibs.^^instead of his actual weight of 170 lbs. — showing his fate of increase of weight to have been 8i«, lbs. more than that of the other barrow pig. If the barrow pig under the sunshine in the common pen had increased at the rate of increase of the barrow pig under the violet glass, his weight on the 4th.of March, 1870, should have been 224/(^ lbs. instead of 210 lbs., his- actual weight at that date. . By these comparisons it seems obvious that the influence of tlie violet-colored glass was very marked, although it must be borne in mind that 6wing to the great declination of the sun during the period of the experiment and the consequent com- parative feebleness of the force of the actinic . or chemical rays of the blue sky at that time, the effect was not so great as it would have been at a later period of the season ; but the time 10 ■- 1 ‘ the experiment was selected for that very reason. The t;viimals were not fed to produce fat or increase of size, but ^■mply to ascertain, if practicable, whether by the ordinary nmde of feeding usual on farms, in this country, the develop- ment of stock could be hastened by exposing them in pens to t'iie combined influence of sunlight and the transmitted rays of the blue sky. My next experiment was with an Alderney bull calf born on 'he 26th "f January, 1870 ; at its birth it was so puny and fee- ]>le that the man Avho attends upon my stock, a very expe- rienced hand, told me that it could not live. I directed him to put it in one of the pens under the violet glass. It was done. In 24 hours a very sensible change had occurred in the animal. It had arisen on its feet, walked about the pen, took its food freely by the finger, and manifested great vivacity. In a few days its feeble condition had entirely disappeared. It began to grow, and its development was marvelous. On the 31st March, 1870, 2 months and 5 days after its birth, its rapid growth was so apparent, that as its hind quarter was then growing, I told my eon to measure its height, and to note down in writing the height of the hind quarter, and the time of measurement — whi.ch he did. On the 20th of the follow- ing May (1870), just fifty days aftei’wards, my son again mea- sured the hind quarter, and found that in that time it had gained exactly six inches in height, carrying its lateral development with it. Believing the question solved, the calf was turned into the barn-yard, and when mingling with the cows he manifested every symptom of full masculine vigor, though at the time he was only four months old. Since the 1st of April of this year, when he was just 14 months old, he has been kept with my lierd of cows, and has fulfilled every expectation that I had formed of him. He is now one of the best developed animals that can be found any where. These, gentlemen, are the experiments about which your curiosity has been excited. If by the combination of sunlight and blue light from the sky, you can mature quadrupeds in twelve months with no greater supply of food than would be used for an immature animal in the same period, you can scarcely conceive of the immeasurable value of this discovery to an agricultural people. You would no longer have to wait five years for the maturity of a colt ; and all your animals could be produced in the greatest abundance and variety. A prominent member of the bar a short time since told me that bis sister, who is a widow of a late distinguished general in 11 the army, had applied blue light to the rearing of poultry, with the most remarkable success, after having heard of my experiments. In regard to the human family, its influence would be wide spread — ^}'ou could not only in the temperate regions produce the early maturity of the tropics, but you could invigorate the constitutions of invalids, and develop in the young, a- generation, physically and intellectually, which might become a marvel to rnankind. Architects would be requii'ed to so arrange the introduction of these mixed rays of light into our houses, that the occupants might derive the greatest benefit from their influence. Mankind will then not only be able to live fast, but they can live well and also live long. Let us attempt an explanation of this phenomenon. It is well known that differences of temperature evolve electricity*, as do also evaporation, pressure suddenly produced or suddenly removed, in ydiich may be comprised a blow or stroke, as, for instance, from the horseshoe in the rapid motion of a horse on a stone in the pavement, striking fire, which is kindled by the electricity evolved in the impact, or, again, from the collision of two silicious stones in which there is no iron, is electricity produced. ^ Friction even of two pieces of dried wood excites combus- tion by the evolution of hydrogen gas which bursts into flame when brought into contact with the opposite electricity evolved by the heat. Chiystallization, the freezing of water, the melting of ice or snow — every act of combination in respira- tion, every movement and contraction of organic tissues, and, indeed, every change in the form of matter evolve electricity, which in turn contributes to form new modifications of the matter which has yielded it. The diamond, about whose origin so much mystery has always existed, it is likely, is the product of the decomposition of carbonic acid gas in the higher atmosphere by electricity, libei’ating the oxygen gas, converting it into ozone, fusing the carbon, and by the intense cold there prevailing, which is of opposite electricity, chrystallizing the 'fused carbon, which is precipitated by its gravity to the earth. To the repellent affinity of electricity are we indebted for the expansive force of steam whose power wields the mighty trip hammer, propels the ship through the ocean, and draws the train nver the land — and to the opposite electricities of the heated steam and the cold water introduced into the boiler to repleuisli it, do we owe those terri])le explosions in steam boilers whose prevention has hitherto, defied human skill. But the most interesting application of electricity, is in nature’s development of vegetation. Let us illustrate it : Seed perfectly dried, hut still retaining the vital principle, like the seed of wheat preserved for thoupnds of years in mummy cases in the catacoinbs of Egypt, it planted in a soil of the richest alluvial deposits, also thoroughly dried, will not germinate. Why? Let us examine. The alluvial soil is composed of the deJrYs of hills and mountains containing an extensive variety of metallic and metalloid compomids min- gled with the remains of vegetable and animal matter in a state of great comminution, washed by the rains and carried by freshets into the depressions of the surface of the earth, 'lihese various elements of the' soil have dilferent electrical attributes. • In a perfectly dry state no electrical action will occur amo-ng them, hut let the rain, bringing with it ammonia and carbonic acid, in however minute quantities, froin the upper atmosphere, fall upon this alluvial soil, so as to moisten its mass within the influeiice of light, heat, and air, and plant your seed within it, and what will you observe ? Rapid germi- nation of the seed. W^hy ? The slightly acidulated, or it may be alkaline water of the rain has formed the medium to excite galvanic currents of electricity in the heterogeneous matter of the alluvial soil— the vitality of the seed is developed and vegetable life is the result. Hence vegetable life owes its existence to electricity. Herein consists the secret of success- ful agriculture. If you can maintain the currents of electri- city at the roots of plants by suppl};ing the acidulated- or alkaline moisture to excite them during droughts, you will secure the most abundant and unvarying crops.^ To do this, your soil should be composed of the most varied elements, mineral, earthy, alkaline, vegetable, and animal matter in a state of greatly comminuted decomposition. The poverty of soils arises from the homogeneous character of their composition. A soil altogether clayey, or coniposcd of silicious sand, or the debris of limestone, or of alkaline sub- stances exclusively, must necessarily be barren for the want of electrical excitement, which no one of the said elements will produce ; but commingle them all with the addition of decomposed vegetable and animal matter, and you will form a soil which will amply reward the toil of the husbandman. What do you suppose has produced the giant trees of Cali- 13 fornia? Electricity! Since tlie west coast of America has been known to Europeans, and perhaps for centuries be- fore, it has been subjected to the most devastating earth- quakes. From the Straits of Magellan to the Arctic Ocean, traces of volcanic action are .everywhere visible. Its mounl'dns have been upheaved, broken, torn asunder, and someti mes, like Ossa upon Pelion, one has been superimposed on another. All volcanic countries are noted in the temperate regions, where they produce anything, for the exuberance of their vegetable productions. Etna has been famous for its large Chest- n,xi trees, which have given a name Catania to the to-wn near irs luise. The ij'noral richness of California has doubtless, by the debris its mountains, carried into the valleys where grow these h.i’ge trees, furni.shed an immense deposite of various matter which,- under the favorable circumstances of the locali- ties, In r . maintained for ages a healthful electrical excitement resulr-'g dii-ough centuries of undisturbed growth in these vegetu!;ia wonders. Who is there that has not been struck with admiration in looking rpon the firmament, when the atmosphere was clear- est, was unclouded by the slightest vapor, — ^Avhen, in the brig' of sunlight, it would put on its livery of blue, and dispiry its resplendent and glorious beauties? How many myris ds of mankind, in all ages, have gazed upon this mag- nificent arch, of what men call “sky;” and howfe-\y havi - ever asked tbe question, Why is the sky blue? aiid why should its intensity of blue vary in different latitudes, and in difierent seasor.is? Hl said he had never seen its blue so intense as in tlie tr(.‘pio 3 and under the equator. Arctic navigators have also declared, that in the arctic regions the intensity of the blue color 01 the sky was amazing. Here are two extremes of lati- tude 'lisplaying the same effect; and in our own temperate re- gion many have observed a variation in the intensity of the blue of the sky, in different seasons, extending from the early spring until the close of autunni, but never equaling in depth of color what is represented of it, eithei in the tropics or in the ai’ctic or antarctic regions. On no part of our planet is the development of vegetable life so grand, so various, 80.e.vcessive and so constant as in the 14 tropics and in the eqnatorif/l r'fegious. "Wliile this wonderful display of vegetation is observed in these regions, the exuber- ance of animal life and the rapid growth of vegetable life m the arctic regions are said to be unequaled, in any other part of our world. Let us see if these results in the two natural kingdoms may not be attributed largely to the same cause. Recent discoveries have shown that the Zodiacal light over the equator and the aurorre borealis and australis arb evolu- tions of electricity. In the arctic i-egions there is little doubt that the auroras are constantly evolved, though they are not txlwciys visible. Tbey li£ive been seen to emeigo iioru tlie sur- face of the ocean, at short distances from the observers, and ascending into the upper regions of the atmosphere, to present those corruscations of brilliant light, shooting as it were to the equatorial regions, in rapid flashes, for which they have been noted wherever observed. In the equatorial regions it is well known that af certain periods of the year the accumulation of efectricity in the upper atmosphere'i's so excessive, 'that the earth is shaken with thun- derbolts, and the air illuminated by day as well as night with constant shoots- of electric flame, as they rush vith trighttul velocity to their great .ceutre ot attraction, the eaith and ocean in those regions. ^V'h^nce does this electi-icity come, and where does it go? If we may be' permitted to form a conjectuie, we might simgest that the sixty odd primary elements which enter into the composition of the crust of our planet such as carbon, sulphur, phosphorus, oxygen, nitrogen, hydrogen, the metals, the- metalloids, etc. — ^having been endowed by the Creator with different electrical qualities and conditions — when they were assembled together in this planet, evolved in the interior there- of electricity, light, heat, and magnetism in certain or variable qualities and quantities. These constitute the forces winch in all probability cause the rotation of the earth upon its axis, and assist in its revolution around the sun. The electricity of the interior of the earth is supposed to be positive electricity which, as soon as evolved there, would be repelled according to the law of electricity of the same character repelling itself —towards the poles of the earth, and escaping there, would be attracted by the negative electricity which surrounds the upper atmosphere, and would display itself by night as aurorae, coiTUScating toward the equator, to be there attiacted by t ® heated equatorial regions, and descending to the earth, to be 15 again_ absorbed by it, for further use. This escape of polar electricity into the upper atmosphere, and forming at night the aurorje, when visible, and by day the blue firmament or sky, will account for the intensity of the blue color of the sky both in the arctic regions and the equatorial regions. This positive electricity of the central interior of the earth, repelling itself towards the poles, and from there into the at- mosphere through the arctic and antarctic oceans, and attracted there by the negative electricity of the upper atmosphere, forms, by the union of the two electricities, the auroras, caus- ing those crackling detonations heard during the prevalence of the most brilliant auroras, in high latitudes and evolving light, which, seen through the vaporous atmosphere of those latitudes, is displayed by refractions of its rays in the lumin- ous corruscations of varying tints as the rays of the sun or moon are converted into the tints of the rainbow. The negative electricity of those frigid regions attracted to the equator through the upper atmos^phere is there concen- ti’ated in. enormous quantities, which are conducted and dis- charged into the earth or ocean in the tropics, by the incessant fall of water in rain during the rainy seasons, every .drop of water being a conductor of electricity, and every leaf of veo-e- tation assisting in the conduct and distribution of this wonder- ful force into the earth. As under certain circumstances electricity becomes magnet- ism, and this again is converted into electricity, we can com- prehend how the auroral rays in some instances, followin'? the law of dia-magnetism, are attracted in the northern hemisphere towards the southwest — magnetic currents flowing from east to west in opposition to the earth’s motion from west to east; hence in the auroras you have rays shooting to the zenith over the equator, and others moving southwest, and others again due west. The simultaneous appearance of. auroras frequently observed in opposite hemispheres in corresponding latitudes would go to show their origin from a common impulse in the central in- terior repelling them towards the poles from under the equator. TV" e now come to a presumed explanation of one of the rea- sons for the blue color of the sky. The sun’s ray, or what is Called the white light of the sun, was resolved by means of a glass prism, by Sir Isaac Kewton, into the seven primary rays of light, viz., red, blue, violet, etc., \ 16 and tl-i oir com'bination again produced the white light-- show- ing hotlx fiynthetically and analytically of what the sun’s light was composed. It was announced in England about the beginning of this c'entury, tiiat the red ray of light was heating, the 'yellow ray was illmniuating, mid the blue ray in a remarkable degree sibnidated the devdoynient of vegetable life. From this discovery we can imagine the immense influence whirdi the intensely blue color of the sky in the equatorial regions has and always has had in conjunction with the sun’s white light, aixd the heat and moisture of those regions, upon the development there of vegetable life. This intensely blue color of the sky in the arctic regions may also serve to explain the exuberance of animal life tliere. It being known that the deeper water of the arctic -ocean is' niucli warmer than the surface water which is often frozen, furnishes abundant food for its inhabitants. The increased temjxeratnro of this deep water is probably derived from radi- ation of heat from the interior of the earth under it — as all those regions ai'e more of less volcanic; witness Iceland, Jean 'Mayer, 'Bpitsbergen, etc. The laws, of animal and vegetable life being very analogous, what would stimulate one would probably have a similar effect upon the othei\ In the arctic waters you have warmth, food, light and elec- tricity, escaping through the waters into the air, and all stimu- lating life. ■ ^ Whoever has noticed the dolor of the electric spark in at- mospheric air, from an electrical machine, will readily recog- nize its likeness of color to the blue color of the sky. If experiments should be instituted to ascertain the electri- cal condition of the sky, as associated with its blue.color, and th(?y should satisfactorily establish the connection, the result would prove to be one of the greatest blessings ever conferred upon ' mankind. "What strength df vitality could be infused into the feeble young, the mature invalid, and the decrepit octogena- rian! How rapidly might the various races of our domestic animals be multiplied, and how much might their individual proportions be enlarged! One of the most beautiful illustrations of the mighty influ- ence of the blue color of the sky upon veg^ation, is to be found in the gre.cn color of the lea^ms of plants. It i.sjcno'wn that blue and yellow when mixed produce gi-een, which is IT darker when tlie blue is in excess over the yellow, and tlie re- voi'se wbcn the yellow pi’edominates. Now let us obscrye the process of germination. Seeds are planted in the soil — at first a wliite w’orm-like thread at the lower part of the seed appears; it is Avhite, ajid contains all the primary rays of ligbt; it is the root of the plant, and remaining under the soil continues white. At the upper end of the seed also appears a white swelling, which continues to grow upward till it approaches the surface of the soil, when a change occurs in its color. This is the leaf ; it absorbs yellow A’om the soil which is brown (composed of yelloAV and black), and as it comes within the influence of the blue sky, it absorbs from it the blue light, which mixing Avith the yellow already absorbed, produces at first a yellowish^uTeen, which finally assumes the deeper tinge of green that is natmal to the plant. The plant blossoms, forms its seeds and seed-' vessels, and having fulfilled its mission, the blue, color of the leaves is eliminated, the leaves become yellow, and ahsm'lfing the carbon of the plant, they change their color to brown ; the sajn vessels of the leaves are choked by the carbon ; the leaves are dead and fall to the ground. Thus the blue ray is the symbol of vitality — the yellow ray that of decay and death. Robert Hunt, in his Researches on Light, says “ that the rays of greatest refrangibility, viz., the violet, '&c., favor dis- oxygenatiou, but the rays^ of least refrangibility, viz., red, orange, &c., favor oxygenation.” _ “ The experiments of Seunebier show that the most refran- gible of the solar rays, a4z., the violet, are the most active in determining the decomposition of carbonic acid gas by plants.” These experiments have been confirmed by Mr. Robert Hunt, who says, “ that experiments have been made with ab- sorbent. media, a,nd the light which has been carefully ana^- lyzed, permeating under the influence of blue light, in every instance oxygen. gas,h as been, collected, but not any under the energetic action of yellow or red light. * * It is only the green parts of plants which absorb carbonic acid : the flowers absorb oxygen gas. Plants grow in soils composed of divers mate- rials, and they derive frpm these by the soluble powers of water, which is taken up by the roots, and by mechanical forces carried over every part, carbonic acid, carbonates and organic matters containing carbon. Evaporation is con- tinually going on, and this Avater escapes freely from the leaves during the night when the functions of the Amgetable, like those of the animal Avorld, are at rest, and carries with it car- bonic acid. Water and carbonic acid are sucked up by ca- 18 pillary attraction, and both evaporate from the exterir part of fhe leaves.” “ There is no reversion of the processes "which are necessary to suppoi’t the life of a plant. The same functions are ope- rating in the same way by day and by night, but ditfering greatly in degree. During the hours of sunshine the whole of the carbonic acid absorbed by the leaves or taken up with water by the roots is decomposed, all the functions of the plant are excited, the processes of inhalation and exhalation are quickened, and the plant pours out to the atmosphere streams of pure oxygen at the same time as it removes a large quantity of deleterious carbonic acid from it. In the shade the exciting power being lessened, these operations are slower, and in the dark they are very nearly, but certainly not quite, suspended.” “ Although a blue glass or fluid may appear to absorb all the rays except the most refrangible ones, which have usually been considered as the least calorific of the solar rays ; yet it is certain that some principle has permeated the glass or fluid which has a very decided and thermic influence. Numerous experi- meirts have been tried with the seeds of mignonette, many varieties of the flowering pea, the common parsley, and cresses under the various tints of glass — with all of them the seeds have germinated, but except under the blue glass these pjiants have all been marked by the extraordinary length to which the stems of the cotyledons have grown, and by the entire ab- sence of the plitmuld — no true leaves forming, the cotyledons soon perish and the plant dies ; imder the blue glass alone has the process gone on healthfully to the end.” “ The changes which take place in the seed during the pro- cess of germination have been investigated by Saussure: oxygen gas is consumed and carbonic acid is evolved ; and the volume of the latter is exactly equal to the volume of the former. The grain weighs less after germination than it did befgi’e ; the loss of weight varying from one-third to one-lifth. This loss of course depends on the combination of its carbon with the oxygen absorbed, which is evolved as carbonic acid.” “For the discovery that oxygen" gas is exhaled from the leaves of plants during the daytime, we are indebted to Dr. Priestley ; and Seunebier first pointed out that carbonic acid is requi red for the disengagement of the oxj’gen in this pro- cess. M. Theodore de Saussure and De Candolle fully estab- lished this fact.” The experiments of Seunebier show that the most refrangi- ble of tlie solar rays, viz., the violet, are the most a'ctive in deter- mining the decomposition of carhonic acid hy plants. “We have now certain knowledge. We know' that all the carhon which forms the masses of the magnificent trees of the forests and of the herhs of the fields has been supplied from the atmosphere, to which it has been given hy the functions of animal life and the necessities of animal existence. Man and the whole of the animal kingdom require and take from the atmosphere its oxygen for their support. It is this which maintains the spark of life, and the product of this combustion is carbonic acid, which is thrown off as waste material, and which deteriorates the air. The vegetable kingdom, however, drinks this noxious vapor ; it appropriates one of the elements of this gas — carbon — and the other — oxygen — is liberated again to perform its services to the animal world.” “The animal kingdom is constantly producing carbonic acid, water in the state of vapor, nitrogen, and in combination with hydrogen, ammonia. The vegetable kingdom contin- ually consumes ammonia, nitrogen, water, and carbonic acid. The one is constantly pouring into the air what the other is as constantly drawing from it, and thus is the equilibrium of the elements maintained.” “ Beccaria examined the solar phosphori, and ascertained that the violet ray was the most energetic, and the red ray the least so, in exciting phosphorescence in certain bodies.” _“M. Biot and the elder Becquerel have proved that the slightest electrical disturbance is sufficient to produce these phosphorescent effects. May we not therefore regard the action of the most refrangible rays, viz., the violet, as analo- gous to that of the electric disturbance ? May not electricity itself be but a development of this mysterious solar emana- tion ? ” ■ • _ It has been long known to chemists that a mixture of chlo- rine and hydrogen gases might be preserved in darkness without combining for some time, but that exposure to diffused day light gradually occasioned their combination, and which is etfected with the greatest speed by the extreme, blue and indigo rays. M. Edmond Becquerel in 1839 first called attention to the “ electricity developed during the chemical action excited by solar agency.” The experiments of Dr. Morichini, repeated by MM. Carpa and. Ridolfi, that violet rays magnetized a small needle, were successfully confirmed by Mrs. Somerville. 20 not solely a radiant visible element. _ It bas other nroTi, .■ies Vvdiich cannot be overlooked. It oxidizes, colors, iil ae'M - Lio'bt becomes, absorbed — light changes into neat, ami heat into^electricity ; in fact, light in its visib e character only shows one of its many phases. Light hole s many forces within its beams. It has properties, powers, ot its^ owii which neither mathematician nor optician can giasp. it is a ercat chemical agent. Colors-:are produced by a change resnltlug from a polaric act of arrestation— yellow and red yellow belong to the acids; blue and red blue to the alkalies. The iimlnlatory theory explains the radiant visible i^ropeity of li'dit, hut it does not explain its chemical eftects, the opti- cal iiohirity of a chrystal and its connection with the polmic condition of its conkitueiits— the ditfraetion, inflection, intei- ferciices, the oxidation of surfaces as_ the cause of natural co- lors, t'iie presence of the chemical action of lig i , le piesen nf heat, electricitv, magnetism; yet xight produces all dhes phenomena; it vitalizes, and the organic action of light is witnessed in the fauna and flora around. I'.ave seen that bine light, and the violet ray which is a com., on-, id of it, and the red ray-being the .mbst refi-iingihle r->vs^ef !he solar spectrum — excite magnetism, and electuuty, l)YAvMch carbonic acid gas evaporated from growing pl.ants k decomposed and oxygen theroot •xo'ain in maturing the flowers, fruit and seed of the plant, thus stimaleting the active energies of the plant into' its fullest and most complete development. I[owthis is just iviiat I think is done in the vegetable world by'the blue light of the firmanent. That Id Lie light of the firmanent, if not itself electro-magne- tism eimlves those forces Avhich compose it in our atmosphere and anplying them at the season, viz., the early J3nug, when tiie sL-i is finest, stimulates, after the torpor of winter, the active ener-ies of the vegetable kingdom, by the decomposi- odroibomc acid |as-saprlyi.;g cajhon for the pi auto and oxygen to mature it, and to complete its mission. In tlie experiment which I have made in the cultivation of cn’apes under violet light, I have endeavored ft the blue light of the firmanent, causing the other rays ol the solai sSrufi to be absorbed while the blue and violet rays were iLrmitted to permeate the violet glass into the gnpiery. The ditference of tLperature under the white glass and under the violot glass of the grapery is supposed to bave exei ed currents of electricity sufficient to decompose more lapidly the carbonic acid gas that bad been evaporated fi-pm the leaves the vines, than would have been doue under the influence of 21 the suiishiae alone — thus stimulating the increased ahsorptiOn of ox/gen, and the deposit of carbon in the vines, and- con- stantly and quickly renewing the evaporation of carbonic acid gas. The result has been seen in tlie wonderfully large pro- duct of fruit, accompanied by a prodigious' formation of new wood, to yield the crop of fruit for the ensuing year. The investigations that have been made during the present century regarding light have developed the existence of some remarkable attributes ; one of the most astonishing is the dis- covery that there is no heat per se in the sun’s ray, though it is one of the causes which produce heat. This is established beyond dispute by the existence of the intense cold which pre- vails in the upper atmosphere, increasing with its altitude, and through which all the sunlight which reaches the earth must pass, but whose temperature it cannot alter. Hence you have at the present time the line of perpetual snow, according to Professor Agassiz, at an elevation of 15,000 feet at the equator, of 6,000 feet at the latitude of 45°, and gradually approaching the surface -of the earth, till it reaches it at 60° of north lati- tude, beyond w.hich ice prevails nearly to the pole. Aeronauts have remarked also at great altitudes above the earth that the thermometer had ceased to mark any variation of temperature w'hen exposed in the full sunshine or in shadow. A curious illustratioh of the fact that something more is needed than sunlight to produce heat is to be found in the fact stated by the famous arctic navigator. Dr. Scoresby, as well as- by others, that when, after a long night in the arctic regions, the sun had appeared, though the thermometer was below 32° of Fahrenheit, and everything around was frozen hard, he observed that the pitch with which the seams of the jilanks of the ship had been payed, on the side of the ship exposed to the sun, wa's melted, notwithstanding the giniat declination of the sun aiid the small angle of incidence, that the nearly liori- pntal rays of it made as they fell upon the pitch, while that in the shade on the other side of the ship was so hard that it was with difficulty broken with a hatchet — other objects on the ship manifesting at the same time the low temperature marked by the thermometer. I am not aware that any explanation of this phenomenon has ever been attempted. I may, therefore, offer to suggest that the pitch being an electric or non-con- ductor of electricity and negatively electrifi.ed when the. sun’s ray positively electrified fell upon it, an explosion took place, heat was evolved, and the pitch was melted — ^thus proving that froni =!un8liine is produced by tlic contact of an electricity opposed to that of the sun’s rays. As a corollary from what has just been stated, it may be. observed, that the heat of the equatorial and tropical oceans is •lot de^ i ve d from the sun. We do not heat our houses by kindl’no- fires at the tops of our chimneys or boil our water ! roni obove, but rather we descend into our cellars, and make onr Urea for that purpose in them its many surfiices, if agitated by winds, the rays of i he smi would be reflected in all possilde angles corresponding 10 the angles of incidence of the rays themselves, and the heat would l)o"lost in space. Whence comes, then, this ocean heat hi the tropics, finding its vent in the arctic and antaictic regiovis through the Gulf Stream of the Atlantic, and the dapan Stream laving the shores of northeastern Asia, and the south-eastern current running 'along the south-western coast ^-'f South America to the Antartic seas ? Does it not come by radiation from the interior of the earth from those great fires which, by the elastic gases and vapors engendered there, in raanv parts of _ the world upheave mountains and islands, and forming chimneys for themselves in their summits, belch oi^ that superfluous heat, light, electricity, and magnetism which radiation to the surface of the earth at times is inadequate to discharge? And are not these great ocean currents of heated water merely channels or flues of radiation of heat fiom he- iieath, by which, for climatic purposes, the Ornnipotent Creator has devised the means of distributing this interior heat over ■the surface of our planet ? All admit the existence of those great forces of nature in the interior of the earth, manifested through volcanic action in those imponderable elements of heat, light, electricity, and niao-netism. Why are those forces there? May they not be the'^forces which turn the earth on its axis,_and aid in propel- lino- it around the sun ? May not the frigid zones north and south furnish the cold cushions of water in the extreme depths of the ocean, of the uniform temperature of 39J° of I ahren- heit and of nearly the greatest density known to that elenaent, for the purpose of restraining and controlling the radiation of that great interior heat of the earth, which otherwise might be wasted? Dr. Winslow, in his treatise on light, its influence on life and health, says : “ Accurate calculations have been made as to the temperature of the ocean. The results obtained clearly establish that the lowest degrees of temperature are obtainable on the surface of the -vrater; and that about ten feet below the surface the thermometer rises several degrees, — 90° is said by Mr. Agassiz (son of Professor Agassiz,) to be the highest tem- perature he has known the oceau to attain ; at very great depths of the ocean a uniform temperature of about 39i-° has been found.” . The low temperature of the surface water of the oceau is attributable to the evaporation which is constantly goiug on, carrying off the atmospheric heat adjacent, and proving con- clusively, that the Gulf and other -^arm ocean cuiTents do not derive their heat from the sun. These reflections have forced themselves upon me, while pondering over some of the great revelations of . nature. In a recent report of the Secretary of the Agricultural Bu- reau at Washington, he states — “ On the loth of June the suu is more than 23° north of the equator, and therefore it miglit be inferred that the intensity of heat should be greater at this latitude than at the equator ; but that it should continue to increase beyond this even to the loole, may not at first sight appear so clear. It will, however, be undei-stood when it is recol- lected that though in a northern latitude the obliquity of the ray is greater, and on this account the intensity should be less, yet the longer duration of the day is more than sufficient to compensate for this effect and produce the result exhibited.” ' It strikes me that this explanation is not sound. I remem- ber several years ago, at Philadelphia, on the afternoon of a day in August, when the thermometer- was at 94°, that in fif- teen minutes the thermometer fell 40°, which was owino- no doubt to a descending column of cold air from the upper at- mosphere, attracted by some local electrical disturbance. The continuous heat of the preceding summer months could no more prevent this thermal change at Philadelphia than could the long day with the oblique sun’s rays increase the intensity of the heat in high northern latitudes. Professor Maury says— “The summer temperature as ob- served on the very borders of the Polar ocean is absolutely marvelous. Observations made with a view of determining this accurately have for some years been, taken in Alaska! One of the observers in the northern district of Yukon states in the ‘Agricultural Report’ for 1868, ‘I have seen the ther- mometer at noon at Port Yukon, not in the direct rays of the sun, standing at 112° ; and I hm informed by the commander of the post that several spirit thermometers graduated to 120° had burst under the scorching sun of the arctic midsummer, which can only be appreciated by one who has endured it. In 24 midsummer, on the Upper Uukou, the only relief from the intense heat un.der which vegetation attains, an almost tropical luxuriance, is the two or three hours during which the sun hovers near the northern horizon, and the weary voyager in his canoe blesses the transient coolness of the midnight air. A-C'cerdhig to hi. (le Humboldt, the sky is bluer between the tro'des than in the higher tempei’ate latitudes, but paler at sea than in the interior of countries ; the blue is less intense at the horizon than at the zenith. The early maturity of human r.fe in the tropics is to be attributed to the stimulating influ- ence of the enormous quaatitios of electricity, which, continu- ally passing by day as well as hy night in the auroras from the poles to the equator, and descending to the earth in those re- gions, in those dazzling sheets of lightning flame, so terrifj ing to all who have witnessed them, and conducted hy the inces- sant rains Jirevailing there in certain seasons of the year de- ox^imnate the enormous volumes of carbonic acid gas gene- rated hy the exuberant vegetation, as well in its growth as in its decay, thus supplying excessive quantities of oxygen gas to stimulate and support the animal life, as well as carbon to fhe fresf vegetation which- is being continually renewed— the cir- cle of development and decay in the vegetable kingdom being thus always preserved. V 'Vv^'e have thus? seen that the magnetic, electric, and thermic pmvers of the Sun’s ray reside in the violet ray, vkidi is a compo-ond ■ of the blue and red rays. These constitute Avhat are terme d the chemical powers of the sunlight. That they are tlie most important powers of indturc, tiiore can he no doubt, as T^'ivliout tlioni life cannot exist on tliis planet. TV^itliout tlicse chemical powers there could he no vegetation. 'Without veg- etation there could he no insect life, and no development of the higher order of animal existence. Tlie earth would he without form and void, and we can now uiiderstaiid the poten- tial iiieaniiig of the first sulilimo utterance of the ,A.lmighty in forming this earth, when he said “Lot there he Light, there was. Light. ■ From the foregoing premises, we deduce the following con- clusions : ' ■ ■ ' ■ ^ , 1. Heat is developed hy opposite electricities in conjunction and in proportion to the quantity and intensity of those elec- tricities in contact with each other, will he the intensity of the The blue color of the sky, for one of its functions, de- oxygenates carbonic acid gas, supplying carbon to vegetation and sustaining both vegetable and animal life with its oxygen. APPENDIX. [I-] UNITED STATES PATENT OFFICE. 119,242, ArausTus J. Pleasontox, of Philadelphia, Pennsylvania. L. prorrA^it in Accelerating the Growth of Plants and Animals. Spfiifieations forming j>art of Letters Patent No.. 119,243, dated September 26, 1871. 7 ; all whom it may concern : . p 0 it known that I, Augustus J. Pleasonton, of the city of Pi.ilauuh-hia, in the State of Pennsylvania, have discovered a new and v tluablo aid and improvement in accelerating the growth to maturity of plants, vines, vegetables, cereals, and the flora of the vegetable kingdom of nature, and of animals, fowls, fishes and birds of the animal kingdom of nature; and that I do hereby declare the following to bo a full, clear, and exact description of the 0 |; -rotion of the same by means, of combining the natural light of the sun transmitted through transparent glass with the nam-ral light of the sun transmitted through blue ^ass or any of t'it var.eties of blue, as indigo or violet, in varied proportions of biuo and white glass, from one of blue to eight of white, up to equal proportions of blue and white, as greater or less caloric is needed,, according to the nature of the plants or animals, to accelerate their natural growth, increase their vitality, and h:i„sten inaturiiy ; reference being also raadO to the accompanying drawing making a part of this specification, in which the figux’e represents one form of construction of a conservatoi'y or grapery, in which A A A represent the clear or transparent glass, and 13 the blue or coloured glass. Proper ventilation is ofibeted by moans of wire cloth placed in the walls, as shown at C, and which can bo opened and clo.sed at pleasure by means of hinged glazed sashes, as shown at D. There is also represented at E a hinged sash, glazed with both cle.y and blue glass, for changing the angle of incidence to agree with the declination of the sun. ' These proportions of the natural light of the sun with the blue or electric transmitted rays may be varied to conform to the epeeific constitution of the varieties oV life in the vegetable world and the vaiaetles of consti- tution in the animal world, and can only bo ascertained throughout both Icingdoms by progressive and continued ex])eriinent. rho proportions of the heating rays and the transmitted blue electric rays must be varied to conform to the constitutional vitality ot the vegetable or animal, and care must be had that the heating or caloric .light is not in excess of the electric or vitalizing and , growing ti’ansmittcd blue light. • • . ^ I confine myself to no particular form, externally or intcrnahy , of the buildings to be used, whether they apply to the growth and propagation of plants, vegetables, fruits, &o., or to the ^rowtu pro])agation,"&c., of animals, fishes and fov.ds; but the best lonn is that building which will receive the rays of the sun daring its daily revolution as nearly perpendicular as pi’acticable_ to the surfaces of the glass covering, so that the rays shall bo as little dcfiected as possible, anlue, purple, or violet glass or equivalents, as and for the purposes set forth. In testimoiTcy that I claim the above, I have hereunto snO-^ scribed my name in the presence of two witnesses at the titj of Philadelphia, the 23d day of Jiine, A. D. 1871. ^ ’ AUGUSTUS J. PLEASONTON. Witnesses : H. Tunison, II. A. Nagle. [II.] In the winter of the year 1872,1 called at the Pennsylvania Hosnital, on Pine street, between Eighth and Ninth streets, in this city, to suggest to its officers the introduction of my plan of using the associated light of the sun and the blue colour of the S'W alleviating the sufferings of, and probably in restoring to health many of their, patients. On being presented to them, one oi the resident physicians, on hearing my name mentioned, asked ’f I was the author of the experiments with blue light of which ho had read r.n accouut. On receiving my answer, he said ; “ 1 have 2J pomctliing curious to tell you. I fim a native of Tlrazil, where niy father still resides ; I have been’ educated in the United States; last week I received a package of books, pamphkU'i, &c., from my father, in Brazil, who had ordered thoin from Paiis. In his ac- companying letter my father directed my partitnilar attention to a French pamphlet wliich detailed some remarkahle experiments on animal and vegctalde life, that had been mude with blue glass and .sunlight, that he thought would he nsefiil to me in my medical proicssion. On examining the pamphlet 1 discovered it to be a transliftion in tho French language of your memoir on that subject. The translator, however, had not mentioned your name in it, or even tho namo of the locality where the exj)criments had been made. It evidently was intended to convoy the impression that the experiments had been made in Paris.” If the trumslator was a Frenchman we can pardon him for omitting the name of tho author, .in memory of tlio ancient Bevo- lutionary aliiancc between liis nation and our own. We can oven condone his fault, smarting as he must have been under the then recent loss of Alsace and Lorraine — but wo think that it might have occurred to him that the scene of my experiments was rdso the locality of tho electrical experiments of Frtinklin, whom his countrymen and women always delighted to honor, and henc. ihe namo of Franklin’s- home might have been associated with the announcement of discoveries in physics that do no discredit > ven to those of Franklin himself. [ni] V Til's Diamoxi); its OuiGiN. — In former editions of this memoir I have attribated the origin of the diamond to electricity in the upper atmosphere decomposing carbonic acid gas, fusing the car- bon, converting tho oxygon gas into ozone, and crystalizing tho fused carbon, under the great evaporating power of the intense cold there prevailing. The Atheneura says; “A somewhat novel idea is stated by M. Desdemaines Hugoii, in a paper ‘ On the Diamond Diggings of South Africa,’ which is printed in tho Revue ScientiJiquedelaFranee et 1’ Stranger. He states that theair is always highly electric where diamonds abound, and he intimates his opinion that this may throw sotne light on the formation of that gem.” 30 [IV.] [From the President of the Indiana University.'] Indiana XlNivEasiTY, ' "I Bloomington, June 15, 1871. j Gen. Pleasonton. Bear Sir: — I received a few days ago a pamphlet containing an account of your iuteresting experiments on the influence of the blue ray in developing animal and vegetable life. If. the experi- ments, where it so difficult to determine tlio amount of influence duo to the light, eorapai’ed with that due to other circumstances, have been fairly made, as doubtless they have been, you have opened up a now field of great practical usefulness to all the world. Thanking you for your kindness in sending me your treatise, 1 remain. Very respectfully yours, T. A. WYLIE, [V.] [P/'o/n the President of the Lehigh University^ The Lehigh Un-iversitv, ) South Betflehem, Pa., President’s Booms, July 10, 1871. ) . My Dear General ; I have ju.st received and at once read your very interesting paper on -violet rays, The facts are astonishing, and your explanation evinces care, judgment and research. I shall take pleasure in putting it- among our scientific papers, and thank you for oending it. ; Yery faithfully yours, HENRY COPPJiE. Gen’l. Pleasonton. [YL] [From the Ron. -Wrh. M. J^eredith, late Secretary of the Treasury of the United States ] My Dear Pleasonton : I have delayed thanking you for the pamphlet you sent me, till I should have read it, which I have now done twice, with very great interest and pleasure. I congratulate you sincerely on the discovery you have made, which must not only be greatly valuable in Agriculture and Horticulture, but in many other matters as well. Alwai'S faithfully vours, W. M. MEREDITH. Gen. Pleasonton, Monday, 10th July, 1871. 31 [TIL] [From Wm. A. Ingham, Esq,, a Director of the Lehigh Talley itailroad Company. 1 320 "WAiiNUT St.. ) Philadelphia, AuguU 29th, 1871. | Pear General : ' Alio .V me to return my thanks for the copies of your pamphlet. I have read it with great interest and am satisfied that your dis- covery will have wonderful results, revolutionizing in fact the f-cience of horticulture. I am, very truly yours, WM. A. INGHAM. - Gen. a. J. Pleasonton. [Till.] [ From the Hon. Joserh R. Chandler, late Minister Plenipotentiary of the United States at the Court of Naples ] 153 North Tenth Street, ) 20th September, 1871. j Pe.ar Sir; I thank you for a copy of the third edition of your pamphlet on '■ the influence of the blue colour of the' sky.” I cannot doubt the importance of your discovery, nor fail to see that the public must hold itself indebted to you for your interesting and success- ful experiments. W'itb great respect, your servant, JOS. E. CHANDLER. Gen. Pleasonton. [IX.] Department of the Interior, 1 Patent Office. j Washington, D "C., August 15th, 1871. A, J. Pleasonton, Philadelphia, Penn. Your letter of the 14th inst., relative to your invitation to the examiner in charge of the Agricultural class of this office to call. u])on you to witness the influence of the “ blue colour of the sky ” i n developing animal and vegetable life, is received. In reply you are informed that Prof. Brainerd is at present con- fined to his room by sickness, but a leave will be given him for the purpose of accepting your invitation, as soon as he is able to travel. Very respectfully, your obedient servant, M. D. LEGGETT, Commissioner. C2 [X.] Department of the Interior, \ Datent Office. J Washinoton, D. C., August 19th, 1S71. Dear Sir: I have so far recovered from my late illness as to he able to pay you a visit in compliance with your invitation, for the purpose nf examining your improvement in the construction of conservatories. I purpose to leave tliis city on the 8 A. M. train on Tuesday, and shall therefore be due at Philadelphia at 1 P. M. Respectfully, J. BRAINERD, Examiner. Gen. a. j. Pleasonton, Philadelphia, Pa. [XI] Department of the Interior, 1 Patent Office. j ■Washington, D. C., September Gth, 1871. Dear General ; ^ Your drawing arrived this morning, and the patent will now go to issue, but will take the usual time. The Commissioner yesterday introduced General Babcock, who is Superintendant of .Public Grounds, and Consulting Engineer of the Board of Public Works. T^ie object of his call was to learn particulars in regard to your eerufean process. I had a pleasant interview with him, at the close of which he desired me to write to you, asking the privilege of using your invention upon a grapery which bo is now fitting up on the President’s grounds.^ An answer directed to the care of myself or Commissioner ot Patents, will reach him promptly. ****** Respectfully, General A. J. Pleasonton. J. BRAINERD. [XII.] Paris, September 29th, 1871. General Pleasonton, Dear Sir:— I have just received and read with great pleasure, vour very interesting paper from the Gardener's Monthly, ot August last, concerning your experiments on the action of coloux-cd light cn plants and animals. You will find in the “Report of tne 33 Department of Agriculture,” at 'Washington, for 1869. a ^'e v 1 ’-g report of mine “on the influence of climalogie agents, atnioreiiej ; and terrestrial, upon agriculture,” where, in the chav-bers of light and electricity, I • have treated fully all these questions with x great number of . experiments aiid quotations of authors. At that time I had no idea of any of your publications, although [ had formed a bibliogranhj' on that subject of 1326 arlicles in every language. I am preparing a work iii French and English on Agricultural Meteorology, and I should be most happy o mention in it your experiments, and to- receive all that you have published. My name may be known to you through my papers on Meteorology at the French Academy and in America. I was the founder and director of the observatory at Havana until tlm., beginning of our war, being now a victim of my patriotism. [ correspond with several journals of the United States, as the American Agriculturist, the Rural Neio Yorker, etc., etc. ^ ^ < ifi iii ii: ^i ^ I remain, General, your most obedient servant, 51 Kuo Mazarine, Hotel Mazarin. ANDRE POE'r. [XIII.] Paris, JYovemher 10th, 1S71, GENEKAtt A. J. PlEASONTOX. Dear Sir: — Your most affectionate of October lOtli, is at hand, with seven copies of your interesting pamphlet. After a very careful study of that paper, I should advish you strongly to pursue 3 ’our exijeriments on the i.-fluence of colouired lights on vegetable and animal life. There are still a great manj' points to be resolved, and, unfortunately, this important question has been totally abandoned in our days. Should you publish anything else, pray do not forget me. I shall be very happy to quote all your experi- ments in my works. At the next sitting of the French Academy, I shall also endeavor to have a little extract of your pamphfefc inserted in ti.o Coniptes liendus of that Institution, with' a copy presented in your name, and also to M. Bocquerel, M. Duebartro, the Meteorological Society, etc. I am waiting for the return of one of its perpetual Secretaries, M. Elie do Beaumont. ' I shail have the pleasuro^to send you whatever may be published on your experiments. I have sent another copy to tho Meteorological Society of Yienna, very much interested in the study of periodical phenomena, treated in ray second report to tho Department of Agriculture. ^****«*=i: I remain, your most obedient servant, ANDRfc POEY. 54 Rue Mazarin, Hotel Mazarin. 34 [XIT.] Paris, November 2Jtth, 1S71. General A. J. PriEASONTON. Dear Sir: — As I had promised you T enclose tho little extract presented to the French Academy of Science, Monday last, and ■which will appear to-morrow in tho Comptes Jlendus. I took par- ticular pains to write a condensed letter, giving the most sG'ikmg facts, to the perpetual Secretary, the great Geologist, M. Ehe de Beaumont, who was very much, interested in your experiments. A copy was also presented to tho Academy, Becquerel Jiathor, DuchaVtre, and Barral, the editor of the Practical Journal of Agri- culture^ Avho will reprint it in that paper. At the same time dif- ferent scientific and political papers whl make some mention of it. I shall send next Aveek the translation of my letter to the excel- lent Emrlish journal called Nature ; so your experiments and name Avill be, in short, spread through tho scientific Avoild in Europe. :|C * * * * I remain, General, your most obedient servant, ANDIlil POEY. 54 Rue Mazarin, Hotel Mazarin. [From Rev. Henry A. [XY.] Boardman, Pastor Tenth Presbyterian Church, Philadelphia. 1 My Dear General : , „ i I thank you for your generous supply of tae Memoir, and not less for the very kind terms of your note. , . ^ 7 . . , , „ Once before in our national history tho subject of Blue Light has caused a great commotion. There will bo a greater still before I'ono-, and in a somewhat more beneficent direction. I heartily congratulate you on tho just fame Avhich is already assured to you as the reward of your great discovery. 1 shall place tho pamphlets whore they will by appreciated. Ycry sincerely yours, H. A. BOARDMAN, May 1st, 1872. 1311 Spruce Street. [XYL] \_From the same.'] 1311 Spruce Sr., June 1st, 1872. My Dear General : “ Laudari a viro laudato," — to bo praised by a man ivho is him- self praised,— the Latins used to think was a very nice thing.'' So 35 I take great pleasure in enclosing a letter from the Rev. Dr. Sprague, for forty years a pastor at Albany, one of the roost ac- complished and revered clergymen of our church or country, and enjoying a high European reputation. You will see what estimate he puts upon your great discovery, and hd-w he prizes your autograph. For I took the liberty of sending him your kind note to me, for his fe,mous autographic collection — the largest (some 200,000 specimens, I believe,) and finest in America. I enclose, also, a note from Mr. Alex. Brown, Nineteenth and TTalnut, to whom I gave the Memoir. I know it will gratify you. With sincere regard, I am, dear General, yours, H. A. BOARDMAN. design these two autographs for your collection, so you will not return them. [XVII.] [iVom Alexander Brown, Esq., Banker, &c,'\ PnmADELPniA, May 80th, 1872. Eev. H. a. Boardman. Dear Sir : — I thank you for the copy of Gen. Pleasonton’s ad- dress before the “ Philadelphia Agricultural Society.” I have read it with great interest, and think that the successful result of his experiments of the blue colour on animal and vegeta- ble life must carry conviction to every mind. Very respectfully, yours,' ALEX. BROWN. [XVIII.] [From the Rev. Dr. W. B. Sprague, an eminent divine of Albany, New Vor^.] Flushing, May 80, 1872. My Dear Dr. Boadman. '' Since I wrote j'ou yesterday, (I believe misdating my letter.) I'have read the pamphlet you kindly sent me, with astonishment and admu’atidn, 1 am not chemist enough to pronounce upon every part of it, but it seems to me that the man who could have written it is destined to be a great benefactor to the world ; I do not seewhy .it should not mark the introduction of a. new and better era. I shall lay it away, with the author’s autograph, as containing everything conceiming him that I should desire. With much love, as ever, yours, W. B. SPRAGUE. 33 [XIX.] [From H. ui. Foardman."] 1811 Si’KTJCE St., Oct. 10th. 1'>EAR General : Wc firo all prepared to testify that the Hue glass grapes are in size, color and liavor of the very choicest. If there bo gainsaycrs send ihom to us. Wo give you many thanks for so generous a sample of your crop. And what too ! The fresh testimonies you recite are very remarkable — a fiir- iiicr presage of the certain and cai’ly attention which will soon be given to this whole subject, by mlm of science.. I regret that I am compelled to send this bare acknowledgment of your es- tremoly interesting letter. - I am, very truly yours, ir. A‘. ]30 AHd:iian. [XX.] [From Lieut. Col. Charles Manly, Loyal Volunteer 'Engineer' StaL Corps, England.'] CO Westbourne Terrace, Hyde Park. 'hoi^i'Don, March 23d, 1S72, Nt Pear General: Pr;' e accej)fmy thanks for your kind letter of 6th inst., and tor Ihc six copies of your most interesting paper, which I sliall .dis- t vibntc to the persons most capable of comprehending it, and of repeat! og the experiments hoi’O; , 1 am grieved to say that my dear old friend A. H., cf t'openliaaen, for whom I ventured to' ask you to' send mo your paper, has died in the interval, and ho never I’ceeived your paper, nor tim copies of tho Comptes Jiendus de V Academje de Sciences do Paris, trpa Ung of tho subject, of which I procured him exomplaires. liis son will, I hope, keep up his Horticultural Experiments and when I next go to Denmark I will tell you whether any experimento hayo bcen.tricd of your sj^stem. I have many friends who will, 1 think, try tho system, and if you dc.siro to make it known, seing made its attributes were at oiice called ii-to use. “ For the earth brought forth tlie green herb, and such as yieldeth seed according to its kind, and the tree that beareth fruit having seed, each one according to its kind.” hTo herb could have been green Avithout light, and no tree could have borne its fruit In darkness, nor . could seed have been matured Avithout light, and yet this light came neither from the sun, nor the moon, modern spectroscopes to the con- trary potAvithstanding, for as yet neither the sun nor the moon had been created. Hence, we can understand that the Creator, in directing that light first of all should be made, intended to constitute a force superior to all other forces, for it is by light that they are all developed, and made auxiliary to the great plan of Creation. “14. And God said, Let there be lights made in the firma- ment of heaven, to diAude the day an d'the night, and let them be for signs and seasons and for days and years. “ 15. To shiue in the firmament of heaven and to ^ivo light upon the earth, and it was so done. “16. And God made two great lights, a greater light to rule the day, and a lesser light to rule the niglit, and the"^stars. “ 17. And he set them in the firmament of heaven to shine upon the earth, “ 18. And to rule the day and the night, and to divide the light and the darkness, and God saw that it was good.” It will be seen from these verses, that the ruling intent of the Creator was to furnish light, and not heat, to the world he was bringing into existence — to separate the day from the night — as signs and for seasons, and for days and years, to shine in the firmament of heaven, and to give light upon the earth. These then are the varied functions to be performed by the sun, moon, and stars, hy the fiat of the Creator. l\Iuch Speculation has been evoked, in the inquiry for the source of that light that was ordered to be made previous to the making of the two great lights, the sun and moon, whicli he set in the firmament of heaven to shine upon the earth. The modern revelations of the telescope in disclosing the character of the more distant fixed stars, the congregations of stars in the “ Milky Way,” in the nebulae and cloudlets of lights, furnish an answer to all such inquiries. The limited vision of Moses, unassisted by the telescope, which, in his day, had no existence, would not have permitted him to compre- hend any revelation of the glories of the world of astronomy, as known to us now ; and hence, no such revelation was made to him. He was only instructed partially on the subject of our solar system, and the myriads of lights, lesser and greater than any that our system contains, which were sending theii' illumination over a boundless world, were entirely unimagiued by him. But we can readily fancy with our increased know- ledge of astronomy, whence this primeval light was drawn. W e may suppose that our solar system was the last created of the various systems which stud the heavens with their brilliant eftulgence, and that the materials which compose it were easily gathered from the mighty masses that illuminated the firmament. Our astronomers tell us of the infinite star depths, in which are assembled series of worlds without number, all circling 34 iirouml their respective central orbs, and all moving with inconceivable velocity towards some region of the firmament so remote that our finite intellectual powers fail to conceive of it, and that, in this grand movement of worlds, our diminu- tive solar system has ifs allotted part and pursues its inevitable destinv. Hence arises the reflection that when our system shall approach the astronomical horizon of this mighty systern of worlds, 'and shall be descending helow it, as our sun now does l)elow our own horizen, another solar system, transcending in its glories anvthing of which the human mind can conceive, sliail arise in the western firmament to take the place that had been vacated by our own, and thus system after system shall he circling in the great expanse of space, till time shall he no more. We must have a starting point in our discussion, and we will begin with matter, out of which all things are made. We define matter to be anything which moves, or is the subiect of motion. W e prefer this definition before all others, since it is entirely irrespective of human existence, and has no reference to human impressions. Motion was produced long before man, and will continue long after he has passed away. When matter is said to be solid, liquid or gaseous, we convey a very inadequate idea of its composition or of its c )udition. The microscope, as its powers are bein^ developed, reveals to us forms and conditions of matter of which the inost fm-tile imagination could have had no previous conception. So in the series of what is termed created matter, we have but a verv faint image of a few of the most obvious links in the chain of its conditions, while we know and can know nothing of its extreme terminations, its greatest density and most minute tenuity. But we may conceive that whatever moves, or can be moved, must be matter — according to this definition, the imponderables, light, heat, electricity and magnetism, are all material substances, so subtle and attenuated, however, that human ingenuity has never been able to discover then components, or" to reduce them to standards of^mparison by which their powers might be measured. We might go farther and assert that all human emotions as well as animal instincts are likewise material, since our only cognizance of them is made apparent to us through our senses, concerning whose materiality there can be' no question. Let it not be supposed that this idea of material being is at all inconsistent with an aspiration for a future life, since the resurrection of 35 the material body is as much a part of the Christian’s creed as is the hope of his immortality. Moses has told us for what jiurposes the suu and moon and stars were created ; “ to rule the day and night, and to divide the light and the darkness, and as signs, and for seasons, and for days and years.” JTow, it is a very remarkable thing, that Moses, who was born ia Goshen, a province of Egypt, who passed the first forty years of his life in Egypt, which lies between north latitude 32° and 22°, and 57° and 34° east longitude, the next foi-ty years on the borders of the Desert, and the last forty years thereof in the wilderness with his people, should have omitted to assign to- the sun the heating qualities which our scientists declare it to f possess if, in fact, the sun did possess such powers, and the fact had been revealed to him by the Almighty. I ^lodern discoveries in science go to show that Moses was. right in his description of the functions of those luminaries. ;■ We may imagine the astonishment, amounting almost tO' ' incredulity, with which Moses received the revelation regard- ing the attributes of the sun, moon and stars. Living in the ^ hot climate of Egypt, or of the Desert, whose “ soil is fire, and , whose wind is flame,-” and termed' “ burning sands of the ! Desert,” from their great heat, to what other source could he ; . refer this terrible heat than to the sun. Yet the sun is de- L Scribed to him as a great light, not a great furnace, not a great ' source of heat, but simply as an illuminating power. When traveling in the Desert, and overtaken by the burning Sirocco,. [ whose blast, like that from a fiery furnace, obscuring the light 7 of the sun by the clouds of burning sand which it had raised, [. Closes might have, by a course of reasoning, traced a connection between the raging tempest and the sands heated by the sun, ' and thus have assigned to that luminary the heating power claimed for its radiations. He might even have been familiar i with the tenets of the predecessors of Zoroaster, and of the fire worshippers in Persia, who worshipped that great orb of light as the source of earthly heat, but if so, he discarded j/ all such imaginings, and boldly declared “ that it is the greater I of two lights, intended to separate the day from the night ; as K. signs, and for seasons, and for days and years ; to shine in the E firmament of Heaven, and to give light upon the earth.” K Light is the gireat source of.terrestrial electricity, magnetism H and heat. K ■ Whatever moves^ or is the subject of motion, is matter. 36 "We cannot conceive of motion, witliout associating with the idea an object to be moved. Hence light, which moves with a velocity of which ^ye may speak, bi^ whicj is not con- ceivable by us, is composed of matter. hen the Creator, in his beneficence, first displayed the rainbow in the atmosphere, he tam?ht mankind their first lesson in philosophical analysis, lie thus showed that the white-light of the sun was not a simple substance, but that it was composed of seven primarv rays, which, by their combinations, produced all the varying tints or colours that are seen in nature, and yet how manv myriads ot years have passed since this magnificent spectacle has been •exhibited to man before any one ventured to impure into the simple and beautiful lesson which it taught. Lven yet, what profound ignorance prevails everywhere in connection wit i , the iiifiuences which these elementary rays develop. Light, which thrown upon the photosphere of the sun. trom the imiumerable orbs that from their starry depths il uiiiinate the expanse of Heaven, is reflected to this planet with a velocity of 186,000 miles per second of time, and recpxires about 8 16-35 minutes to reach the earth from the sun, iiinetv-two millions of miles distant. Whatever may be the composition of the space intervening between the sun and the earth ou - side of our atmosphere, as we are taught that nature abliom a vacuum, it must be composed of s^uiethnig which is of matter. Give it its most attenuated form and call it ethei it is still matter, and light, which is also composed of matter, however subtle it may be', passing through it marvelous speed, must produce everywhere enornioim tiictioii. How whenever one body moves in, on, under, around, or anoTher body in contact with it, such motion produces friction. Friction, derived according to Webster, from the Latin/nco, to rub, as we know evolves electricity, and it is His electricit} an . its correlative magnetism, discovered by Oersted, thc_ c e- brated Danish naturalist, to be its constant accompanimeifi when opposite electrical polarities are united, thus ^lerived which form those tremendous forces of nature that everywhere those changes in, on and about our planet, that meeLur observation at every instant. _ Creator, after having assembled m their respects e po^it o us the materials which compose the planetary and ^^ehar v orij^^^^ uttered the sublime words, “Let Light be made, calk, into being a power which became the generator of all ti e physical forces which control and regulate ^ for a moment imagine the radiant reflection of luminou. matter 37 from every part of the photosphere of that great luminary, the- sun, which in its magnitude was intended to illumine and vitalize all animated matter, as well as to give form and con- sistency to whatever had been created, passing from every point thereof with a velocity of 186,000 miles per second, penetrating through planetary and stellar spaces which, how- ever subtle and attenuated, must have offered some resistance to the passage of this material light, producing everywhere in its passage an enormous amount of friction, and with it elec- tricity and magnetism. Electricity, by the junction of its opposite polarities, evolves heat and also imparts to all sub- stances that are capable of being invested with it, magnetism. The sun, the planets, the stars and all the bodies that stud the expanse of heaven, are doubtless all magnets, to which mag- netism was imparted when the Creator uttered in heaven the words without parallel in sublimity, “Let light be made.” This then is the origin of all the physical forces of the universe. ' Let us consider for a moment the nature of heat, and it will be- apparent that terrestrial heat cannot be directly derived from tlie sun. The tendency of heat is always to ascend into the atmos- pliere, when it is derived from combustion on the surface of the earth, or from radiation within it. The flame of a candle is vertically upward, on every part of the earth’s surface, when the air is still. The eflbrt of heat is to depart from its source with a rapidity proportionate to the intensity of the combus- tion. This is a repellent force — at the same time from its being associated with positive electricity, it is attracted to the upper atmosphere by its negative electricity, always associated with cold, w'hich is- opposed to positive electricity. The diffusion of heat, laterally or downwards, is very inconsiderable, as is constantly manifested in our rooms, where the fire in the grate emits very little heat below the bottom of the grate, and parts of the room distant from the fire are very imperfectly he,ite(l by it. The sun in its daily course being above the earth, if it had any calorific rays, could not send them to the earth below it, through a space of ninety-two millions of miles, which, according to calculations of Pouillet, has a temperature of minus 142 degrees of Centigrade thermometex’. We will illustrate this by an example or two. During our late unhappy sectional war, xit the siege of Fort Sumter, in South Cax’olina, General Gilmore’s heavy guns threw their enormous shells into the city of Charleston, four xmd a half miles distant. While the expansion of the powder in the chamber of these o-uns, in its combustion into gases, evolved a power wbieli tlirew these shells so great a distance, it was totally inadequate to drive the heat disengaged in the conversion ot the powder into these propelling gases to a greater distance trom the muzzles of the guns than thirty feet. It ascended, instanth on leaving the guns, into the upper atmosphere, attracted by an opposite electricity. Any one familiar with the fire of artilleiy, must have observed similar efiects regarding the heat trom the discharge. We will illustrate this by an example. “ Mount W ashington, in the White Mountains, in Hew^ Hampshire, is in north iMitud'^ 44° 16' 25", and in west longitude trom Greenwich /I 16 '26". Its elevation above tide water is 6,293 feet ; and in altitude it is the second highest mountain northward ot the Gulf of Mexico, the highest mountain thereof being Clingmaus Peak, in the State of North Carolina— which is 6,707 teet above tide water. “ The limit of the growth of trees on the north side of Mount Washington is 4,150 feet above tide water. The climate of Mount \\"ashiugton corresponds with that of the middle ot Greenland, about 70° of north latitude or 26 further north than New Hampshire. ' It is an arctic island (so to speak) in the temperate zone, and, on account of its great elevation, it exhibits also the condition of the atmosphere where tlie mercury does, not rise above 24 inches in the barometer. lor peculiar interest, therefore, the Mount Washington (meteoin- logical) station is not exceeded by any point within the arctic circle." It was on this mountain that a party of scientific gentlemeri passed the winter of 1870 and 1871, amid great privations and suffering,. for the purpose of investigating the physical con- ditions of the atmosphere and mountain at that great elevation. “ Observation shows that the climate of any country becomes colder in proportion to the height of the land above the sea. Thus in tropical regions there may be an arctic climate at an. altitude of 12,000 or lo,000 feet. The room inhabited by these gentlemen was in the south- west corner of the railroad depot, about 20 feet long, 11 teet wide and 8 feet high. It was well protected trom the outer cold, was heated by two stoves, one an ordinary cook stove, the other a Magee parlor stove, prized for its marvelous heating power. Their Journal reports as tollows, viz ; 39 ^ " February 4th, 1871, temperature at 7 o’clock, A. M., — 33°; ; at 9 o’clock, P. M., — 40°. In the room the temperature was ^ +35° and sometimes +60°. To do this, the stoves were kept I at a red heat. The thermometer hangs 5 feet from stoves, the ' temperature 10 feet from the stoves at the floor was 12°, in ^ other parts of the room the temperature was 65° ; midnight, i wind fully up to 100 miles per hour and northwest. j “February 5th, some of the gusts of wind 110 miles per [■ hour; at 3 o’clock, A. M., temperature in the room 59°, ‘ barometer 22.810 inches, attached thermometer 62°. Yester- [ day, barometer 22.508 inches.” . i. I7ow let us see what this means : 5 feet from red hot stoves f ' the thermometer marked 60°, 10 feet from the same stoves on t the floor the thermometer marked 12°, being a loss of 48° in a S distance of 5 feet in length and 2 feet below the sources of ^ heat.' Now at that rate of radiation of heat, how hot must the I sun be to transmit any degree of heat 92 millions of miles , J- through a temperature of — 142° of centigrade to this planet, and not merely to this earth in a column of heat of 8,000 miles in diameter to envelope it, but also to difluse its heat through an ' ellipsoid of ether, whose circumference would be the orbit of the earth around the sun ? But the actual loss of heat in its ^ descent to the earth (if that could be possible, which it cannot f be,) per foot would be immensely more than is stated above,' t as the heat would have to pass -through space chilled to — 142° of centigrade instead of in a rOomheated to +65° of Fahrenheit. Again,"in this latitude of 40° north, we have in our winters I fatls of snow which lie upon the ground sometimes for weeks, I with the sun being unable to make any impression upon it — I and when the snow does begin to melt, it commences with the i: layer of snow in contact wdth the earth, and not with that on [: the upper surface exposed to the sun. Our farmers all know I that when their fields in winter are covered with snoAV, their I growing crops under it are kept warm, though no ray of the t sun could reach them through the snoiw , and they anticipate r therefrom a large yield in the ensuing harvest. If terrestrial ; heat is derived dire'ctiy from the sun, how is this fact explained ? i A gentleman in the State of Maine, during the early part of I the last winter, when the ground at his residence was deeply f covered with snow in many places, made some experiments to [ ascertain the temperature of the earth under the snow. He found that the heat increased at the surface of the earth with the depth of the snow above it. The following is the uccouu*, nz : 40 ^^xpcrinionts wci’e made in the winter of 18^2— ^ 3, with a view to ascertain how far the soil is protected from cold by snow. For fonr successive days in winter, there being four inches in depth of snow on the ground on a level, the average temperature, immediately above the snow, was found to he fourteen degrees of Fahrenheit’s thermometer below zero; immediately beneath the snow in contact with the earth, it was ten degrees above zero; being an increase of twenty-four degrees of temperature, occasioned by a covering of the earth with four inches of suoav; and under a drift of snow two teet deep the temperature Avas tAventy-seven degrees above zero ; making an increase of temperature at the earth’s surface under two feet of snow, of forty-one degrees of Fahrenheit over the Temperature of the air just above the upper surface of the suoav, iso one can pretend that these variations of temperature were derived from the sun. Let us attempt an explanation of this phenomenon. It is thi?. The radiation of heat from the interior of the earth, positively electrilied, meeting at the surface of the earth with ’the snow in contact Avith it, negatively electrified, the conjunction of these opposite polarities of electricity evolves heat, melting the under layer of the snow, irrigating the plants under it Avith water moderately Avarm, and keeping the earth from being frozen, so that in the spring folloAving, when the snow had disappeared, the plants Avere ready_ to receive the stimulating infiuence of sunlight and the blue light of the sky, of Avhich they had been deprived during the winter. Professor Tyndall, Avriting of Avhat he calls solar radiation, sa 5 ^s: “ ilever did I sutfer so much from solar heat, as when descendino- from the corridor io the grand glateau of Mont Blanc on" the 13th of August, 1857. Whilst I sank up to the waist in the snoAV, the sun darted its rays upon me with intolerable fierceness. On entering into the shade of the Dome du Goute, these impressions instantly changed, for the air was as cold as ice. It was not really much colder than the air traversed by the solar rays, and I sutfered not from contact with AA^arrn air but from the stroke of the sun’s rays,_ which reached me after passing through a medium as cold as ice,” It is singular that to so learned and astute a scientist as Pro- fessor Tyndall, it did not occur that if his sensations, so dis- tressino- on this occasion, were derived from the heat of the sun’s fierce rays, that he could not have Avalked through snoAV waist deep, in'^ such heat, without the snoAV becoming melted 41 by the same heat which oppressed him, and that he would have been swept away by the torrent of water thus produced by the melting of the snow by this great heat; but it does not appear that the snow was at all atfectcd by it, while the water was drawn out of the Professor in profuse perspiration. I venture upon an explanation. The heat from which the Professor suffered came from his own body, and was dei’ived from electrical action of sunlight upon his dark woolen clothes, warmed by the animal heat of his system. He was sti-uggling through deep snow in an atmosphere of icy coldness. The natural heat of his body, ninet^’-eight degrees of temperature of Fahrenheit, was greatly increased by the muscular efforts he was maldng in his descent of the glacier. His woolen clothes had become positively electrified by the heat of his body. The strong sunlight of August having passed through the cold, dry ether of planetary space and the upper atmos- phere of the earth, by its friction with them was negatively electrified, and falling upon his warm body and clothes, posi- tively electrified, increased heat was evolved in and around his person, and his sufferings were intensified. As soon as he left the sunlight, his clothes, by induction, became negatively electrified and the temperature of his body was soon lowered, and his sufferings from heat ceased. Again, there is no heat in the moon, which' proves that the moon has not an atmosphere, as it also proves that there is no heat in the sun ; for if there was an atmosphere about the moon the sun’s light penetrating it and producing friction by the contact with it would evolve electricity, which uniting with the opposite electricity of the moon’s atmosphere would produce heat, but no such effect has been perceptible with the most delicate instniments. Besides, if there was heat in the rays of the sunlight, that heat would be reflected with that light from the moon’s surface to the earth, which we know is not the case, JTow, if the sun possessed heat, and could force it down- wards to the earth, which, according to our knowledge of the. laws of heat, is impossible, we could have no clouds in our atmosphere, as from the absorbing power of gases of heat the clouds would be so expanded and attenuated by the absorbed heat that they never could be formed. The sun is a great magnet, as are all the planets of the solar svstem, and it is by their magnetism and not by their weight or gravitation that their motions in tlieir respective ori)its are regulated by the greater magnetism of the sun. Is ow as mag- netic attraction or repulsion varies inversely as the squares oi the distances, svhich relation has been heretofore attributed to gravitation, it is not difficult to assign to magnetism, iii its attraction and repulsion, the forces which have heretofore kepi and now keep our solar system in its various motions, nor need we hesitate to conceive that all the motions of infinite systems, of suns and stars, of nebulas, and cometary and meteoric matter, are in like manner regulated. The meteoric matter whicli. has fallen to the earth, has been found, when examined, to be highly magnetic. If the sun is a magnet, there ts only sufficient heat generated in its interior by opposite electricities to cause its daily rota- fion on its axis, and it- cannot be an incandescent body, since magnetism is destroyed by heat. "Wherever there are differences of temperature, there are opposite electricities-— one electricity being always associated with what is called heat while the opposite electricity accompanies cold. These terms of heat and cold are mere expressions of relative differences in varied temperatures, with- out regard to the intensity of either condition. Professor Tyndall, in his book on “ The Forms of Water in Clouds and Rivers, Ice and Glaciers,” has given what he con- siders explanations of many physical phenomena connected with his subjects, attributing to radiations of solar heat the. changes and transformations Avhich he describes. 'With great deference to so learned and distinguished an authority, I take occasion to offer other explanations of the caipes of the jffienomena alluded to, which seem to me as being more in • accordance with our knowledge of general physics. In his article on “ Mountain Condensers,” he says : “Imagine a southwest wind blowing across the Atlantic towards Ireland. In its passage it charges itself with aqueous vapour. In the south of Ireland it encounters the mountains of Kerry ; the highest of these is Magillicuddy’s Reeks, near Killarney.^ Row the lowest stratum of this Atlantic wind is that which is most fully charged with vapour. When it encounters the base of the Kerry Mountains, it is tilted up and’ fiows bodily over them. Its load of vapour is therefore carried to a height, it expands on reaching the height, it is chilled in consequence of the exoansion, and comes down in copious showers of rain. From 4:0 ■this, ill fact, arises- the luxuriant vegetation of Killarnej; to this indeed, the lakes owe their water supply. The cold crests of the mountain also aid in the work of condensation.” Let us examine this. The tilting up of the masses of cloud on coming in contact with the face of the mountain is the resultant of the impact of two forces, one being that of the wind from the southwest with any given velocity from twenty miles per hour to that of eighty or one hundred miles per hour ; the other, tlye static force of the resistance of the mountain itself ; the diagonal of these two forces is the tilting up of the cloud after impact. ISTow these two great masses of cloud and mountain, oppositely electrified, when they come together in contact produce great friction of their molecules, which friction evolves positive electricity from the higher temperature of the southwest wind; this positive electricity thus evolved rushes into conjunction with the opposite electricity of the atmosphere, producing heat, which heat being absorbed by the air holding the water in suspension communicates to it positive electricity, and the air so electrified is attracted by the negative electricity of the upper atmosphere, carrying it up and by expansion so comminuting the particles of air that they can no longer con- taiti the globules of water they before held in suspension, which latter thus released then begin, being attracted by the positive electricity of the earth, to fall as rain oppositely electrified, and it is, therefore, these electricities thus excited with the heat which is evolved by their conjunction and the rain charged with ammonia and carbonic acid gas which furnish the stimulants to the remarkable vegetation of Killarney. During the prevalence of these rain bearing clouds, driven across the Atlantic by the southwest winds upon the above mentioned mountains, the sun must be obscured by them,' and hence there can be no I’adiations of solar heat to expand the air of the clouds after their impact with the mountains, and they have been tilted up in their further progress over the crests of the mountains. A similar explanation covers the example the Professor gives of a heavy fall of rain or snow in the Alps, while the sky is clear and blue over the plains of Italy — while the wind is bldxcmg ■over the plains to the Alps. The warm wind, positively electrified and holding water in STispension, coming in contact with the negative electricity of the cold Alps, and producing friction by the impact, evolving more positive electricity to combine ■with the negative electricity of the atmosphere at that great * 44 clcvatiou, increases tlie lieat, and by it expands tbe air of the clonds so much that it can no longer hold the globules of water held by it in suspension. The heated and expanded air, attracted to the still higher atmosphere from its greater nega- tive electricitv, separates from the water it before held, A\hile (he water having lost its heat by the superior capacity of the air to absorb it, becomes negatively electrified and is attracted to the earth by its positive electricity — hen'ce the rain fall. Professor Tvndall also states in the same work, “that the nnconfined aii’ heated at the earth’s surface, and ascending by its lio-htness, must expand more and more, the higher it rises in the atmosphere,” and that the ascending “air is chilled by its - expansion. Indeed this chilling is one/Wurce of the coldness of the higher atmospheric regions.” It strikes me that this explanation is not correct. In the first place the ascent of heated air in the upper atmosphere has a limit beyond which it cannot pass. Secondly, it ascends not by its lightness but bv the attraction of the negative electricity of the upper atmosphere for the heated air, ivhich is oppositely electrified. In its upward course it loses its heat by radiation and with it its positive electricity— and by induction becomes negatively electrified with the air whose altitude it has reached— nor is this chilling bv expansion, as he terms it, one source ot the coldness of the upper atmosphere. That coldness associated with negative electricity is derived from the ether m which the atmosphere as well as the earth is continually revolving, that ether has a temperature, according to Fouiliet, ct of Centigrade thermometer, and our upper atmosphere in contact with this ether receives from it, by induction, both its (■old and its negative electricity, and the atmosphere itseii is kept in its place as an envelope of the earth by the positive electricity of the earth and the opposite electricity atmosphm’e. The snow line from the equator, (15,000 feet above the equator to the 60° of north latitiide, where it coincides with the earth,) being the dividing line between these two opposing electricities. . The Professor gives another example of the air being chilled bv its expansion, as follows, viz : “ with a condensing syringe you can force air into, an iron box furnished with a stop cock, to w'hich the syringe is screwed. Do so till the densitj of the air within the box is doubled or trebled. Immediately after this condensation, both the box and the air within it are warm, and can be proved to be so by a proper thermometer, bimply 4 .:= turn the cock and allow the compressed air to stream into the atmosphere. The current, if allowed to strike a thermometer visibly chills it, even the hands feel the chill of the expanding • 5 > air. J^ow for another explanation different from the Professor’s. The air in the iron box had become heated by the friction of it with the sides of the bo.x ; that friction evolved positive electricity associated with the heat; on turning the cock and allowing the heated air to escape into the atmosphere, the heat and the positive electricity both left the escaping air with the velocity of lightning, rushing into the oppositely electrified air in the upper atmosphere, and the air that reached the ther- mometer deprived of its heat i-educed its temperature. There is also an inconsistency in the explanation of the Professor in producing heat by condensation in his iron box, while he produces rain by the condensation of the clouds by cold in the upper atmosphere. This reminds one of the fable of .^soj), in which a satyr invited into a husbandman’s hut, blew upon his hot broth as he said to cool it before eating it, and again blew' his breath upon his fingers to warm them on coming into the house from the cold outside air. The husbandman turned the satyr out of dooi’s, as he could not comprehend how any one could blow hot and cold from the same breath. If compression of the atmosphere produces heat, condensa- tion, which is merely another form of expression for the same thing, cannot produce cold. If cold condenses, why does it not condense the air in the upper atmosphere where the greatest cold prevails, and the air is veiy dry, rarefied and attenuated? According to the theory of condensation by cold, the air should be very much more dense at great elevations above the earth, than it is at the surface of the ocean, but the reverse is known to be the case. The higher in the atmos- phere a balloon, inflated with hydrogen gas, ascends, the more the gas becomes expanded by the rarefaction of the atmos- phere, w’hich shows that the cold of the upper atmosphere cannot condense the gas in opposition to the expansive influ- ence of the rarefied atmosphere at great elevations. Ice water poured into a glass tumbler in the heat of summer, causes a deposit of drops of water on the outside of the tumbler resembling dew, w’hich is the result of a conjunction of opposite electricities, the glass and the air within and around it being warm and positively electrified, while the ice water is negatively electrified. Their conjunction evolves heat, w'hich 46 ia absorbed by the molecules of air, bolding in suspension tbe humidity of the atmosphere ; these molecules, so heated, ascend immediately with inconceivable rapidity into the upper atmos- phere, attracted by its opposite negative electricity, while the globules of water thus released from their suspension in the air on the outside of the glass, being now negatively electrified, are attracted by the vitreous or positive electricity of the glass tumbler and are deposited on it. On the thirty-first day of March, A. D., 1872, I visited my farm to give directions to apply heat to start the growth of the vines in my grapery, at the commencement of the season. The weather was veiy ' cold, patches of ice and snow lay in places on the fields, which the sun, shining with great brilliancy through a remarkably clear atmosphere, was unable to soften or melt. No semblance of cloud or vapour was anywhere visible. In the open air, protected from sunlight, the ther- mometer (Fahrenheit’s) marked 34 degrees, two degrees above the freezing point of water. On entering the grapery, in which there had been no artificial heat from fuel of any kind for the space of nearly a year, mj’ son and myself were astonished at the great heat that there was within it. On examining the thermometer which hung on one of the middle posts of the grapery, completely sheltered from the sunlight, about four ieet from the floor, we were amazed to find that it marked one hundred and ten degrees of Fahrenheit. Here was an increase of seventy-six degrees of temperature over that of the outside air, and produced by a film of glass not exceeding one-six- teenth of an inch in thickness, but associated as blue and plain glass. This extraordinary increase of temperature, mani- fested the supreme wisdom of the Creator in kindling this heat at the surface of the earth, where it was needed, by rays of light passing through a denser medium than air, instead of sending heat from the sun through ninety-two millions of miles of ether at a temperature of —142 degrees of Centigrade thermometer, in the passage through wdiich so much of the said heat would have been lost by radiation. I have had many occasions to observe since that date, that during the passage of strong sunlight through the blue and plain ”glass of the grapery, the temperature through the day, within the grapery^ varied from one hundred degrees to one hundred and fifteen degrees, while that without, according to the seasons of the year, at the same times of the day would range from thirty-two degrees upward to sixty degrees or sixty -five degrees. 47 During the winter of 1871 and 1872, which, in this city, was a very cold and rigourous one, two ladies of my family residing on the nortlieru side of Spruce streets cast of Broad street, in this city, who, at my suggestion, had caused blue glass to be placed in one of the windows of their dwelling, associated with plain glass, informed me that they hful ol)served that when the sun shone through those associated glasses in their window, the temperature of the room, though in mid-winter, was so much increased that on many occasioTis they had been obliged during sunlight to dispense entirely with the .fire which, ordinarily, they^kept in their room, or when the fire was suffered to remain, they found it necessary to_ lower the upper sashes of their windows, wdrich were wdthout the. blue glass, in order to moderate the oppressive heat. ii- ^ These examples go to illustrate the remark of a distinguished (derman scientist, made to a friend of mine after he had read an account ot my experiments with blue light on animal and vegetable life. He said, “ that the discovery o"f this extraordinary influence was destined to produce the most important and beneficial results on the comfort and happiness of mankind throughout the civilized world. That fuel was everywhere recognized as one of the most indispensable elements of social and domestic economy. That it is, particularly in Europe, very expensive from its scarcity, which is becoming greater every year with its annual consumption, and in the^'narthern parts of Europe, furs, skiiTs of animals and the down of aquatic birds are extensively worn, sometimes with two or three suits at once ot clothing, in order to preserve the animal heat of the body, owing to the great costliness of fuel and the severity of the cold. “ That even in England, apprehensions are being expressed of an exhaustion of their coal mines in the not distant future. Now since this wonderful discovery of General Pleasonton, of the influence of the blue light of the sky in developing animal and vegetable life, which is largely due to the heat and elec- tricitv developed by the passage of sunlight through these associated blue and plain glasses, I am of the opinion that during sunshine, for many hours in the day, by means of blue and colourless glass arranged together in*^ doors and windows exposed to the sun, sufficient heat can be evolved to enable families, and work people in factories, to dispense with a large proportion of the fuel that they have heretofore been oblio-ed 4:- to use. Let us suy that ono-lnilf of the fuel heretofore required, can be saved by thus utilizing sunlight, and von will begin to comprehend how vast will be the bencltt derived to mankind in the economy of fuel alone, by this discovery of General Pleasonton.” • I have said that while the rays of the sun’s light were one of the causes of terrestrial heat, yet there is no heat in them.. This can be proved by any one, in the follo^ving experiment, viz: During winter, when the ground is covered with snow, and the temperature of the open air is at zero of Fahrenheit’s thermometer, it will be found that the sun, however brightly shining, cannot melt the snow or ice on which it may shine. Take now a piece of black or brown silken or woolen cloth oi’ any form and of convenient size, and place it on the snow in the shade where the sun does not reach it with his rays. Tin- snow will not be melted under this cloth, which will have th< same temperature as the snow ; hence it is'obvious that therf is' no heat either in the sunlight which could not melt the snow, nor in the coloured cloth whose temperature was the saine as the shaded snow on which it had been placed ; now take up the cloth, and place it on the snow where the sun can shine upon it. Let us observe the effect of thi.s new position : the rays of the sun moving with a velocity of 186,000 mile.s per second are suddenly arrested by this cloth, which they cannot penetrate. This sudden stoppage of velocity produces friction, by the impact of the rays of light upon the cloth; electricity is evolved by the friction, having a polarity opposed to that of the cloth; instantly these opposite electricities rush together, pi’oducing heat, warming the cloth and melting the snow immediately under the cloth, by which the cloth begins to sink below the level of the snow, and if it shall be allowed to remain, it will melt the snow under it till the cloth shall rest upon the ground beneath, clear of the snow, and the sur- rounding snow shall enclose the cloth, of its exact size and form. From this experiment, we conclude that the heat which melted the snow under the cloth was not derived from the sun as heat, but that the electricity produced by the impact of the sun’s rays with the cloth oppositely electrified, through friction, evolved the heat which melted fhe snow. Ffow suppose that instead of a single piece- of this cloth having been placed upon the snow, you have put a series of pieces 49 of the same cloth upon the snow. The same principle applies hut a different action is observed. The cloth is a bad con- ductor of heat as well as of electricity, consecpiently the heat evolved bv the conjunction of the opposite electricities produced by the friction of the rays of sunlig-ht by impact on the cloth with the opposite electricity of the cloth, cannot descend through the cloth to an}- depth, being contrary to the laws of heat, but it immediately ascends into the atmosphere and escapes, vehile the edges of the series of pieces of cloth in ■contact with the snow become warmed by the conjunction of the opposite electricities, produced by the friction of the ravs of light with the edges of the cloth and the cloth’s electricity, and soon melt the snow in contact with them, till the pieces of cloth are left high and dry above the snow which surrounds them. Glaciers— their Origin, Fosition, Duration, Changes and Move- Much has been written on these subjects, and many distinguished scientists have been greatly exercised to give a satisfactory explanation of the phenomena they have witnessed in connection with them. It seems to me that glaciers are formed in the regions of perpetual snow by the deposition of snow in the valleys of the lofty mountains where, they exist; clouds laden with vapour wdien they reach the^ neighbourhood of the mountains whose valleys are filled with glaciers, being positively electrified encounter the negative electricity of the higher atmosphere. These opposite electricities meet in conjunction,^ heat is evolved the air associated with water as vapour in the clouds being thus heated, is rarefied and expanded to such an extent that it can no longer retain its water, (while it ascends rapidlr into the upper atmosphere attracted bi’ its negative electricit}' ) which on being liberated from the air that held it as vapour is converted by the surrounding low temperature of its great altitude into flakes of snow, which having an opposite magnetism to the earth are attracted downward to it, and are at the same time repelled from the height where they are formed by the opposite magnetism pre%miling there. The crystallization of these snow flakes is made in a vacuum, produced by the escape of this heated and rarefied air, and by absorbing the magnetism which is developed by the con- junction of the opposite electricities of the clouds and the atmosphere as they come together in contact, these mao-netic snow flakes transfer it to the-earth to replace the macrnetism ■which is constantly leaving the earth in evaporations to escape into the upper atmosphere. This, then, in all probability, is the origin of glaciers. The successive snow falls in the upper valleys of tliese elevated regions, by their magnetic attraction to the earth, serve to' pack the snow, and to compress the lower portions of it into ice of greater or less density, according to its elevation in the atmosphere and the depth of the valleys in which the glaciers are formed. The effect, therefore, is that the bottom of the glacier is ice, while the upper part of it is snow, termed neve. Crevasses are .fissures of various depths and widths in the glacier, whose formation Professor Tyndall attributes to the effect of the solar radiation of heat upon the glaciers. lie says, in his book on “ The Forms of "Water,” &c., page 100, “first, then, you arc to know that the air of our atmosphere is hardly heated at all b,y the rays of the sun, whether visible or invisible ; the air is highly transparent to all kinds of rays, and it is only the scanty fraction to which it is not transparent that expend their force in warming it.” I have shown that heat ascends in our atmosphere by the attraction of the positive electricity Avith which it is always associated, by the negative electricity of the colder air in the upper regions of the atmosphere, and by its repulsion from the earth by its positive electricity ; it is, therefore, contrary to the laws of heat that the , sun should, can or could transmit ra;js of heat downward to this planet, and as these heat raA^s can not be so transmitted, they are therefore not present to bo absorl.ied by the snoAV of the glacier or on the mountains. On page 98 of the same book, he says: “ we have wrapped up our chain and are turning homewards after a hard day’s work upon the Glacier du Geant, Avhen under our feet, as if coming from the body of the glacier, an explosion is heard. Somewhat startled, Ave look inrpiiringly over the ice. The sound is repeated, seAmral shots being fired in cpiick succession. They seem sometimes to our right, sometimes to our left, giving the impression that the glacier is breaking up, still nothing is to be seen. “"We closely scan the ice, and after an hour’s strict search Ave discover the cause of the reports. They announce the bii’th of a crevasse. Through a pool upon the glacier, we notice air bubbles ascending, and find the bottom of the pool 51 tTossed bj a nan-ovv crack, from which the bubbles issue, mght and left from, this pool, we trace the young fissure tbrough long distanees. It is sometimes almost too feeble tO' >e seen, and at no place is it wide enough to admit a knife- blade. It is difficult to believe that the formidable fissures, amono" which you and I have so often trodden with awe, should vjmmence in this small way. Such, however, is the case, i ho great and gaping chasms on and above the icefalls of the (:reant and the Taletre begin as narrow cracks, which open ,gi'adually to crevasses. The crevasses are grandest on the higher neves, where they, sometimes appear as long yawning Assures, and sometimes as chasms of irregular outline ; delic(de him light shimmers from them, but this is gradually lost in the. darkness ot their profounder portions. Over the edges of the chasms, and mostly over the southern' edps,_ hang a coping of snow, and from this depend like stalactites, rows of transparent icicles, ten, twenty, thirty feet pendent spears constitute one of the most beau- tiful features of the higher crevasses. How are they produced ?’ hvideutly by the thawing of the snow. -But ivhv, when once thawed, should the water freeze again to solid spears ?” Hovv let us examine this ; if the supposed heat of the sun’s rays,, could melt the snow at the southern edges of the crevasse, why did not similar rays from the sun, conveying the like^ temperature, melt the general surface of the glacier, and. profluce thereby -large pools of water on the surface of the glacier ? Particularly, as the Professor states, “ that the suow on which the sunbeams fall, absorbs the solar heat, and on a- sunny day, you may see the summits of the high Alps glisten- ing with the water of liquefaction. The air above, and around the mountains niay, at the same time, be many degrees below the freezing point in temperature.” If the surface of the snow on the mountains was melted by the solar heat, as the Professor supposes, what was there to arrest the .streams of water thus produced, and to prevent them from .flowing into the valleys occupied by the glaciers, and converting the glaciers themselves into mountain torrents, while at the same time the mountains were being denuded of snow? But we know that such results have not been pro- duced. Above the snow line the mountains are perpetually covered with snow, and the glaciers have remained from a remote antiquity to attest that the snow does not absorb tlie heat of the sunbeams, foi’ the simple I’cason that the sun- beams in themselves do not bring any heat from the sun to this planet. In my early boyhood, I dwelt on the banks of the Potomac, a river fancifully named by the Indians, before the advent of the white man, '‘ the river of swans,” from the abundance of that water fowl that frequented- its waters. Well do I remember, lying awake on the eve of our several winter holidays, when the river was deeply frozen, anticipating a day of s})len(lid skating on the morrow,’ to have been often startled by the noise of a great explosion of the ice on the river, ■occasioned by the compression of the air beneath the ice, as the Tide rising rapidly forced it upwards between the water .and the iee, till its accumulation and compression would over- cojne the re.'sistance of the ice, and a iissure would be opened in it extending sometimes for miles, and liberating the pent up air into the atmosphere. If the temperature of the night air was l)elow the freezing point of water, as the tide receded the water which had filled the fissure, when the tide was full, was frozen into ice, and the track of the fissure could be marked on the next day by the film of thin ice that had been formed in it, as the tide was recediim the nis-ht before. In this way, air holes, so dangerous to travelers and skaters on the ice, are constantly formed on our rivers and streams, •subject to the flow of the tides, and in lakes and mountain .•streams, they are also formed by the currents of water flowing tlownwards in a similar manner. In my later youth, I had' observed similar effects from similar causes, produced on the ice of the river Hudson, at West Point. In short, fissures on the surface of anything, whether on the surface of the earth by volcanic eruptions in which lava, rocks, scorite, mud, boiling Avater, are thrown out from ' the iiiterior, or by Geysers spouting their hot streams into the atmosphere, or the cracks in the ground produced by long continued droughts, evapo- rating the moisture contained in the soil, and even eruptive diseases among mankind or other animals whether wild or domestic, are all the results of interior forces, acting from the' interior to their respectiAm surfaces. . Hoav let us explain the crevasse on the glacier. The snow falls carry to the glacier large quantities of atmospheric air, Avhich are confined between the glacier and the snow as it falls; every fall of snow presses its predecessors and the air they contain closer together against the ice. filling its 53 vacancies with air. This column of air, thus pressed down upon and into the ice, encounters the air which has been enclosed between the bottom of the glacier and the earth on which the glacier rests, — this last mentioned air has been warmed by the radiation of heat from the interior of the earth, and has become positively electrified by it — the contact of this positively electrified air with the negativelj'^ electrified ice of the bottom of the glacier.* evolves more heat, which, melting the lower stratum of ice of the glacier, constitutes the source of the stream of water that flows from the glacier. Such is the origin of the river Ehone. This warm air, in its effort to rise through the glacier into the upper atrnosphere negatively electrified, meets in the crevices everywhere abounding in the ice of the glacier^ the air which has been forced down by the snow falls, and which last air is negatively electrified; the coninnction of these two airs oppositely electrified evolves heat, which expanding the air, displaces the ice of ' the glacier, foi’ming channels for its escape into the upper atmosphere, and when it reaches the upper surface of the glacier, forces its way' through it into the atmosphere in that .minute fissure, which Professor Tyndall had such difficulty to discover; Again, this warm air as it escaped into the atmosphere, melted the edges of the ice or snow at the surface through which it passed, and through which it was visible in the air bubbles Professor T. described. The melting of the lower stratum of ice of the glacier in contact with the earth produced by the heat evolved by the conjunction of the positive electricity of the. earth with the negative electricity of the ice, is the cause of the subsidence of the body of the' glacier, and the declivity of the valley itself is the cause of the glacier moving bodily downward in it. The fractures, strains, torsions of certain portipns of the glacier are the results of the forces of expansion and contraction in the interior of the glacier, produced by variations of its interior temoerature as mentioned above. In this country, the winter of the years 1874 and 1875 has been an exceptional one. The cold has been of long, and almost uninterrupted continuance, and of great seterity. The rivers in the 5liddle and Eastern States have been closed with ice, which has been of great density and depth, extending in some of their courses through the mountains even to the beds of their streams. The frozen condition of the waters has 54 rcniained till lute in tiie sprint season; and from the aecumn- lulion of immense masses office in certain portions of these rivers, forming what were called ice-gorges, filling their entire widtli for the distance of miles in lengtli, the most serious apprehensions were entertained of extraordinary damages to towns and villages, railways and canals, in the valleys of these rivers, that would he sustained hy the sudden breaking up of these gorges of ice from rain-storm’s, and the melting of the snows on the mountains, which would produce the most extensive and alarming inundations. These apprehensions were justified by the advanced spring season which usnallv, ' by its increased temperature, terminates the rigours of winter. To obviate, if possible, these threatened dangers and calami- ties by the sudden In-eaking up of the ice, various expedients Avere resorted to, viz : cutting chamiels through the ice below the gorges, to liberate the Avater above, should it assume alarming proportions ; attempting to destroy tlie gorges thom- seh^es by the explosions of gunpoAvder, or of nitro-glycerine, confined in chambers in the ice itself, and one very liberal gogtleman, evidently a believer in the theory that the sun is an incandescent body and sends its heat bodily to our earth, dowiiAvards, presented to the authorities of one of the towns e^-dangered by the ice-gorge in its neighbourliood, tAventy- eight barrels of ISTaphtha, to be burnt on the ice-gorge, under the impression that the heat produced by their combustion, would descend through the ice, and liquefy it into water. It is scarcely necessary 'to add, ' that, AA^hen "the experiment of burning the Kajihtha upon the ice-gorge was tried, tlie heat evolved by its combustion immediately ascended into the upper atmosphere, leaving the, ice unaffected by the experi- ment. F rom a very interesting book entitled, “ IMount Washington in Winter ; or, the Experiences of a Scientific Expedition uj>on the Highest Mountain in Xew England — 1870-71,” pnblislicd in Boston in 1871, we make some extracts that seem to. have a connection Avith the subjects of Avhich Ave are treating. “ Mo.osilauke Mountain, near IMount Washington, is nearly fiive thousand feet high, and lies Avithin the arctic zone of climate. It was on this mountain that tAA'o scientific gentle- men, viz., Messrs. A. F. Clough and II. A. Kimball, deter- nAined to pass tAvo months, in the winter of the years 1869 atid 1870. in order to fit themseh’-es the better for a Avinter residence on Mount Washington, at a future day. They attempted the ascent of the mountain on ISTovember 23d, 1869, but were driven hack by the severity of the weather. On the 31st of December, 1869, the attempt was renewed under better auspices, and was successful. “About two months were spent by them on this summit. So valuable were the experiences acquired, and so unusual were the meteorological phenomena observed, that the Mount Washington phenomena, subsequently experienced, have not equaled those upon Mount Moosilauke, and among them the possibility of living on a mountain top during the winter, was fully demousti'ated. “ There is scarcely a mountain in Xew England from which the view is more extejasive. We can see from it, nearly the whole of the State of ISTew Hampshire, avith its numerous mountain peaks. Eastward is Mount Washington, in solemn repose, — its neighbouring peaks of immaculate whiteness — Momit .Lafayette and its lines of white extending far, down into the evergreen forests. Southward is Lake Winnipiseogee, with its numerous isles, glittering in the sunliglit, like a gem of the purest water. W estward is the whole State of Y ermont, and Ascutney, the most pointed of its mountains, is conspicu- ous. Moosilauke is so muck higher than the immediate neighbouring peaks, that the whole country is spread out as a grand intrusive raised map before the- beholder. “ Ho scene more grand and beautiful ever greeted the eye of man, than when, beyond the dark band of clouds just below the summits of the Franconia and White mountains, appeared those tints of rose and orange, lying along the horizon just above the snow capped summit of Mount Washington, and against a deep azure sky. From Moosilauke, you command the whole panorama of the White Mountain range, and you may see something of the effect witnessed among the Alps. As the day dies, the lost shadows pass with strange rapidity from peak to peak, vanishing from one height as they appear on the next.” The following are extracts from their.Journal, viz : “ On the 1st of January, 1870, the sun rose clear. We were above the clouds, and a grander spectacle one does not often behold. Tlie clouds seemed to roll and surge like the billows of the ocean. They were of every dark and of every brilliant hue ; o6 Lore they were resplendent .with golden light, and there of silvery brightness; here of rosy tints, there of sombre gray, here of snowy whiteness, there of murky darkness, here gorgeous .with the play of colours, and there, the lurid light ha.shcs deep down into the gulfs formed by the eddying mist. But above all these clouds, these fla.shes of light, this darkness, rise in stately grandeur, the summits of Mount AVashington, sublime in its canopy of snow, and of Lafoj'ette, with a few peaks of lesser altitude, glittering in the bright sunlight. As the sun rises higlicr, the picture fades away, the whole country is flooded with light. “ Did this grandeur, this magTiilicence, this brilliant display ■•flights, of sluidows, and shades — of these clouds, so resplen- dent, so beautiful, portend a storm? In the evening the Avind '•hanged to the southeast, and increased in velocit\ . “ At daylight on the 2d of Tanuary, 1S70, it Avas snoAving. . This soon changed to sleet, and then to rain, and at eight o’clock, A. AI., the velocity of the wind aauas seventy miles per hour; at tAvelve o’clock, noon, there Avas a perfect tempest. - Although thcAvind Avas so fearful, yet Air. Clough Avas determined to knoAv the exact rate at AA'hich it aa’US bloAving. By clinging to the rock, he succeeded in reaching a place where he could expose the anemometer, and not be'bloAvn aAvay himself. Re found the velocity of the Avind to be ninety-seven and a half miles per hour, the greatest velocity, until that time, ever recorded. AVhen he reached the house, he Avas thoroughly .saturated Avith AA’-ater, thcAvind having driven the rain thi'ough every garment, although they Avere ot‘ the heaA-iest material, as though they had been made of the lightest fabric' During the afternoon, the rain and gale continued Avith unabated violence. The rain Avas driA’-cu through every crack and crevice of the house and the floor of our room Avas flooded. So flerce Avas the drauglit of the stove, that the wind literally took aAvay every spark of fire, leaAung only the half charred wood in the stove, and it Avas Avith the greatest dilficulty that Ave succeeded in re-kindling it. During the evening, the Avind seemed to increase in fury, and although theAvindovvAvas BomcAvliat protected, yet nearly every glass in it, that Avas exposed, Avas broken by the pressure of the gale. As the lights Avere broken, the fire Avas again extin- guished, and even my hurricaiAC lantern Avas blown out as quickly as if the flame had been unprotected. * * * * After nine o’clock, P. AI., there were occasional lulls in. the storm, and by midnight it had considerably abated. “ TVlien it was clear, there was a strong temptation, notwith- standing the cold, to he out of doors to watch the clouds, at first of almost fiery redness, then changing to, gray and neutral tints, until almost black, they seemed to gather around some distant peak, or as a dark band, they lay between the Franco- nia and hite ^lountains, leaving only the snow-clad summits above the dark border; or at sunset, when they lay in narrow bands, or rose tinted clusters around the summit of Mount ^ i^hin^ton, while elsewhere they were those of leaden hue, such as are seen only in winter. Often when the sky is par- tiallj' overcast, through the intervening spaces of the clouds, we see that intense blue sky, which is peculiar to high altitudes. _ “ On the 19th of February, 1870, there were two currents of air, the upper had its lowest stratum probably two thousand feet below the summit. In the morning the upper current was northwest, with a velocity of fifty miles per hour ; about noon, the wind changed to the north and increased in velocity, a,ud at five o’clock, P. M., it had a velocity of seventy miles- per hour. At the foot of the mountain, nearly 5000 feet below there was scarcely a perceptible breeze, yet up, a thousand feet, there was a strong current from the southioest, and the clouds seem to move almost as rapidly as those from the north, higher up the mountain. On account of the velocity of the wind, and the upward pressure of the currents below, .the etfect was remarkable. The. whole country, except the higher summits, was covered with clouds, and these were moving at the rate, probably, of more than sixty miles per hour, and everywhere they were broken into seething, undulating masses, for as they came near the mountains, in an instant, almost, they would be lifted more than a thousand feet, to be carried over the summits. As far as the eye could reach, embracing thousands of square miles, Avas this rolling tumultuous mass of clouds.” These gentlemen left the Moosilauke mountain on the last day ot February, A. I),, 1870. It was extremely cold, wind GO to 70 miles per hour, thermometer ranging from 0 degrees to —17 degrees. The complete organization of the expedition to pass the winter of the years 187,0 and 1871, on Mount 'Wash- ington, "was as follows, viz : ■ C. H. Hitchcock, State Geologist, J. II. Huntington, in charge of the Observatory upon the mountain. S. A. Helson, Observer. A. F. Clough and H. A. Kimball, Photographers. Theodore Smith, Observer and Telegrapher for the United States Signal Service. “Mount Washington, in the ^Whte Mountains in New Hampshire, is in latitude44 degrees 16 minutes 25 seconds north and in longitude from Greenwich 71 degree.'^ 16 minutes 26 seconds west, or 1 degree 0 minutes 43.99 seconds of longitude east from Hanover in New Hampshire. “Its elevation above tide water is 6,293 feet, and in altitude it is the second highest mountain northward, of the Gulf oi‘ Iklexieo, the highest mountain thereof being Clingman’s Peak, in the State of North Carolina, which is 6,707 feet above tide water. “ The limit of the growth of trees on the north side of Mount Washington, is 4,150 feet above tide water. “The climate of Mount Washington corresponds with that of the middle of Greenland, about seventy degrees of north latitude, or 26° further north than New Hampshire. “It is an arctic island (so to speak) in the Temperate Zone, and on account of its great elevation it exhibits also the ct)ii- dition of the atmosphere, where the mercury does not rise above 24 inches in the barometer. For peculiar interest therefore, the Mount Washington Station is not exceeded by any point within the arctic circle.” Professor Edward Tuckerm'an, of Amherst, Massachusetts, in his admirable treatise upon “the Vegetation of the White Mountains,” marks out four regions: first, the lower forest, in which are found the hard wood species of trees, the rock maple, the- beech, the white and yellow birches; with these are often large white pines, firs, white spruces, the aspen, the witch hazel and the mountain ash. “ In the second region, the upper forest consists mostly of black spruce and fir, with occasional yellow' and canoe birches, Frazer’s balsam fir and a mountain . ash : at 4,000 feet of altitude these trees are dwarfed but are very strong, and w'hen close together form a thicket almost impenetrable. , “ Among the plants of the third or sub-aljnne region are the mountain sandwort, the evergreen cowberry, the Labrador tea and the mountain bilberry. This seems not to be well charac- terized- “The foux-th and highest region is called alpine^ and con- tains many plants peculiar to Labrador and Greenland. There ax’e some fifty or sixty of these, and among them are as many more lowland species which have emigrated to the summit and manage to live there in favourable seasons, though often much dwarfed. The lichens are very conspicuous and beauti- ful, one of a sulphur yellow colour is quite noticeable, and is a good indication of the visitor’s arrival in the Alpine District. Another is the reindeer moss, a very common article of food for the most useful animal to man in Lapland. The best localities of these arctic plants are in the great gulfs or ravines, upon the east side of Mount Washington. “ As far as- the upper limit of trees, boulders that have been transported by the glacial drift from more northern summits are common. They rapidly diminish in number and size upon that point, and have not been seen far above the fourth water- tank, or above an altitude of 5,800 feet. “It winter weather on Mount Washington in Octobei'. Most of the necessary preparations ha\ung been made on November 12th, 1870, Mr. Huntington promptly climbed Mount Washington and commenced to take and recoi’d the meteorological observations. The other members of the party Avere delayed by various reasons — but on the 30th of November, 1870, four gentlemen of the pax’ty, viz : Charles B. Cheney, of- Oxford, A. F. Clough, of Warren, C. F. Bi'acy, of Warren, and HoAvard A. Kimball, of Concord, ari’Wed at the summit, and on the 4th of December, 1870, Sergeant Theodore Smith, of the U. S. Signal Service, detailed as an observer, joined the party, “ KoA^ember was making its exit in what might be ternxed a lovely winter day, and the prospect of so choice a time to make our ascent, toilsome at best at this season, and A-ei'y hazardous except at special times in good Aveather, inspired us with enthusiasm more and more increased as we approached the final reach that stood in defiance of any aid that could be rendered by the panting steeds that noAV bore us forward. “ At Marshfield Ave are three miles from the summit, and at present all travel. over this distance must depend- solely upon Inxman ■ muscle and energy to achieve. At this point Ave decided to make the ascent at once, though there Avere serious misgivings on the part of some of us in vicAv of the near approach of night, Avhich at this season, half-fast two o’clock. CO P. M., leaves a small margin of the day, at best for such a task as stood before us. In ascending from this point we to lowed the railroad track. We were compelled to walk upon the ties for the snow was several feet deep, with a sharp upward grade in some places rising one foot in three, with the ties three feet apart and loaded with ice and snow and built on trestle work\ over gorges of some 25 or 30 feet in depth; the careless eager steps of unbaffled enthusiasm, are soon compelled to give place to great caution and the constant stress of nerve and muscle % * * * The end of the first mile carrying us up to within one half mile of the limit of wood growth, found us in tolerable condition, when a halt for breath and ob- servations discovered to us an approaching storm Ijing on the Orceii Mountains of Vermont. It would iindoubtedly strike us but we still hoped we might press on and reach the summit first The thought of being overtaken by a furious storm on the wintry, shelterless clitfs of Mount Washington, \yith the nif'’ht about to enshroud us, w'as fearfully impressive, and prompted us to our best endeavours. With all the eftort we could well muster, we had only advanced a half mile more, cari-yino- us fairly above the wooded region to. the toot ot ‘ Jacob’s Ladder,’ when the storm struck us. There were suddenly wrapped around us dense clouds of frozen vapour, driven so furiously into our faces by the raging winds as to threaten suffocation. The cheering repose of the elements, but a moment before, -had now given place to what might well be felt as the power and hoarse rage of a thousand tunes, and the shroud of darkness that was, in a moment thrown over us was nearly equal to that of the moonless night. Compelled to redoubled efforts to keep our feet and make proper advance, we struggled with the tempest, though with such odds against us that we were repeatedly slipping and getting painful bruises. Mr. Kimball finding himself too much exhausted to continue this struggle on the track, we all halted in brief con- sultation — during which Mr. Clough suggested that our only hope consisted in pushing upward with all our might. “Here we became separated, three of our party left the track, and Mr. Kimball willingly left behind his baggage in order to continue the ascent. By thus leaving the track, we escape liability to falls and bruises, but found ourselves often getting buried to our ivaist in snow, and forced to e^^t our . ^f^ost strength to drag ourselves out. and advance. We repeatedly called to Mr. Bracy, who had kept on the track as we supposed, but oould get no answer. The roar of the tempest overcame G1 our utmost vocal efforts, and the clouds of frozen vapour that lashed us so furiously as it hugged us in its chilling embrace, was so dense that no object could he seen at a distance of ten paces. Against such remorseless blasts no human being could keep integrity of muscle and remain erect. We could only go on together a little wa}' and then throw ourselves down for a few moments to recover breath and strength. We had many times repeated this, when Mr. Kimball became so utterly , exhausted as to make it impossible to take another step. He called to the others to leave and save themselves if possible. The noble and emphatic ‘ never,’ uttered by the manly Clough, whose sturdy muscle Avas found ample to hack his will, aroused him to another effort. . , “The two stronger gentlemen, whose habits of life and superior physical powers gave hope of deliverance for them- selves, were both immovable in the determination that our fate should he one, let that be what it must. “The situation was one of most momentous peril, especially as to Mr. Kimball, whose exhaustion was so extreme that he was wholly indifferent to the fate that seem to impend, only begging that he might be left to that sleep, from whose embrace there was felt nopoAver of resistance. Still there Avas a listless drag onAvard mostly in the interests of his compan- ions, and in obedience to their potent Avills. After this sort we struggled on a few rods at a time, falling together betAveen each eftbi’t to rest and gain new strength. At each halt Messrs. Clough and Cheney used their best endeavours by pounding and rubbing Mr. Kimball’s feet and limbs, and in various other Avays endeavoured to promote circulation and prevent freezing. The last saving device AA’as supplied by a cord, Avhich Ave chanced to have, and the end of this was made a noose, A\"hich was placed in Mr. Kimball’s hand, Avhile the other end Avas passed over the shoulder of Mr. Clough, who tugged along in advance while IMr. Cheney helped at his side. Most of the last mile was accomplished in this manner. “ With the Avind at 70 miles per hour and the thermometer down to 7°, as Avas fpund after arriA'ing at the Observatory, we came at length to ‘ Lizzie . Bourne’s Monument,’ only thirty rods from the Observatory. One of our party shouted an exultant hurrah at the glad sight of this rude pile, Avhich was erected to commemorate the sad fate of one aaLo Avas overtaken by the darkness and heAAuldering fogs and chills of a rude October night. ‘Then,’ in the AAmrds of the eloquent StaiT King, ‘tvas the time to feel the meaning of that pile of 8tonc3, which tells where Miss Bourne, overtaken by night and fog, and exhausted by cold, breathed out her life into the bleak cloud.’ “ It took more than a half hour’s time to miake this last thirty rods. Even the stronger ones had become wearied by their unusual exertions, and had not this been the case, their progress would have been slow, for it was found absolutely impossible to force on the one who had become unable to regard his own peril more than a few feet at a time. lie would then sink down into a deep sleep, while the others would employ the time in chafing his hands and feet, and after a few' moments manage to arouse him and make another struggle onward. “From Lizzie Bourne’s Monument to the summit, Mr. Kimball was mostly insensible to passing events, and only awoke to clear consciousness, as from a dream, io find himself in bed in a comfortable room in the Observatory building, safe from the dreadful tempest, and owing his life to the unyield- ing devotion of these brave men w'ho scornlid: to save them- selves at the expense of a comrade left tos^phrieh. Mr. Bracy, who had got separated from us during ouri, earlier struggles,, had got in about 7 o’clock, P. M., our own Wrival being at 7^ o’clock, P. M. He had kept on the track. “ Thus at least three hours of this ascent were made amid the dai’kness of a moonless night in the howding tempest, the horrors of which will be more readily appreciated when it is remembered that a wind of 45 miles per hour blew down buildings and uprooted trees in Hew York City. Twenty- five miles per hour added make a most fearful hurricane. We were abundantly supplied with nourishment on our ascent,, chiefiy in the form of a strong decoction of tea, of which w’e occasionally partook. This is found to be by far the most potent and effective stimulant that can be used in such con- ditions of extreme exposure. “Mr. Huntington, aroused by the arrival of Mr. Bracy, sallied out with a lantern in search of us, hut found his best exertions of little avail, the storm being so fierce and thick, he could neither make himself seen nor heard beyond a few paces, and they were regarding us as probably lost, though they were pre- paring for another effort in our behalf, when we arrived. 63 “A sleepless uight gave place at length to a day thick and stormy, and for several days the clouds gathered densely around us, and the storm continued to rage, during which we were recovering from ‘ the wear and tear’ of our adventures, and recruiting for the work in store for us.” The railroad depot, in a part of which this party passed the winter of 1871, was a wooden unfinished building, sixty feet long by twenty-two feet wide and stands nearly , north and south. It has eleven feet posts and the elevation of the ridge pole is twenty-five feet, the roof of the usual form in ordinary buildings. The apartment occupied by the party is situated in the southwest corner, of this building. It is a room about twenty feet long, eleven feet wide and eight feet high, The large part of the depot forms a sort of vestibule to this roomv and is wholly inclpsed except at' the easterly end of the northern face, where the outer door is situated. An extract from Mr. Kimball’s diary, reads: “December 5th, 1870. The day is beautiful, we are perfectly comfortable outside without overcoats, and on the east side of the Observatory, the frost is thawing quite rapidly. Thermometer 22° Fahrenheit.” jSTow Avhy, Avith-the thermometer at 22°, should the thaAving of the frost be confined to the east side. of the Observatory, when the sun was shining all around the building on the suoav or Irost Avithout thawing it elscAAdiere away from the building? If the thaAving Avas the result of the heat rays of the sun, so improperly termed, Avhy Avas not the thaAving general all over the summit of the mountain, instead of being confined to one locality ? The explanation, I think, is this, viz : the early morning rays of . sunlight being nearly horizontal, impinged with a velocity of 186,000 miles per second perpendicularly on the vertical Avail of the Observatory, partly covered 'with frost Avork ; great fx’iction AAms produced by the impact and positive electricity eAmlved ; this electricity rushing to the conjunction or embrace of the negative electxucity of the frost work, Avhen in contact AA'ith it developed heat which thaAved the frost Avork over the other parts of the summit of the mountain ; these morning rays of sunlight either passed horizontally or fell upon them Avith such small angles of ixxcideixce, as to be Avholly reflected into the upper atmosphere. Mr. Kixnball continues : “ Ave have succeeded in making some G4 Tery good (pliotograpliic) views, but not as large a variety as we intend to have before we complete our winter’s worlc. * * * "We have also made three negatives of clouds, which wore at least half a mile below us. They resemble the Avaves on the ocean, only the cloud waves are iu some places twenty or thirty miles long. They pass over a range of mountains, and take a long SAveep across the valleys and then rise over the mountains on the opposite ; and as a general thing,' after passing over and coming doAAm on the other side, they break up in small clustei’s resembling, on a grand scale, the surf from breaking Avaves. 'Wo have made some photographs of this. * * * All these clouds move rapidly from the south- Avest, probably at a velocity of forty miles an hour, AAddle on this summit, it blows generally from the iiorthAvest. W e have made a vieAV w^hich shows a small portion of a remarkable cloud effect or phenomenon, It was like a parallel belt on the distant horizon, Avhose circuit must have been more than a thousand miles. It resembled the tire of an immense cart- AAdieel, (Ave occupying the place for the hub,) Avhich was beyond and encircled all the lakes, mountains, &c. It was even beyond Mount Katahdin— at the south, its upper edge Avas parallel with the point farthest north. At noon it appears to be approaching irs as a.centre, and as it nears us, it breaks up in magnificent great thunderhcads, minus the thunder, — all this time our vieAA’’ is becoming more limited. * * * All this time it was snowing beloAV, but we knew nothing of it until night. Our view of the surrounding moun-tains lasts only a short time longer, for Ave see to the AA’est thick heaA^y clouds, marching upon us, a)nd by 4 o’clock, we become densely shrouded — AA'e cannot see Tip Top House from the Observatory not many feet distant. “Hecembcr 12th, 1870. This morning the Avind was south, but changed to the northwest in the afternoon ; at ten, A. M., there AA'as a bow in the clouds, and at noon there Ave-re in ad- dition three, supernumerarv bows Avhich remained for an hour and a half, and some of the time they were remarkably distinct. Late, in the afternoon the sky Avas intensely blue.’^ From their journal we make the following extracts, viz ; “December 21st, 1870. Messrs. Kimball and Thompson (a visitor,) took an observation from the roof of the Tip-Top House’; wind 60 miles per hour. They were out but five minutes, yet their coats, . caps and hair were covered with frost 65 and Mr. Thompson had slightly frozen a finger. Later, the wind had fallen to 30 miles per hour, and now, eleven o’clock, P. M., it is moderate for Mount Washington. “1870, December 23d. A cold morning, thermometer zero, but Ave don’t feel the cold as sensibly as in the lower regions. “December 24th. "Yesterday afternoon and late at night a ‘snow bank’ lay along the south; this forenoon, enow was falling^with a temperature of — 13°, at times during the day the wind was as high as 70 miles an hour, consequently, we were confined to the house. It is cold to-night, (now nine o’clock, P. M.,) the thermometer — 15°, "^nd only 42° in the room, although we have two fires. “ December 25th; There were no clouds above or around the summit. Below, and but a little lower than this peak, the clouds were dense and covered an extensive tract of country. Through the less dense portion of the lighter clouds the sun’s rays gave a peculiar rose tint, e^ctremely beautiful in eflfect. * * * About ten o’clock, A. M., Mr. K. and myself, wont out for an observation. "We had the pleasure of witness ing the formation of several coronse, sometimes single, but oftener three; even on one occasion /owr distinct circles appear- ing and disappearing so rapidly that it was impossible to more than catch a glimpse of form and colour. It was a phenomenon of rare beauty. “December. 29tb, 1870. The wind has been increasing all day. ' At 7 o’clock, A. M., observations : wind, 46 miles per hour; at 2 o’clock, P. M., 57 miles; at 4 o’clock, P. M., 72 miles; at 7 o’clock, P. M., 46 miles ; and at 9 o’clock, P. M., nearly calm ; a great change in 14 hours, especially in the last tAvo hours. Barometer has fallen rapidly all day. “December 30th, 1870. The morning is calm, clear and bcautifull It is what Ave have Avaited a month for. We com- menced AAmrk making negatives at sunrise. In the morning we made a feAV 8 by 10 negatfA’’es, but as AA-e were making the last of them the Avind freshened up, and AA’e could not make as many as aa^c wished. * * * Before I close to-day’s memo- randa I must speak of the splendid Anew we had afterthe wind, by bloAving so fiercely, obliged us to quit work. We could see distinctly hundreds of mountains, lakes, ponds, &c. Off to the northeast in the distance — one hundred and fifty miles distant — Ave see Mount Katahdin, the highest mountain in Maine, and 6G II little to the 'nortli "vre see mountains Avhicli ap.parently are much farther awaj^ than Mount Katahdin, and must be in the upper part of Maine, near Canada. We never before saw the ocean nearly as plain as to-day ; '''"g could see a great distance ‘to sea.’ Off to the southwest Ave could sec Kearsarge mountain and ^lonadnock, and over the Green mountains, the Adiron- ■dacks and Lake Champlain, in northern hTew York, were distinctly visible. About 2 o’clock, P. M., I noticed, a long hazy line over the ocean ; soon it grew larger and then I could sec it was nearing us, and in an hour it was within 40 miles, and we could see it as a vast sea^f cumulus clouds. The wind was increasing, and had chang'^ from the east to the south, and it carried the appi’oaching clouds and storm to the north of us. We were thankful to see it go by without striking us, for it is grand to behold but not desirable for a covering. To-night we have some of the effects of it in the wind, which, as I write, is blowing a most, violent hurricane, making the Observatory creak. A few hours ago the wind was scarcely noticeable ; . now its velocity is over eighty miles an hour, and .for a wonder ■ it comes from the south, instead of nortlnvest as usual, and as a natiu’al consequence it tears off’ all the loose ice and frost from the Observatory.’ It seems as if we Avere at sea in a severe gale, and broken ice and timbers were beating against our ship, and at times our building shakes like a vessel in a storm. Contrary to what ordinary experience would seem to teach, the north side of the building is less exposed to the fury of the element than any other.” This is OAving to its haAong but one electricity. ' ■Yow, why docs not the north wind, or the northwest wind, produce similar effects? The sun shines upon both Avinds alike, and if it sends doAvn heat to this planet, the northwest wind should be as warm as tire south wind, and should tear off the frost-Avmrk from buildings and rocks just as the south Avind does, But no such effects are observed during the preA-a- lence of these porthern Avinds; on the contrary, it is Only while these northern winds are blowing in winter that this frost- Avork is formed. The explanation I conceive to be this: the southern winds coming from a warm atmosphere are positively electrified, and when theyreach the frost work on the buildings or rocks oppositely electrified, their impact produces friction, which evoh'ing more positive electricity, develops heat that detaches the frost work from its adhesions, breaks it into pieces, and 67 finally melts into water — while other frost work protected from the south wind remains firm and unaffected, the tem- jterature of ' the atmosphere being below the freezing point of water. “ A telegraphic wire connected the Observatdr} with liiarshfield, a distance of three miles, where it is joined with the Western Union Company's line, at Littleton, twenty-three miles farther. The wire has frequently been charged with, atmospheric electricity, especially in the afternoon of the 7th of January, 1871, when, on account of the high tension of these, eurrents, it became utterly unmanageable. When the kew was opened, the flow of the current still continued, exhibiting- bright spai’ks, leaping from one platinum point to the other.. After dark, no auroral display could be seen. There is also wire connecting the summit with the. G-len House, which is- detached from the poles and laid upon the ground during the^ winter, to protect it from the violent winds prevailing at this: season. We had it attached to an instrument, and, althonglr no battery was used, we discovered that it was sometimes charged with . electric currents, which deflected the needle* considerably. The Glen wire was broken about a mile and . a half from the summif, and the one down the railway had parted at about the same distance, thus making thephenomenoa quite remarkable. “ 1871, Januai’y 10th. After ten, A. M., the summit was freo from clouds, but below masses of clouds were driven along the valleys and over the lower summits. The clouds about and over gave grand effects of light and shade along the mountain range — they were particularly fine on Adams and Jefferson and near the Glen. The snow’ is nearly all off the houses and the' rocks — a great change in three days’ time. I cannot leh this da}’’ pass without a mention of the high temperature: at one o’clock, P. M. it was 37°. Like April it seemed, but ■'vho knows what it wull be to-morrow ? “January 14th. Last night we saw a fine aurora, broken arches with streamers , never before was one apparently so near; it certainly did look as though it \vas within reach. “ January 16th. Still raining; at. eleven o’clock this fore- noon, Mr. S. started out on a voyage of discovery, but it rained so hard and the w'alking was so difficult that he soon came back. =!:**. ^ent down to the spring to-day and brought up a pail of w’ater. A w'eek ago this w'as an arctic region, now it is more like April in the valleys of Hew Hampshire. cs “ January 17th, The wind was high during the night, say eighty miles per hour ; at 7 o’clock, A. M., to-day, only 75 miles • per hour, strong enough however to compel Mr. 11. to sit while he measured the force of the wind that he might, not be blown over into Tuckerman’s ravine. * * * * JXas blown stilSl}'’ all day, yet we have taken the air several times; pleasant walks in the face of a fifty mile breeze. Perfectly clear at sunset. Had one of the best views of the shadow of Mount ‘Washington on the sky yet obtained. The mountains far and near look dull and gray now since the rains. “ 1871, January 19. Mr. R. called us out, before sunrise, to see the beauty of the morning ; in truth it was wicked to miss such a glorious view as we had. Perfectly clear, and nearly calm. Hever before liave I seen the shadow of the mountain so grand on the western sky, never so charming the purple tints at break of day. Hever so impressive have been the shaded outlines, the lights and shadows on the mountains and in the valleys, as on this memorable morning. Sunset was J)Ut, the complement of the morning,' and the evening is beau- tiful as ever night can be, the stars shine with a light as soft as June, all, all is beautiful. “ January 22, 1871. Having a gale to-day, and not only a high wind but a temperature below any thing I have ever expe- rienced before; now, at nine, P. M., — 34 degrees inside the door; at two, P. M., wind 72 miles per hour. Professor 11. measured ^ the velocity, he had to sit with a line around him, myself at the other end indoors as an anchor ; even then it was impos- sible for .him to keep his position. Temperature — 31 degrees. I put up a pendulum, this morning, in our room, it is four feet long, and the rod passes through a sheet of cardboard, on which are marked the points of the compass. The oscillations, when the wind blew in gusts, were in every direction, chang- ■ ing suddenly, and sometimes had a rotary motion. '\Wien the wind was steady, the oscillations were northwest and southeast. ‘With two fires the room is cold to night. “ January 23, 1871. The wind raged all night. The house rocked fearfully, towards morning the wind ceased, and all day it has been nearly calm. The temperature outride — 43 degrees. Professor H. and myself sat up all night to keep the fires going. The pendulum gave oscillations of an inch and a half at times during the night. Temperature to-night at ten o’clock — 40 degrees; a changeable climate this. 69 “January 31, 1871. The most glorious sunrise this winter. To the east was a sea of clouds broken and much lower than usual. The protruding peaks resembled islands, more than ever before ; over noTthern Xew Hampshire and Maine, and along the coast, the clouds .were very dense, but their upper surface, as the sun shone across them, was of dazzling bright- ness, while singular forms of cirrus clouds overcast- the sky. Low in the west it was intensely black, and detached masses of clouds floated along the northern horizon. For an hour after sunrise all these cloud forms were constantly changing in colour — purple and crimson, leaden hues and rose tiht.s, almost black and dazzling white. “February 1, 1871. Clouds on the summit till noon, when it suddenly cleared up. Early in the forenoon, the wind was fully 50 miles per hour, at noon it was nearly calm, and till nine, P. M., not above 20 miles per hour. At nine, P. M., tlie thermometer indicated — 16 degrees. “From 3.30, P. M., to sunset, there were the finest clotid dis- plays posgfble. Eastward, heavy masses of clouds, in color from gray to an intense black. Westward, detached cirro-stratus, presenting every shade and colour; along the northern horizon a clear light rested; the west was burning bright in crimson, purple, and gold, while far south, fading out toward the east into gi’ay, the colour was a delicate rose tint. Below, to the. west, far as we could see, the Avhole country was covered with cloud. The icy peaks glow' and glisten in the bright sunlight. The transitions of shades and tints, the colours, burning into the radiant sunset, surpassing any thing we have seen yet for a sunset scene, mark this as a day never to be forgotten — as I write, it seems like a dream. “1871, February 2d. All day the wind has been light, and it was nearly calm this evening till half an hour since, when, without any warning, (except the falling in the barometer,)- the .gale began, not with a rising wind, but with a single blast that shook the house to its foxmdations. * * * How, at 11 o’clock, P. M., the wind has risen to the dignity of a gale. The temperature — 20° out of doors. ^ “Friday, February 3d. W ell, it did bloAv last night, making some of the time such a racket out-doors and in-doors too,'for thatiiiatter, that sleep was out of the question. The wind must have been as high as 90 miles per hour during several of the heaviest gusts. For a change to-day, we got the most severe 70 enow storm of tlie winter so far. The wind is northwest, the point from which our storms and hurricanes come. At no time has the temperature been higher than 5°; it was — 25° this morning at 7 o’clock. “ Saturday, February 4th, 9 o’clock, P. M. The wind rising towai'd morning has held its own all day, at no time being below 75 miles, and since 8.30, acts as if it was ambitious to attain the 90 miles per hour standard. At 7 o’clock, A. M., temperature — 33°; from 5 o’clock, P. M., to this last observa- tion it has gradually worked down to -^0°. '\Vo have not suffered from the cohi simply because we have not exposed ourselves to it, In the room at no time has the temperature been lower than 34°, and most of the time we have managed to keep it up to about 60°. ’ To do this, we have the stoves at a red heat; the thermometer hangs precisely five feet from the stove; ten feet from the stove at the floor, to-day, the temperature was only 12°, at the same time was 65° in other parts of the room. Midnight — really there is quite a breeze just now. Some of the gusts, from what we know of the jueasured force, must be fully up to 100 miles per hour. In fact it is a first-class hurricane. The wind is northwest, and as the house .is broadside to it, the full force is felt; at times it‘ seems as if every thing was going to wreck. We go to the door and look oiit ; it is the most we can do ; to step beyond, with nothing for a hold fast, one Avould take passage on the wings of. the wind hi the direction of Tuckerman’s ravine. However unwillingly one might go, such would be the result if he should Venture outside, so irre.sistible is the force of the w'i.nd. What varied sound the wind has as it changes, now howling, screecliin.g, roaring as though the building was sur- rounded by demoniac spirits, bent upon our destruction. We shout across the room to be heard. Xow it suddenly lulls, and moaning and sighing it dies away; then quickly gathering strength, it blows as' if it would hurl the house from the summit. The timbers creak and groan and the windows rattle; the walls bend in-ward ; and as the wind lets go its hold, rebound with a jerk that starts the joints again. The noise is like rili.e firing in fifty different directions, at the same moment in the room— a moment ago close by me as I sat here, leaning against the wall, now in the outer room or up aloft and out- side as well. Then there is the trembling and groaning of the whole building, which is constant. Everything movable is on the move, books drops from the' shelves, we pick them uj), replace them only to do it again and again. The tempera- ture is now — 10°. 71 “ Sunday, February 5tb, From one to two o’clock, A. M., tbe wind was liigber than during the early part of the night. Some- of the gusts must have been above 100, possibly 110 miles per hour. The tempest roared and thundered. It had precisely the sound of the ocean waves breaking on a rocky shore, and the building had the motion of a .ship scudding before a gale. At 3 o’clock, A M., the temperature had fallen to — 59°, and the barometer stood at 22.810, attached thermometer 62°. Barometer was lowest yesterday at 8 A. M., when it was 22.508, and attached thermometer 32°. Isow, 7 A. M., the thermometer indicates — 25°, and the wind has fallen to 70 miles per hour. By accident, the spirit thermometer has not yet been received. But this has been the only day when the mercurial instrument has not been perfectly reliable. The valleys are foil of stratus clouds ; charged with frost as they are, occasionally sweeping over the summit, they completely cover one in a moment, hair, beard and clothing; when the face is exposed it feels like the touch of hot iron. To breathe this frosty air is very unpleasant. A full inhalation induces a severe coughing fit. “ Monday, February 6th, 9 A. M. Talked oyer the events of the past night at the breakfast table. * * Of all the nights since this party came here, the last exceeds every one. 9 P . M. ; it has been a rough day, down in the world people would say a severe one, so should we but for the recollection of last night; our coal bin is under two feet of snow, and anywhere in the room, that snow is six inches deep. The highest teni- pex-ature is to-day 12°, and the lowest now, at 9 o’clock, P. M., is 2°, a very acceptable change — wind 50 miles in the fore- noon, now 20 miles per hour, is good as a calm. It is clear, and the moonlight is that of the niountain, seen only at this or . higher elevations. “Tuesday, Febniary 7. A glorious sunrise; a quite warm dav, and at sunset almost equal to that, of the 1st; tempera- ture at 2 o’clock, P. M., 62° in the sun; change of temperature since Sunday of 121°.” These sudden and great valuations of temperature in the same latitude elevation above the sea, and identical locality, in short spaces of time, are strong evidences that the tempera- ture' of our atmosphere is exclusively to be attributed to electrical causes within it, and not to any supposed rays of heat emanating from the sun. “Tuesday, February 7th. I have given some time this after- oon to the study of cloud formations. Days like this are so rare, that we improve every opportunity for investigation. Gales, sTorms, hurricanes, all clear off with a north wind — a wind gentle and soft as the south wind of the lower regions. How can this he explained? It is S. S. to-night and 2 miles per hour; a marked contrast to Sunday morning.’ Let us attempt an explanation of this phenomenon : Tnicn masses of clouds, freighted with moisture, and at different elevations, approach each other, attracted hy their opposite electricities, heat is evolved hy their conjunction. The watery vapour constituting the clouds undergoes a radical change ; the atmospheric air, which holds the water in suspension, absorbing the heat that is evolved hy the conjunction of the opposite electricities of the clouds in commixture, is so greatly expanded and rarefied that its molecules can no longer sustain the particles of water with which they had been associated ; this attenuated air, thus heated, leaves the watery particles, and being positively electi’ified, is attracted hy the opposite electricity of the higher atmosphere and ascends instantly into it, while the Avater being negatively electrified is repelled from the air above, and begins, to fall in sheets, Avhich soon separate into drops, repelling each other, and carrying to the earth the. electricity in a latent form with which they were. associated. When the clouds have thus discharged all their water as hail, snow or rain, to the earth, the atmosphere - in which they floated becomes very dry and electrical. The north wind, Avarmed by the heated air AA-hieh has escaped from the clouds when they met, is attracted to the spaces before occupied by the clouds in the direction of the ocean and becomes the gentle, balmy air described by these observers, and as dry air has an electricity ahvays opposed to that of moist air, the north wind at Mount Washington ahvays is attracted to the Atlantic ocean to the south of the mountain, and storms thus terminate in that locality with a north wind. “ WednesdaA', February 8th. Ten o’clock, P. !M. There is evidently a snow storm along the coast, the northern edge, within fifty miles of us. This forenoon we could see the storm as it moved eastward. It aauis cloudy and clear by turns on the summits, that is, the loAver current of cloud. rested at times over us. The valleys east were full, and the upper stratum OA'ercast the entire country as far as could be seen. Wind S. S.‘W., from 20 to 50 miles per hour. Temperature from 73 14°, at 7 o clock A. M., to 20° at 2P. M. Interesting to watek the progress of the storm and to see tke lower current of cloud driven by an easterly wind, running under the higher stratum, which of course is toward the northeast. Let us here stop to admire the infinite wisdom of the Creator, who, using the attractive forces of his electricities to gather and collect the watery vapours of the atmosphefe into clouds, disperses them by the repellent forces of these same electricities and scatters in this way their manifold watery blessings over greatly increased areas of the surface of the earth. “ Thursday, February 16th. A storm of snow and rain. It rains here, wdth the thermometer at 22°, as it did to-day, and snows with it at 30°, as might be expected. Why it should rain at 22° is hard to explain. Wind steady; southwest through the day ; but, at 8.20 P. M., changed suddenly to northwest in gusts, 60 to 80 miles per hour. Forgot to men- tion last night, that at 6.30 P. M. I read from the ‘Atlantic^ in the open air. Our days are about 46 minutes longer than they are at the sea level.” • The warm southwest wind explains the |rain at 22°, which was probably the temperature outside of the column of warm . air brought up by the southwest wind. “ Sunday, Februaiy 19th. A bright, sunny day, clear and calm, yet the temperature was at no time higher than 8°.” Where was the sun’s heat ? “ Tuesday, February 21st. When S. left this morning the thermometer read — 4°, and wind 20 miles per hour; at the Gulf Tank it was so warm he had to lay aside overcoat and gloves ; no wind there ; the -snow was melting and the water running down the centre rail; quite a contrast to the summit, only one mile distant — meteorologically speaking, he was 300 miles south of his mountain home, though in sight of it. We took a walk. Fine weather for a. change. Beautiful cloud views this afternoon. Light fleecy clouds floating over Mount Monroe. Dissolved before reaching Tuckerman’s ravine. They passed between us and the sun, showing the prismatic colors ; then as they x-olled eastward, gradually faded out and changed to a cold gray. The transitions of light and shade were inex- pressibly beautiful, enough to give sensations of pleasure to the dullest observer, and drive an artist crazy with delight. 74 The buildings are cased in ice and frost worls: of most elegant forms, resembling rocks, flowers, leaves, shells and the wings of birds. “February’- 24th. From 9 o!clock A. M. to 3 P. M. the tem- perature varied hut a deg^-ee or two from 37° ; the barometer, steady. ^ “February 27th. This time we are favoured with a rain storm, pouring Avhen it was calm, and in driving sheets after . the wind rose to 84 miles per hour. At 9 A. hi. it changed to snow, and then, by turns, rain for a moment, then quickly changing to snow, and suddenly rain again; but the snow obtained the mastery. “February 28. If cleared oflT early in the morning. Wind from 50 to 70 miles per hour. The mean temperature, zero. “ March 3. A storm seemed to be brewing last night at a late hour, and early it came, a heavy rain storm. Towards noon the wind, rose, and at One P. M., it blew 96 miles per hour. How the wind roared in the flue ! How the house shook ! Had to shout across the room to be heard. It was grand, however, l^Tom 4 o’clock P. M. the wind abated. “ March 23. At 9 P. !M., snow squalls to the northea^., and the clouds gradually settling in the valleys. * * * * J3y 2 P. M. the mountain was in the clouds. They were at a higher elevation than has , generally been ■ the case — cirro stratus; color gray; uniform in density nearly over the entire field of view. * * * * Evidently the lower current was from the east, while the wind on the -summit was west north- west. * * * * The clouds passed over Mount Adams, and later over the dividing ridge, between Mounts Washington and Clay. They seemed to curve, as they passed over these mountain tops, as though the upper currents of air conformed to their irregularities of surface.” [The mountains and the clouds having the same electricities, which repelled each other. — The Author.'] . * “ When there are two strata of clouds, they unite before the snow or rain falls, as a rule, though to-day the snow fell an hour previous to the clouds settling on the mountains. “April 1. To-day, 64 degrees in the sun, at 11 A. M. Afterwards cooler — 15 degrees at '9 P. M. * * * * northeast wind to-night, seldom- from that quarter. * * * “ April 3 . * * * * Sucli is the atmosphere here, that iilthough the thermonaeter, iu the shade, marked 27 degrees, I wore neither hat nor coat, and yet was warm enough. “April 4. 'All the forenoon, -till one P. M., the summit was in a dense cloud. Suddenly it lifted, and then we had the most gorgeous display of cloud-scenes we have yet wit- nessed. Eastward, masses of cumuli rested over the valleys and the mountains. Why not call them mountains of clouds ? (■ertainly. They rose far above our level, six thousand or perhaps eight thousand feet higher than this peak. They con- formed to the heights over which they lay, and seemed to envelop other mountains, nearly as lofty as their upper limits. The illusion was perfect, and Mount Washington in compari- son, was a diminutive spur, or outlying peak of this great mountain range. * . * * * sun rises high, but we knoiv nothing of Spring. Truly it is more like Winter than some of the time in March. Then there was no snow. hTow, ■ everywhere there are snow and ice. “ April 6. • A clear sunrise — cold— thermometer only. 3 degrees, the wind 20 miles per hour, and the morning view, that of December. Though clear, the sun gave little heat— -a pale Avhite light ; the sky a light blue, and so clear, that it seemed almost as though we could see beyond its bounds, or through it into the regions of space. “April 15. The rule holds good; .no two days alike on Mount Washington. Ten hours we had splendid cloud-effects in every direction; cumuli north, in every form beaiutiful and fantastic, and colors as though some radiant angel had thrown aside his robe of light. “ April 28. ■ To show tlie changes in temperature here, in a few feet of altitude, I note my trips down, to-day, and up as well. Left the house at 4.30 P. M.; wind 30 mites an hour; at the Lizzie Bourne monument, 40 miles; at the Gulf House ruins and below, 60 miles, thus reversing the order of things in regard to wind. Thermometer on the summit 28°; frost- work forming some distance below the: monument. At the Gulf Tank, when the sun came out, as it did several times, the ice on my cap would thaw completely; then, while the cloiid was passing, icicles two inches in length would form on the visor. It was difficult to work or even stand against the wind below the Gulf House ruins. .Keturning, the wind was not so violent. 76 “May 1. May Day, and still it is winter; every aspect is that of mid-winter. The spring near the Observatory remains frozen solid, and so we daily melt ice for nse, and yet down the mountain a half mile there is seldom a day when the stteams are not running. “ !May 4, Another tough snow-storm -^ * * * wind got up to 48 miles per hour and temperature down to 21°. “ May 5. The storm — ^snowing in such a wintry way last night — turned to rain toward morning, and has been raining all day. * ■* * The wind was Avest here — not higher than five miles per hour — yet in the valleys it must have been much stronger, judging by the velocity of the clouds; besides, wo could hear distinctly its almost roar. “ Monday, May 6. This morning, clear, calm and warm. The thermometer, at 8 o’clock A. M., indicated 85° in the sun ; warmest morning this spring. “May 7. The barometer fell 50-100ths from last night at 9 o’clock to this morning at 7 o’clock. Wind rising at 3 o’clock A. M.; reached its highest velocity, G7 miles per hour, at 2 o’clock P. M. — highest recorded for some time, quite strongly reminding us of the winter months. Snowing all day. * * * At 5 o’clock P. M. the cloud passed otf and we. could see that not the mountains alone, but the lower country as well was ‘ snpAv-bouird.’ At 9.40 P. M. snowing again. Temperature, 2 o’clock P. M., 21° — highest for the day — aud 19° at 9. o’clock P. M. . “May 8. We did have a rough night; called tue wind 80 miles per hour at midnight. Temperature at 7 A. M., 15°. “ !May 9. Mountain peaks white as winter, but the valleys are bare. The frost Avork has seldom been more beautiful. Measured some feathers to-day, on a tall pole, at the Tip-Top -House ; found them 36 inches in length, and on a rock south of the house 49 inches in length and 15 inches broad. ■ “ May 11th. AAvintry sky and Avinter scenery this morning. The sky a pale blue and the sunshine Jhat of Jlecembcr. * * *- * Temperature 20° at 7 o’clock A. M. “May 14th. The Avind was high as 80 miles per hour, if not higher, during the night. All day, as usual, it has been cloudy and frost work forming. Temperature at 7 A. M. Avas 11°, aud highest for the dayat 9 P. M., 21° ; at no time the Avind lower than 46 miles per hour. Mr. IT. left at 9 A. ]\I. in the face of a 48-mile gale and the temperature only 14°. I am auxieus for his safety, and shall he till S. returns. The winter s work is done. Storms of unparalleled severity, when, for days in succession, the summit , was enveloped in clouds, and the hurricanes lasted longer and were more vio- lent than any yet recorded in the United States, together with very low temperatures, have been a part of our experiences. Just such an experience has seldom before been the lot of human beings. * * =(= And ours has been the good for- tune to witness some of 'the most magnificent winter scenery upon which mortal eyes ever rested, scenery of transcendent grandeur and views surpassingly beautiful. _ “ There were days when the shifting views of each hour fur- nish(^d new wonders and new beauties, in the play of sunlio-ht and changing cloud-forms, every hour a picture in itself and perfect iu details. Sunsets, too, when an ocean of cloud sur- rounded this island-like summit, the only one of all the many high peaks visible above the cloud billows, all else of earth hidden from sight; there were times. when this aerial sea was burnished silver, smooth and calm, ancKtimes when its tossing waves were tipped with crimson and golden fife. * * * » Gone are the long days and longer nights, when the stoves failed to comfortably warm the little room, though we kept them at a red heat, and when the thermometer indicated 66 ' near the stove and 4° at the floor ten feet distant.” Wo have presented these extracts from the published obseiv- ations of the gentlemen who passed the winter of the years 1870-1871 on Mount Washington, to show the sudden and great variations of temperature that occurred on the mountain by day as well as by night, and that these variations could not have resulted from solar radiations of heat, as sometimes when the atmosphere was the clearest and freest from vapour, and when the sun was shining with the greatest brilliancy, the temperature on the mountain was lower than when these conditions of the sun and atmosphere did not exist, and further, when the sun had passed the vernal equinox, and- was approaching the summer solstice, the temperature on the mountain, and the condition of its atmosphere, continued still to be wintry, unaftected by the change in the position of the sun, relatively to the angles of incidence of its rays. When we consider the altitude of Mount Washin^on, 78 wliich. is only 6,293 feet alcove the sea level, or not mucli more than one mile, we find that its projection above the periphery of the earth would he about 1-8000 part of the earth’s diameter, a protuberance so slight as to be wholly inappreciable at the sun’s distance of 92,000,000 of miles from it. What proportion of solar radiation ot heat (if there is such a thing,) could fall upon so microscopical a spot as Mount Washington, cannot therefore readily be imagined. But when we contemplate the electrical forces of our planet developed by sunlia^ht, the radiation of interior terrestrial heat into the atmospliere — the movernents of oppositely elec- trified currents of air, and the commingling ot tumultuous masses of cumuli clouds, all evolving heat and changing vith great suddenness the temperature of various localities, _we begin to comprehend the plan of the Creator in furnishing each planet with its own sources of heat, instead of attempting to supply them with heat through almost interminable spaces, from so distant- an orb as the sun. To an observer outside of our atmosphere, looking down upon our planet, he would see sometimes masses of dense clouds, which, intercepting the sunlight would cast dark shadows of various forms and sizes proportional to the clouds which would form them on the surface of the earth. ' The darkness of the shadow would be in proportion to the depth and density of the clouds floating between the sunlight and the earth, ■ These shadows would ' flit across our earth as rapidly as the clouds which had pro- duced them, in great storms or hurricanes of perhaps 100 or more miles per hour. JSTow may not tfie sun spots which have so much exercised our astronomers be produced m a similar way ? Clouds or vapours of various luminosity being interposed between the most luminous part of the sun’s envelope and the gray atmosphere of the sun, would cast upon the latter shadows so dark and so flitting as to resemble the shadows of clouds on our own planet, and the dispersion of the clouds so making the shadows would account for the rapid disappearance of the sun spots. The forms of the sun spots would vary with the sinuosities and unevenness of the surface of the gray envelope of the sun upon which these shadows fell, and the continual interference of intense liglit derived from other luminaries of the stellar world, with the fainter light received from our planetary system, would greatly increase the darkness of the shadows so produced. Let us now consider the case of a total eclipse of the sun by the moon. In the reports of observers, the following appearances have been described: Solar prominences during- eclipses, red protuberances, red clouds, red flames, &c. One observer says: “They form around the solar globe a denticulated and continuous series of projections of very curious appearance.” Another observer says: “The. promi- nences were seen very distinctly, their colour was that of red coral, slightly tinted with wolet. They all appeared to be adlierent by their bases, and none of them floated detaehed at a certain distance from the moon as was observed in the years 1851 and 1861. “ The following facts may be considered tolerably certain ; “ 1. The prommences (or protuberances) belong decidedly to the sun. “ 2. The prominences are of a gaseous nature, that is, they are coVnposed of an incandescent gas, principally hydrogen gas, but thej' contain doubtless other substances, perhaps sub- stances tha.t arc unKnown on the surface of our earth, at least such would xrppear to be proved by the existence of a brilliant . line in the spectrum, near to the yellow line of sodium, but not coinciding with the latter, and, moreover, most curious to relate, it does not coincide with any dark ray of the solar spectrum. “3. The matter which forms the prominences is of very ' great , extent, whether it spreads over the entire photosphere or not ; it forms a continuous layer, the thickness of which is estimated by Mr. Loeyer, at some 5,000 miles on an average, and the prominences appear to be only portions of this layer projected to a certain distance from it, sometimes detached from it a.nd floating above it. One of the great prominences, represented upwards of 100,000 miles in vei'tical height above the photosphere. “ 4. These stupendous accumulations of incandescent gas undergo, in very short intervals of time, very great changes in their form and size, which indicate that the layers, of gaseous matter of which they form part are iu a state of con-, stxuit agitation, the cause of which is unknown, perhaps it is the same that gives rise to the spots and faculse. “It is extremely probable that the the entire globe of the sun has a very high temperature throughout its mass — a tem- perature which surpasses the melting (or boiling) points of 80 most of the elementary substances of which spectral analysis has revealed the existence in its atmosphere. At the same time, it is evident that the various concentric layers of which the solar globe may be supposed to be formed, exert one upon tlie other considerable pressure, since we find that at the sur- face itself, the intensity of gravitation is twenty-eight times as great, as it is upon the earth’s surface. This pressure may hinder fusion to a certain extent, but not incandescence, fiut we believe that the hypothesis of a liquid incandescence or even a gaseous nucleus is more probable.” All such hypotheses are put at rest by the recognition of the sun. as a great magnet, since magnetism is destroyed by heat. “ The prominences on the right, (western 'edge) appear like a mass of snow-capped mountains, the bases of which rest on the limb of the moon, and are lighted up by the, rays of a setting sun.” (From M. Jansen’s observations on the eclipse of the sun from Aden to Malacca, Augu'St 18, 1868.) “ In 1858, M. Liais found that the light' of the sun’s corona, is really polarized, and at once concluded that the sun has an atmosphere extending far beyond the nhotosphere. “During the short, phase of total darkness, a luminous corona makes its .appearance, being generally of a silver whiteness, but is sometimes coloured and surrounds com- pletely the dark limb. Its apparent breadth is from one-fifth' to one-twelfth of the diameter of the moon, and from it, light decreases gradually.” ■We have here in the aspect of the clouds in sunshine, from the summit of Mount Washington as they gather from the sea or from the land, advancing, stationary, or retiring, the most vivid descriptions of the varying brilliant tints and gorgeous groupings of colours, as the changing angles of incidence and reflection met their sight, that it is possible to conceive. We, who are familiar with the magnificent autumnal sunsets of many parts of our country, may begin to imagine the exquisite beauty of the scenes which these gentlemen have witnessed. But the particular object we have in view in calling your attention to it, is to trace the analogy of these displays of colour, light and shade, with those described by astronomers in investigating the physical condition of the sun. We have the same tints, brilliant colours, neutral colours, shades and shadows, in our planet as are described to be seen in the sun— -similar disturbances in the vapour of both orbs. 81 I.s it too mucli to imagiue, therefore, that if an obf 5 errer could , he placed within telescopic range hejond our atmosphere, he might see in our atmosphere an exact imitation, upon a reduced scale however, of whatever has been exhibited by the sun, as the disc of our planet would then display a reflection of the illumination of the whole stellar world? And wdiat more does the sun do ? He receives the light of the whole stellar and planetary world, and reflects it again through space, thus presenting to one orb, or set of orbs, the light he has received from others, until throughout the great expanse, light is diffused everywhere to shine in the firmament of heaven, atid give light upon the earth. We have had exhil)ited in this city, (Philadelphia,) a few W'oeks since, by a distinguished artist, an oil painting of ‘‘Pike’s Peak,” one of the grandest mountains of the Eocky Mountain range. Its height is 14,216 feet above the sea level, and on its very summit is a signal station and observatory of the United States, erected in the year 1873. Its summit is covered with snow to a descent of perhaps a thousand feet. The painting, which represents a sunset scene, portrays the .snow-covered summit, illuminated all over by a brilliant red tint, resembling red coral, and creating at first sight the im- pression of a mountain on fire. The resemblance to the red protuberances around the sun, during eclipses, as depicted in photographs taken by the observers, is • most striking. This brilliant red coral colour jDervades the whole surface of the summit of the mountain that is covered with snow, and which is seen through the red colour. Here we have, an exact resem- blance of one of the appearances of the sun, as displayed during an ■ eclipse, and yet there is no incandescent gas covering “Pike’s Peak” to produce this colour. On the com trary, the atmosphere around and above the mountain is - wintry, with a temperature below freezing point “ JEx pede IlereidemI” May we not infer from' this illustration that thei'c is no incandescent gas about the sun, and that the varied tints and colours, however brilliant, and however resembling what w'e suppose to be incandescent metallic vapours, are reallyonly manifestations of light in its protean displays, as fitful and evanescent as we see it in our autumnal sunsets. How let us for a moment imagiue that by the interposition of the moon between the sun and the earth, each suffers an eclipse from the other. Let us suppose that the snow-clad mountains of our planet are bathed in sunlight, and that the 82 T>rilliant colours derived from that source, changing with the angles of incidence and reflection, with which they encompass these snow-clad peaks, become displayed beyond the peripheiy of the moon, which has concealed a large part of the body of the earth. N"ow, if an observer could be placed belwcen the moon and the sun, at the period of such an eclipse of the earth, would he not witness displays of light and colour, greatly re- sembling, if not identical, with those which woulcLbe seen by another observer placed between the moon and the earth, as he regarded the appearances about the sun ? What then would l»ecome of the terrific heat of the sun and its incandes- cent gases ? “ In the hypothesis of undulations, instead of supi)osing the transport of a material agent to great distances, it is held that the vibrations of luminous bodies are communicated to the atoms of an all-pervading ethereal fluid. These vibrations, propagated througli this fluid, reach the organ of vision, which in time transmits them to the optic nerve. In this bpothe- sis, the nature and transmission of light would be analagous to the nature and transmission of sound, light being produced by atomic, and sound by molecular vibrations.” This idea confines the action of light to animal vision. In these cases there is no analogy, for sound has a very limited range of action, with comparatively small velocity, and is only of value to living beings. While light has scarcely a limit as to distance in penetration, and a velocity inconceivably ■great, and is indispensable to planetary existence. Two persons hold a table-cloth, twmnty-flve feet long, by its two ends, loosely in their hands — the actual distance between these persons in a -straight line is twenty feet — one of these 'persons raises his arms, and, by a strong impulse, shakes the cloth, while the other end is held by the other person firmly, a wave of the cloth is formed, and runs through its entire length, at the extremity of which it is lost. This is called undulation, or wave-making. The cloth rises and falls in the wave, which runs through twenty-five feet, its whole length. The distance traveled by the wave is twentj^-five feet, being five feet more than the distance between the two persons holding the table-cloth. Should the table-cloth be stretched to its full length, no wave could be produced. - llow, let us apply this example to the sun and the earth. The luminous ether, as the intervening space between these 83 two orbs is called, is uiuety-tw'o millions of miles in length and, to admit of its undulation,, must be very loose in its con- sistency. We may safely infer that such undulations as would lie required for the transmission of light from the sun to the earth, would increase the actual distance traveled by the light in its undulations fully ten millions of miles, making the traveled space between the sun and earth to be one hundred and two millions of miles instead of ninety-two millions of miles, the measured distance. ITow, the greatest velocity known is that of lightf which is 186,000 miles per second. We do no injustice to Divine Wisdom when we suppose that this extreme velocity has been imparted to light, in order that it should pass through space without interruption, and that it should reaclr rts destination in the shortest possible space of time — in other words, that it should go directly to its object in, right lines, without any deviation, up or down, or laterally,, which would only retard its progress. Hence we reject entirely the undulatory theory of liglit, as enunciated at the present time. If fhe laws of light arc not comprehended by- scientists,, it furnishes no excuse for resort to absurdities in the effort to- explain them. While light, in traversing inter-stellar and inter-plauetary spaces, is thought to be confined to rectilinear directions, there is nothing incompatible with this idea when it is brought Avithin the influences of our atmosphere, by which its refrangibility, its reflection, its polarization, and its power to develop electricity, magnetism, aud heat are manifested, and its more speedy diffusion through our atmosphere, by these disturbing influences, may furnish a reason for its attri- butes here, which Avould have no application in its passage through inter-stellar or inter-planetary spaces. “ Light diminishes in force or intensity in proportion as it recedes from its source. This diminution is in direct ratio to the square of the distance. Thus, the quantities of light at dis- tances 2, 3, 4, etC'., will be 4, 9, 16, etc., times less than at dis- tance 1. Light requires eight minutes thirteen seconds to arrive from the sun to the earth. It travels 11|- miles in of a second, or 186,000 miles per second. It travels alw^ays in a straight line. “ Light added to light, by interference, produces darkness. The movement of such rays neutralize each other, and the light ceases to cast any lustre. “ Of the thousand rays of variegated shade and refrangibility * EKcepting that of electricity, which is 288,000 miles per second. 84 Avliieh compose colourless (or white) light, those only ueutrali^^e each other Avhich possess co-ordinate colour and refrangihility. Thus a red ray cannot obliterate a green ray. Two win to lights cross each other at a given point, and one time the red ^ay alone will disappear, and the point of intersection will become green — green being Avhitc minus red.” Let us see what can he made of the fragmentary knowledge of light that we have so far attained. Tlie white liglit of the sun is composed of seven primary rays, all differing in colour from each other. The first analysis of this white sunlight was displayed to mankind in the rainboAv, whose magnificent beauty Avas admired Avith stupid Avonder, AA'ithout the faintest conception on the part of the beholder of what it meant. After a lapse of ages of tinle, Sir Isaac ISTcAvton, Avith a glass prism, separated the rays of a sunbeam, and developed the primary colours Avhich, in their association, had formed the AA'hite light of the sun. He reunited these primary rays, and thus, hy synthesis as well as analysis, he proved the composite chaz’acter of sunlight. Hoav, astronomers have shown that the planets and asteroids of our planetary system each emit a colour peculiar to itself: Mercury, a pale rosy light; Mars, a reddish tint; Yenus, asih^ery- white colour, with occasional streaks of pale blue light ; J upiter gives out a pale yelloAV light ; Saturn, a pale bluish tizit, Avhile its rings are gorgeous Avith a Avhite, silvery colour; the Moon gives out a yelloAvish hue ; Pallas shines Avith a 3 'clloAvish light ; Juno is a reddish star; Yesta has a ruddy tinge, sometimes of a pale yelloAA'ish hue ; the ' Earth emits a red colour. Another remarkable feature of these star systems, and jzer- haps the most brilHajit and intrinsicall}^ beautiful phenomenon of astronomy, is the resplendent and gemlike variety of colours by Avhich the binaiy, ternary and other multiple systems are (fliaracterizcd. Here all the colours and intermediate tints of the Spectrum are to be met with, manifested with the richest intensity and the most A’ivid and distinctiA-e strength and fulness ef hue. Thus in y, Andromeda, we have a ternary combination, the brighter star being a rich and full orange, and the two fainter stars green. In a, Cassippeite, we have a liright blue and a sea green star, /5, Cygni, is a pair of stars, yelloAV and sapphire, a, Ceti, is a very fine orange star with a blue companion. * * * “In a celebrated cluster of stars, near z of the Southern Cross, there are about one hundred small stars of different colours, from the A*arious reds to all the tints of green, blue and bluish- 85 green, so crowded together, that they appear in the larger telescopes like a piece of magnilieent celestial jewelry, stmled and flashing in the most superb splendour ^nth the richest and most brilliant gem-light.” * These colours are primary. hat becomes of all these primary rays of light unless thej’" are used to compose the white light of our sun, and of all the fixed stars or suns that illuminate the firmament ? TMiatever sunlight, therefore, has fallen upon these planets has been de- composed; six out of the seven primary rays thereof have been absoibed for the use of the planet, and the remaining primary has been emitted by the planet, and sent to the sun to associate in his photosphere with the different primary ravs sent to him from other planets, to form anew the Avhite sun- light, which by him is to be diffused throughout the planetary and stellar Avorld. -r- ^ iN oy we must not suppose that the orbs composing our diminnti\'c solar system have furnished, or can furnish, to the sun a surticient c|uantity of their respective primary rays of light to supply that luminary with the amount of elementary light which it is his function to combine and to furnish to the universe. _ We must remember, that, from the great deptlis of the infinite expanse, elementary light comes up from every star, nebula, or meteor, seeking its complementary element in the photosphere of the sun, there to be associated as white light, and thence to be reflected from the gray covering of the sun, as a mirror, to all the orbs of creation. This circulation of light, this absorption by the stars and planets of such of the primary rays of liglit as they need for their own support, and the emission,_ severally, of their own peculiar rays, to be reas- sembled again in the various photospheres of the infinite number of suns that stud the firmament, and to be again dif- fused, according to the plan of creation, in endless suc^cessibn, present an image of the wisdom, the beneficence and power of the Creator,_that fills the mind with awe, and teaches man the utter insignificance of his being. Our sun is simply a huge reflector of light. The gray covering of his nucleus or body is represented in our miirors by the metallic covering which we place on the backs of our glasses. These transparent glasses are tjiflfied by the trans- lucent photosphere of the sun, and the associated primary rays of light from every luminous object in the universe, mingling together, and reflected from this gray covering of the sun, furnish the white sunlight that illuminates the world. *J. A. S, T!ollwyi’-i A«*nn'>ray. 86 TTeat destroys gravitation. Even our astronomers, -in assert- ing that the lunnnous matter in tlie photosphere of the sun is sliWn by the spectroscope to be composed largely of incan- descent metallic gases, the bases -of winch are among the heaviest matter in the crust of our earth, commit the incon- sistency of supposing that these heavy incandescent metallic vapours or gases are supported by a photosphere of much greater specific gravity, as well as density, than these heavy gases themselves; otherwise these metallic gases coidd not float in the photosphere. Some of these astronomers go so far as to suppose that the body or nucleus of the sun itself is gaseous, and that the density of the sun is much less than the densities of the incandescent metallic vapours which they suppose to float in its photosphere. K^ow, if these incan descent metallic gases are heavier- than the material composing the sun., itself, it is clear that the gravitation, according to l!^ewton, of these heavy metallic incandescent vapours is not towards the centre of the sun; and if not to him, where do they gravitate ? We know Avhat the spccifie gravities or densities of many of the metals on the surface of the earth are, whose incandescent vapours, as revealed by the spectoscope, are supposed to exist in the photosphere of the .sun, and astronomers have calculated that the attraction of gravitation to the sun in its jfiiotosidiere Avould be twenty-eight times as great as the gravitation in the earth’s atmosphere to the earth of bodies of similar weight. If, therefore, we suppose that these metallic incandescent vapours in the sun’s photos^phere to be twenty-eight times^ heavier than they aa-ouM be in the. earth’s atmosphere ; and it they nCA'cr fall to the body of the sun, it must folloAV that AA’hat is called graA’itation in the |)hoto.s2:»herc of the' sun ean- not exist, and the Avhole thcoi’y of ISTcAAfion, of centripetal and centrifugal forces, has no substantial existence. Wo knoAV that in our OAAm planet heat destroys gravitation, as the vol- canic action in the interior of the earth, ujihoaVing island.s, mountain ranges, and even continents, abundantly proA^es The mean density of the earth is about five times greater than that of water — actually 5.44 times. Water, therefore, rests on the surface of the eartli — penetrates its crust till it encounters the heat radiated from the interior of the eartlp where its further descent below the surface Is arrested, then it is converted into steam by the heat it has absorbed, and it is driven upwards into the atmosphere, heaving u|) tlie most solid and heavy materials of the crust of the eaz’th, that lie i 87 nljove the direction it may take. This expansion of water into steam by heat in the crust of the earth, produced by the repellent affinity of the homogeneous electricity associated with it, is one of the forces of volcanic action, which are con- tinually changing the forms of the outer surface of the earth’s crust. The density or specific gravity of the sun is 0.25136 (or nearly one-fourth of that of the earth). In other words, taken in equal volumes, the weight* of the matter which com- poses the sun is scarcely more than one-fourth of the weight which composes our globe. Compared to water, the density of the sun is 1.367 ; that of water being 1. How, if what our astronomers tell us of the inconceivably high temperature of the sun be true, there can be no gravita- tion towards iffi centre from its photosphere, its chromosphere, or any of its possible^nvelopes, the heat expanding, rarefying and driving oft' all such material substances. Heat disinteg-’ rates solids, separates their molecules, destroys their densities, and consequently . is opposed to gravitation, which is the attraction, of densities. Alas ! for poor Sir Isaac Hewton and his grand theory of centripetal and centrifugal forces! A ray of light passing through a narrow chink, and through a glass prism, has done the business. .The incandescent nietallic gases and the transcendent intense heat of the sun which has vapourized these metals (the supposed discovery by the narrow chink and the prism), have demolished Hewton and his erratic fancies. Sic transit gloria mundi I According to Professor Tyndall, “gravitation consists of an attraction of every particle of matter for every other particle planets and moons are supp)Osed to be held in their orbits by this attraction.” “ The earth is supposed to attract to its centre all the bodies upon its surface by Avhat Howton termed centripetal force, and when one of them falls, it is always towards the earth’s centre. Tins force is said to be resident in all the bodies of nature. It exerts its influence upon the largest masses as well as upon the most minute particles of matter. This it is which gives harmony to the univei'se, and explains the formation of bodies of all kinds.” Hewton held that “ Bodies exercise attraction in direct ratio to their mass, and that this law was of universal application.” Let us examine this. 88 Ttae circulation of tlie blood in animals is not affected by gravitation, nor are any of the secretions of tbe animal body. Tlie development in growth of animals is upwards, opposed to gravitation, and totally unaffeeted by gravitation. Tbe move- ments of animals in the performance, of their varied functions have no reference to gramtation. So also in the vegetable world ; the sap of plants rises from the roots, is distributed through the branches, ancT enlarges their size irrespective of gravitation ; the trunk of the tree aseends into the atmosphere and extends its huge limbs laterally, as if gravitation had no existence. The smoke from combustion, the exhalations from the earth, and the evaporation of water, all of them material substances, are in opposition to gravitation. Light, electricity, magnetism and heat, the vital forces of the universe, all treat gravitation with groat contempt. The atmosphere surrounds and envelopes, the earth. It has wluit is called gravity or weight, but it is not subject to what is called the law of gravitation, since when its lower strata l)ecomo warmed, they ascend into the upper part of the atmos- phere, and do not descend or fall to the earth, as having weight they should do; thus a difference in the relative weights of the same substance, in one condition or another, removes that substance from the influence of gravitation. The vapours or clouds in the atmosphere, which are heavier than air, float in many directions, and do not fall to the earth. A piece of iron will float upon a fused mass of iron, instead of passing through it to the bottom. The inertia of matter is opposed to gravita- tion. Form, which is . a force, ;and is the resultai\t of the forces that have produced it, is antagonistic to gravitation, which Ave illustrate Avith this example : suppose we have a cube of soft iron, Aveighing five pounds; let it be held by the hand OA'cr a pool of AA'ater; release it from the hand, the iron falls directly to the bottom of the pool ; our philosophers Avould say it fell by gravitation. Now, take that cube of iron, roll it out into a sheet of iron one-sixteenth of an inch in thickness, and again place it over the water horizontally; release your hold upon it; it sinks immediately to the bottom of the pool, Philosopliy says, by- graAutation. Recover it, and holding its edge vertically over the water, again AAuthdraw^ your hand; it descends at once to the bottom. Still by gravitation. Now, again take it_ from the pool, bend its edges up some six inches around it, in the form of a dish; then place its bottom on the surface of the- 89 \rater, release your hold, and lo ! it does not sink to the bottom of the pool, but it floats upon the surface of it ! It is no longer drawn to the bottom of the pool by gravitation, although what Ave call its weight is unchanged. It still weighs five pounds. Why does it not sink as before ? It is arrested by its form, which is antagonistic to what is called gravitation. G-ravita- tion, therefore, is not universal. It does not ahvays attract matter to matter, in proportion to its mass. What then is the repellent force which pi’CA^ents this iron dish from sinking ? It is magnetism. The water is magnetic, a condition produced by the electricity, whose opposite polarities in the oxygen and hydrogen meeting in conjunction, converted those gases, by . the combustion of the hydrogen gas in the oxj-gen gas, into the lirpiid state of water, and rendering the water at the same time magnetic. The iron dish, in contact with the water by its horizontal bottom, and having vertical sides, became mag- netic by induction from the water — the water and the iron presenting the same' magnetic poles to each other, mutually repelled each other, and the flotation of the iron dish was the result. . Flotation, heretofore attributed to the lightness of the floating body compared with the Avoiglit of the liquid in which it floated, is due to magnetic repulsion, and not to ^gravitation. Now let us look at the condition of- this water when it has changed its character by crystalizing into flakes of snow, of whatever diversity of form, or of hall, or of sur- fxce or dense ice. Thes'e forms of water at temperatures beloxv 32° of Fahrenheit, are all magnets, and their minutest atoms are all magnets, also; each endowed with its two poles, one at either extremity of the atom, and each Avith opposite, atti'i- butes. The commerce of the world, thei-efore,. is sustained on its oceans by the repellent force of magnetism; Avhile the mari- ner directs his course over their trackless Avastes, in darkness and in storm, guided by that opposite quality of the magnet which attracts it to the poles of the earth. Noav, when water, owing its form, Avhether liquid or frozen, to magnetism, is exposed to heat, and converted into steam, its magnetic qualities are driven off by the heat, and are re- placed by electricity, AAdiich is the force that rends the strongest fabrics of human skill to pieces, and scatters death and deso- lation in cAmry direction. The electricity of steam is of one 90 kind, imd is repellent of itself; and its effort to escape from itself and to unite tvitli the opposite electricity of the atmos- phere is so violent and so powerful that it furnishes to man one of tlie greatest forces with which he is accj[uaiuted. The forked flashes of lightning, seen ah.ove volcanoes in eruption, are merely the results of the conjunction of the positive electricity of the heated air, steam and lava thrown out of the volcano by violent interior forces, with the negative electricity of the atmosphere above and around the volcano. Rotary motion. of an object is antagonistic to magnetism, hy the production of friction with the atmosphci-e by the re- volving object. This friction evolves electricity, which, uniting with tlie opposite electricity of the revolving object, produces heat that expands and disintegrates its molecules, separating them, and removing the magnetism. As the heat of the sun (if it has any) cannot pass down- wards through ninety-two millions of miles of ether with a temperature of —-142° of centigrade thermometer, so the heat radiated from the interior of the earth, or proiluced oh its surface, or, in its lower strata of atmosphere, cannot penetrate upwards through the canopy of cold which surrounds the earth at various altitudes froih the snow line of 15,000 feet above the ecpiator, 6000 feet at 45° of north or south latitude, and at the level of the earth at 60° of north latitude. Let us admire the ineffable Avisdom of the Creator who, by a barrier of ice in the Arctic aijid Antarctic regions, confiiics the internal heat between them and the erpiator, and tije superficial heat of the earth below the region of perpetual snow in the atmosphere, for the uses intended by Him- of the- planet and its productions Rewton’s theory of centripetal and centrifugal attractions and repulsions is fallacious. There can. be no rotation on the centre of a sphere or spheroid, though there may be at the ex- tremities of any of its diameters or axes. ^Yhat is called cen- trifugal force is merely the repulsion from the axis of rotation and not from the centre. So centripetal force is merely axial attraction. Any force is the resultant of the forces which produce it. If there was, therefore, such a force as centripetal in a sphere or spheroid, the opposing forces acting from the ends of the diameters would neutralize each other, and an im- mense heat would result at the centre, which heat would 91 destroy the very forces which had produced it, and would prevent their continuance. ^ "^Hien we consider the repellent forces of the interior of the earth, such as heat and electricity, upheaving by volcanic action immense masses of islands and continents, changing in many places the configuration of the land and the sea, we cannot for a moment accept the theory of centripetal attraction or gravitation. The mean density of the earth is said to be about five times greater than that of water. If this be so, why does not this great density or mass of matter bring down the clouds by centripetal attraction or gravitation instantly to the earth? Why docs the atmosphere, still less dense than the clouds, re- main above the earth, when according to the laws of grarita- tion it should be precipitated upon it ? and why should the upper strata of the atmosphere be more attenuated and thin than the lower strata, which besides their own weight have the additional weight of the upper strata upon them ? There are no centripetal or centrifugal forces, as hTewton supposed. In the rapid rotation of a sphere or cylinder on its axis, the outer surface, by its friction with the atmosphere, evolves electricity, w'hich, in conjunction with the electricity of the atmosphere, produces heat, which insinuating itself among the molecules of the rotating body, expands'them and, if the velocity of the rotation is sufiicient, this heat loosens their mutual coliesion, and electricity being at the same time imparted to these molecules associated witli the heat, they are attracted thereby to the opposite electricity of the atmosphere, and the rotating body is separated into fragments with great violence, as the molecules of the mass, haring the same electricity, repel each other w^hile they are attracted to the opposite electricity of the outer atmosphere. This is the explanation of the bursting of millstones, grind- stones and other revolving bodies at great speed, as well as of meteors, shooting stars and comets, heretofore attributed to centrifugal force, blow, w'hat is there to attract at the centre of anything or to repel therefrom. The centre is an imaginary point, having neither length, breadth nor thickness, absolutely without dimensions, and consequently writhout matter — how therefore can it be invested with force of any kind ? There can be no rotation on the centre of any sphere, oylinilcr, or cone, or other solid or hollow body, as the forces ] ■.•f|aisite to produce the motion, would be antagonistic, and would destroy it, as the attempt might be made — conceive for a moment, that while the earth is revolving on its axis from west to east, you should apply an equal force to make it revolve also from north to south, the rotation would then be from northwest to southeast — now apply equal intermediate fu'ces between northwest and west, and northwest and north, and so on till you have equal forces for every degree of the hemisphere, and equal opposite forces from the other hemi- phere. This would be equivalent to centripetal force or attraction, and as these opposing forces would be equal, rota- tion would cease, the body would remain at rest, and centripetal force or attraction would not exist, consequently there is neither centripetal nor centrifugal force, and we must look therefore to other forces to explain the motions of the planetary and stellar Avorlds. It is to Oersted, the celebrated chemist and physicist of Denmark, that we owe the discovery that currents of electricity passing over a conjunctive wire, from one pole of the Voltaic pile to the opposite pole, produce magnetism. The meeting’ of these opposite electricities, he has termed an electrical con- jllclj’^' I sliould prefer ,to call it an electrical embrace, as it more resembles the ardour of lovers, in its attraction, than an attack by. force or. violence. From his experiments he con- cluded that the electric conflict is not inclosed in the conducting wire, but that it has around it quite an extensive sphere of activity, and that it acts l>y a vortical or whirling movement. A few weeks after the announcement of Oersted’s discovery. Ampere, by his experiments, discovered that two parallel con- j unctive Avires, from opposite poles of a Amltaic pile, attract each other, Avhen electricity traverses them in the same direction : and that they repel each other if the electric currents move in opposite directions. The sequel of Ampere’s labours shoAved that the reciprocal action of the elements of tAA'o currents is exerted in conformity Avith the line AAdiich unites their centres ; that it depends on the mutual inclination of these elements, and that it Agarics in intensity in the inverse ratio of the squares of the distances. Ampere finally succeeded in establishing that a conjunctive Avire Avound into a helix or spiral curved Tine, AAnth very close spires, is sensitive to the magnetic action of the. earth. For many AA'eeks there AA'as to be seen in his cabinet a conjunctive Avire of platina, whose position A\^as ■PIMIIl L.|, L 'Ill . I| I JLIWIIMII I 93 determined by the action of the terrestrial globe. Ampere ivv constructing a galvanic compass, had shown that the forces which act in the magnetic needle are electric currents, and by Ills learned calculations on the the reciprocal action of these curients, he accounted for all the actions which the conjunctive wire of the pile exerts, in the experiment of Oersted, on the magnetic needle. M. ^Arago, the eminent French astronomer, associated wit^ Ampere in some of his experimepts, says: coiled coppei’ wire for a length of two inches, _ from right to left, into a helix ; fhen an eijual length of wire in the same manner, from left to right ; and lastly, a similar quantitv again from right to left. These three^ helices were separated from each other by recti- linear portions of the same wire. “One and the same steel cylinder of a suitable length and of rather more than .04 of an inch diameter, and enclosed in a glass tube, was inserted in the three helices at once. The o-al- vanic current, in passing along the coils of these different helices, magnetized the corresponding portions of the steel cy linder, as if they had been detached and separate from each other , foi I remarhed that at one ot the extremities there was a north pole, at two inches distance a south pole, farther on. a second south pole followed by a north pole ; lastlv, a third north pole, and two inches farther on, or at the other extremity of the cylinder, a south pole.” Thus, by this rnethod, the number of these intermediate poles, which physi- cists ha\ e denominated consecutive points, could be multiplied at pleasure. M. Arago also observed, that “if the intervals comprised between the consecutive helices are small, the parts .of the steel wire oi; cylinder, corresponding to those interns, will themselves be magnetized as if the movement of rotation impressed on the magnetic fluid, according to Ampere’s idea, by the influence of a helix, was continued beyond the extreme spires of the coil.” As the conjunction of opposite electricities, according to these authorities, develops magnetism; and as tornaefoes, huriicanes, cyclones, and other atmospheric disturbances move in spiral curves from their respective points of departure till their terminations, and as, according to Ampere and Arago, currents of electricity passed through spiral cjdindrical coils ot wire develop magnetism, we see here the sources of the I supply of magnetism to our planet, its atmosphere, and the t 94 objecta upon or in them. This magnetism, so developed, is- absorbed by every object in nature. Being an imponderable, its presence cannot always be discerned or detected; but it resides in a latent form everywhere, till it is evolved by the opposite attraction or repulsion of some object approached to it which is also magnetic. In many parts of the world springs of water exist in which a great degree of magnetic power is manifested. In the state of Michigan there are such springs, in which, if penknives, or small pieces of iron, or steel, should be immersed for a few minutes, they would become highly magnetic. These springs ai’e visited and bathed in every year by thousands of persons for the highly curative influences over diseases that they exert. There is no magnetism in the earth pnder the erpiatorial regions, owing to the heat of the interior of the central parts of the planet, which destroys magnetism. This is proved by the magnetic needle losing its dip under the equator. I think, also, it Avill be shown that the magnetic needle has no dip over the G-ulf stream, as under that stream the interior heat of the earth has a flue extending far into the Arctic regions, through Avhich the Gulf stream is warmed, and magnetism in the eai'th about the flue destroyed; the same- vail be found to be true, also, of the Japanese current that runs througli Behring’s strait to the Arctic regions ; and of all other warm currents of water in the oceans. The eA’-aporation of the warm waters of the Gulf stream and of the Japanese current develops electricity, which, being positive as the waters thereof them- selves also are, they are both attracted by the negative elec- tricity^ of the waters of the Arctic oceafi ; and those currents flow in that direction. It will be found that terrestrial magnetism is irregularly distributed in the crust of the earth, and the magnetism of the Northern. Hemisphere being attracted to the South Pole, while that in the Southern Hemisphere being attracted to the Horth Pole, these opposite attractions have increased the . equatorial diameter of the earth twenty-six miles more than the polar diameter; and the earth’s crust under the equator hamng been thickened by the addition of so much material taken from other parts of the sphere, it fol- lows as highly probable that basins filled Avith seas have resulted at the poles of the earth, and that oceanic currents from the North and South Poles, respectively, are produced by the rotation of the earth on its axis, Growing off' the siir- plus of accumulated water at the poles, and thus the circula- 95 tion of water in oceans and seas is produced, in spiral curves rrom the polar basins. I have, in the former editions of this work, sim^ested that the rotation of the earth on its axis is the result of electrical torces within it, excited by the juxtaposition of the materials ot various kmds_ forming its composition, and having opposite electrical polarities. • I have an illustration at hand to prove this. A neighbour of mine recently erected in the rear of his house a one- storied dining-room, in which was a chimno}^ which projected some three feet above the roof of the building — which was 12 feet above the groun d — on the top of the chimney he jdaced a sheet-iron cowl in the form of a truncated hollow ellipsoid with spiral flanges from top to bottom of the cowl. ^Vhen there is no fire in the chimney .the cowl is at rest, Avhen a fire is kindled, as the air in the chimney becomes heated and, accompanied by its positive electricity,- rises to the top, it meets with resistance in the flanges of the cowl, which only begin to turn when the gather- ing positive electricity of the warm air attracted by the greater negative electricity of the outer atmosphere forces its .way through the openings and along the surface of the metalic cowl and sets' it in motion, and according as the combustion is more active so is the rotation of the cowl on its axis the more rapid, and the draught of the chimney is so increased that finally the flanges of the cowl can no longer be distin- guished in their rotation. So in the interior of the earth the intense positive electricity evolved there, in conjunction with the negative electricity also there in great quantities, produces enornaous heat, which fusing metals and disengaging gases of great volume and expansive power, forces them against the irregular surfaces of the interior of the crust of the earth, and sets the ball in its rotary motion on its axis. ‘ Similar causes produce like effects in the interior of the sun and of all the planets, giving them all the rotation on their respective axes that we know they have. With the electricity thus evolved and escaping as it is formed at their respective 96 poles, currents of magnetism arc evolved at right angles to the earrents of electricity and. cause the revolutions on their axes to be from west to east. There is no necessity, therefore, for our .^astronomers to suppose that the Almighty has created the sun to he an incandescent body, whose combustion is to he fed by half a world to illuminate the remainder.' The sun, in fact, is proba- bly only a huge reflector or mirror, receiving the rays of light from every orb, which rays themselves are of various tints, ns every planet and star has a colour peculiar to itself, and the groupings of these primary, colours in the sun, and their re- flections from him constitute the white light that we call sun- light. This explanation is in harmony wnth our ideas of the Divine economy, which imyer wastes any of its material. The siin is a great magnet, and regulates and controls by magnet- ism and not by gravitation all the planets of his system, which, consequently, are severally all magnets. The system is held in its place and conforms in its movements by its magnetism to the movements of all the ox'bs which exist in space. As these pdanets are all magnets, they can have no other heat than their own internal heat, which is simply sufficient to produce their respective rotations on their several axes, as heat in intensity destroys magnetism. The reversal of the tails of comets in their approach to the sun and departure from hiiUj is due to the attraction and repulsion respectively of their magnetic poles — by induction from the greater magnetism of the sun itself. Winds are simply currents of electrified air, repelled from their points of departure by air similarly electrified, and attracted in their various directions by air at rest or in motion, as it may be, with opposite electricities. These repellent and attractive electricities acting on a strong current of air, cause it to be deflected from its rectilinear direction, and to assume a spiral curve in its course, continually contracting towards its centre, till the opposing electricities equalize each other, •when the electrical equilibrium is restored, and a calm ensues. During the continuance of the movem'ents of the oppositely electrified currents of air in these spiral curves, magnetism is developed, and this is the source of magnetism in the atmos- phere. Magnetism in the crust of the earth is, likewise developed 9? ^ there ] ;^ r’.r: -onjmictiois of opposite electrkal_ cur. ents cir- ^ ciilatm^ cieev i;aily throij^h *t !Ci«s magnetism permeates % ^ tlu’ougii its various molecules, elippijiog them with .c!!.'- :etic attractiovt aco rcpnlsion, aud chus Tr aLcef, from its a-'i - opti- . bility 01 hococ dig magnetized, assumes the power ot’eUrao- • tion atfribni-ed to gravitation. Having thuB. shown the source froni which atmospheric as j 'well as terreeirial magnetism is derived, we proceed to men- 'f. tiou some of i 's attributes. The terra niagiietism, which is^ applied to the science that' I' describes the rnodcs and properties of a remarkable force pos- r/ repellent qualifies, is derived from a magnetic i''oii ore, .that was first noticed near Magnesia, and il; hence was. named by the ancient Greeks, 3 Iagnes. It had. the I'. |>eculiar property of attracting iron. This force is not con- fined to the mineral, but seems to pervade all' nature. It is produced by ine meeting of currents of opposite electricities in the- crust of the earth aud in our atmosphere. Its exioteneo ‘ in the fixed stars, in the infinite number of orbs, in the firma- j, ment, in the nebulas, comets, meteors, &c., may be attributed 5 to a similar origin. The primary rays of light from these f illuminated orbs, of greatly diversifica colours, passing with > almost incredible velocity from them to our sun, through ■ interstellar and interplanetary spaces whose temperature is i . inconceivably low, and consequently associated with negative electricity, developing as they pass through this attenuated t etlier,^ wliieii. fills these spaces, by friction therewith, negative f electricity, pisj be supposed to enter the photosphere of the r sun charged with negative electricity. This negative . .. clectridtv b. g homogeneous, of immense volume, and great >; iuteneitj, rep-f .. these commingled primary rays of light, by I", reflection trom the body of the sun on their impact with it, with the ei -ormous velocity which belongs to light. The mixture of these primary rays of various colours produces the. . white light of the sun, or, as we call it, sunlight. This sun- light, negatively electrified, driven wb h this immense speed to the most distant orbs of creation, encounters -in their atmos- i. phere, when such exist, and by impact with the bodies of i these orbs themselves, which have each a greater density than t: has^ the ether through which it had passed, great resistance. This impact produces friction, and friction electricity. r The friction of matter having a temperature above 32° of 98 ITahr-iulioit evolves positive electricity, wliile tliat of matter whose temperature is below 32° of Faliroiiisit evolves nega- tive '.‘Icefricity. When two blocks of iee are iol>bed together they iulberc by their contiguous- surfaces v, ii’' a foret; greater than cliiit by which the molecules of either u'-'cle (if ice are held together, and a Tracture of the ice wiU or. ur anywhere in tiii; Idocks before it will at their jun'-tiori. A notable illusi ranon of the fricticin of matter, belov 32 ’ ot Falirenheit, prodo.iug cold and its associate negathm eh ctricity, is furni ; lied every day in the manufacture of icnl .roams and juices of fruits. The cylinder contain mg the mr.ojiul to be frozen is placed in another vessel, surron mb d I',/ a iVeezing mixture of broken ice and common sahg ny iuruiug this cylinder rapidly in this mixture friction ie produced, which, in abstracting the heat from the cream ;u jirrees of fruits to be frozen, reduces, their temperature, and die cold of the freezing mixture, with its negative electricity, is transferred , to the cream or juices of fruits. We may infer an analogy between the composition of these, distant orbs of the hrmarnent and that of oar own planet, and tliat an opposite electricity to that of sunlight exists in them. The conjunction of thep opposing eloctriciti horoid or an ellipsoid, with its equatorial diameter longer than its polar diameter, thickened at its equator and ilattcuctles3 formed upon the same principle aa those on which the earth is established, and as we know that similar ditfer- ences exist between the eqxvirtorial and polar diameters of tVcrxe orbs to the extent of 25 miles in Mars, 6000 miles in Jupiter- and 7500 miles in Saturn, we may reasonably infer that magnetic attraction and repulsion have increased their erpiatorial diameters at the expense of their polar diameters ir. tb.e pi'oportions mentioned, and that like the earth they are all magnets,, and owe tlieir axial and orbitual rotations to magnetism, and not to gravitation. In this increase of matter in the equatorial regions of these planets of our system, we have the most conclusive evidence that the attraction of mat- ter in- these orbs is to their respective equators, and not to their respective centres as Newton supposed. "When we regard these immense differences in the equatorial and polar diameters of the planets, Jupiter and Saturn — ^that of Jupiter being 6000 miles, and that of Saturn 7500 miles, we begin to comprehend, in a sligiit degree, the idea of the Creator in placing these planets at such immensely great distances from the sun, while He invests them with a magnet- ism so transcendantly pO’iverful in its attractions and repulsions, that their revolutions' around the sun are performed with a marvelous certainty and exactitude. The law of magnetic attraction and repulsion between objects being inversely as the square of the distance, those distant orbs must have a propelling or repellent power at their greatest distances from the sun of almost infinite magnitude, to bring them within the attractive power of the sun, so as to pass over such immense spaces in their allotted .times. It is the repellent power of magnetism that returns them towards the sun. “Similiar poles of a magnet repel,, and contrary poles attract one another ; magnetic poles always occur in pairs. • If a magnet be broken into many pieces, each fragment is found to have its north and south poles. “Magnetic attraction and repulsion vary inversely as the square of the distance between the magnet and the body attracted or repelled. “ If in two magnets of equal strength, the north polo of one of thera be placed in contact with the south pole of the ott er magnet, all attractive force will disappear. Remove tl.e contact, and the magnetic force is restored in each of the magnets. . “ If a pole. of a permanent magnet is placed near to the end of a bar of soft iron, this bar will be magnetized by induciion-, the end of the soft bar next to the pole of the mac-net bavilic there an opposite pole to tliat of the magnets, while at the othei end of the iron bar will be found a contrary magnetic pole. Magnetization hy induction, he efFected^throug-h a plate of glass, wood, metal, &c., without detriment. This condition ^nnishes as soon as the magnet is withdrawn. “Besides iron and steel, nickel, cobalt, manganese, chro- mium, platinum, oxygen gas and inany other substances, suffer attraction by a inagifft. Heat powerfully inflrpcnces magnet- ism. A magnet if heated to redness, loses all its magnetism, and a red hot ball is not atttracted by a magnet. “ Every-.magnetic substance has its limit of temperature; thus cobalt does not cease to be attracted at a white heat: iron ceases to be_ attracted at a red heat; chromium just below a red heat; nickel at 350° Fahrenheit; and manganese ic not attracted on a warm summer day. Hence it is probable that certain substances which do not appear, under ordinary cir.- cunistances, to be attracted by a magnet would be attracted if their temperature was reduced to a sufficiently low degree. “A magnetic needle tends to set itself in -a line with the poles of the earth, and if moyed from this position returns to it, as if it was in the presence of another magnet. This is due to the magnetism of the earth— in fact, the earth is a huge magnet, the poles and equator of which do not coincide with the geographical poles and equator. “ The magnetic meridian of a place is a yertical plane which passes through the two poles of a horizontally suspended magnetic needle at this place, and which being continued in both directions will, of course, pass through the magnetic poles of the earth.^ The magnetic meridian of a place will not coincide with its geographical meridian, and the ano-le formed by the two meridians is called the magnetic deviation, variation or declination, at this place. “ The yariation of the needle does not hlways remain the same. In the year 1580 (the first year in which accurate 102 . . 'ions were made) the north end nf tlm needle deviated 11 ' ' to the east of the true north in London. In 1G22 the deviati >r. was 6° east of the north, and in IGGO the magnetic iiortli ’ ■■>(6 coincided with the' gcograpl'ieal north pole. In 1G0*2 ii had passed to G^ west of noi'th. In 1TG5 it was 20° west ; fU' i in 1818 it attained its maximum westerly deviation — 24° 41 . It is now returning to the north. In 1850 the westerly deviation was 22° 30'; and in Oetoher, 1871, the de- viation observed at the Kerr Observatory war 20° 18' 7''. This i: the secular variation of tlie magnevic needle. A deli- cately suspended magnet may be obsevsed to undergo an annual, daily, and even hourly variation. “ If a steel needle be accurately balanced about a horizontal centre, and be there magnetized, it will no longer be in hori- zontal -<|uilibi'ium. In'Loridon the north end of the needle will G’. :> down, forrning an angle of more than 60°, wnth a horizor.tul plane. The angle which a magnetic needle, capabii- c>f vertical movement, [dipinng needle,) makes with a horizo?; cal plane is called the angle of inclination or dip. The vertical ]dane in which the needle moves must coincide ^vith the ma .luetic meridian of the place. “Tlw dip varies in different parts of the world. If we convi'y a dipping needle north of London the dip increases-; if, ori" the other hand, w^e go south of London the dip diminishes; at the magnetic equator there is no dip, the needle 's perfectly horizontal ; and south of the equator the south ■'■'ie of the needle begins to dip, and the dip increases as w'c i ■ ' further south. Thus the dip at Peru is 0°, at Lima 1G° 3C'h at the Capo of Good Hope 34°, and at Hudson’s Bay behvec--; 89° and 90°. “•T'h' 'magnetic 'poles of the earth are those points on the earth's surface at wLich a dipping needle assumes a vertical position. The north magnetic pole. W'as discovered by Sir James Loss, in 1830. It is situated in longitude 96° 43' west, latitude 79° north. The south magnetic pole, is as yet, unknowii. “The magnetic equator of the earth is a line connecting all those places on the earth’s surface, at wdhch there is no dip. It is an. irregular closed circular line cutting the terrestrial equator at four points. The dip of a magnetic needle is subject to both 3«cnlar and periodic changes. Thus in 1576 it was 71° 61' in' London; a hundred years later, it was 73° 103 r 30', and in 1723, it readied a maximura of 74° 42'. In 1800, it had decreased to 70° 35', and in October 1871, the dip registered at the Ivew Observatory rras 67° 56' 3". The dip also undergoes annual and daily changes. “If a horizontally suspended magnetic needle be moved from its position of rest, it returns to it, passes it, and oscil- lates backwards and forwards across the final positioii of rest in the magnetic meridian of the place; in fact, it beconies a horizontal peiKlrdum" oscillating under the intluence of the earth’s magjietism. It has been proved that the intensity of the earttds magnetism, at any two places, is proportional to the square of the number of oscillatious made by the same magnetic needle at these places. “ Yarious determinations of the intensity of the earth’s magnetism prove that the force increases as we pass froin tho CHjuator to the .poles, as in an ordinary magnet. Thus if tlie intensity at Peru' he taken as unity, the intensity in London will be represented by 1.369, and at Baffin’s Bay by 1.7U7. ■ “All matter is affected by a powerful magnet, hut while many substances (iron, nickel, manganese, oxygen gas, &c.,) are attracted, other substances (bismutb, copper, hydrogen, &c.,) are repelled by both nolcs of the magnet. “- If a email bar of iron or other attracted substance, be sus- pended iioLweeu the poles of a magnet, the bar will set itself axkdbj, that is with its length in a line joining the two poles. If on the other hand a bar of bismuth or other repelled sub- stance bo suspended in a like position, it ^vill set itself oj'iatorb- ally, that is at right angles to a, line joining the poles of tfio magnet, because as it is repelled by both poles, it will endeavor to ki'cp as far away from them as possible. Such bodies are called dia- magnetic” In Professor Tyndall’s introduction to bis “Besearcbos on Bia-^Magnetism.” writing of Professor Faraday, be^ state^ “ That having laid hold of the fact of repulsion, he_ immedi- ately expanded and multiplied it. He subjected bodies of the most various qmdities to the action of his magnet; mineral salts, acids, alkalies, ethers, alcohols, aqueous solutions, glass, phosphorus, resins, oils, essences, vegetable and animal tissues, and found them all amenable to magnetic influence. N"o known solid or liquid proved insensible to the magnetic power. When developed in sufficient strength, all the' tissues 104 of f he hu.Vian body, the blood — it coi.t.d;! ; iron-^ inclviuud, .voi'o proved to be dia-ma^notic, so !lt.u d’y .u could suspend ft onar. between the poles of a magnet, 'his extrenuties ' would retreat from the poles, until his length dei iioic ecpiato- rial,” tliat is to say, horizontally peroendicular to the magnetic merhlian.. From the dip or inclination of the magneti(- needle on various jiarts of the e/u'th’s surface — as magnetism is a dual force — we infer that one of its poles is jiitraiitcd by the ■magnetism existing in the upper atmosphere, wldlo the other is attracted to, the magnetism in the crest of the earth beneath. At Peru the dip is 0°, owing itrobably to the heat, in the interior of the earth under 1‘fwu, Avhich is freqncrddy manifested in the most violent carilvi'mices and volcanic action, and heat we know destroys mar'-ruitir-m. As the dip of the needle in either hemisphere increases from the magnetic equator toward, the poles, it is obvious that the magnetism in the upper atmosphere, as well 'as in the crust of the earth, also increases in a like proportion, attrilmtablo cr atmosphere and' I he crust of the earth in high latitude, and as negative clectriciiy and magnetism arc both associated witli extreme cold, we find herein an 'Explanation of the dip of ibo im.ignetic needle. In the .attraction and repulsion of the mag.e.etic needle, horizontally, at the magnetic, equator towards tlm north and south ])o1g 3 of the earth, we have a dual horkionta! force. In the deviation of the needle cast or west of imrili or south, we ha.ve another dual force acting horizontally. Iii the class of siiiiiccts called din-magnetic, which arrange themselves at right angles to the magnetic meridian, or equatorlaliy as it is termed, -we have -another dual force acting horizontally. In the dip of the needle, which is nothing at the _ magnetic equator, hut whose angle with the horizon hicreasing there- . from as we advance towards either pole till it reuchos 90 ° or a quadrant of a circle, we . find another dual force with one set of poles in the frozen crust of the earth, wlnle an o}>posite set of poles is in the equally frozen regions of the arctic and antarctic upper atmosphere of our planet. These forces, with electricity and heat, all developed by light and controlled by the omniscient wisdom of the Almighty, are the powers which regulate the, motions of our planet and preserve it in its integrity. 105 TVe ■■•-y --ell dispenso^ therefore, w’"i' the wh.Me uieory or f centri i 1 : 1 iiii 'lcentrifiiejal forces, and of tlieaitracrt on of matte., r by wt •..!.■! I.-', 'doh continually is being change;: with tire fovihs ^ and l'- it assumes, the same subsrauce heing at ononme solid .!■’ : 'fixed to the earth, then liquid and tnoval.fie ou its ; surface ana again- gaseous and floating in its atia.Ocphere. I above It. In c.-nnoction with this subject of magnetism, b is ourioiib to ob: Li'. e that in the animal and vegetable ki gdoms the forms ->f -be productions all conform, in a groa;' ‘ :u;ie?f -v degree, b. ’he typical forms of ellipsoids, or oblate sphoroir..ir, as maniicsied in the planets. Examine the forms o'houi 'rees. Vcrtic;h cc; horizontal sections, when they a-’e in ;u)’ leai^ would dis' ir)i?A curved lines, which, if tangeutiai to tno ox- tremi: ■ < -f their leafy branches, would represent the cl nnents of an - -■ — in some cases elongated, in others nppr o'; hing p nearly O'- he form of 'a circle. So with thf.ir lcave«, l.-ov, over K- 'long and narrow tliey may be, the elemental character of. the ■ellipse is" .'oi.arent in them. The fruits they bear have >1’. similar ':;.;:::ieteristics. The apple, the peach, tho p'.ui, the £ apricor, ti'C nectarine, and indeed all the stone f-uits, haYO S. shapes -orresponding nearly to the ellipsoid. The nut-lx-ariug g trees, from the coeoa-iiut through the walnuts, hieko-ie-S, S pecan n^r.ei, chestnuts and beeches, all produce fruits which, S; in tbeir ou c •f'orma, piartake of the character of ellipr oid-Y or By. ■ oblate sj-;.ciY>his. The coffee-berry, the olive, the tig, the date, j all cogi espY.. •;! in their general forms to the sfime type. A moiig W ‘ what r;re cal -od vegetables, from the enormous mclnn, in' ail Ei. its varir it 8, Tlirottgh the pod-beariug plants,- the eabljago. ,&c., t tlie same tvjie is visible. So in the roots and tabciY,; the jt turnip is vn ublate spheroid, the potato commonly an cllip- r sold, as -y'y also the carrot and the parsnip. • In the seeds of t. the faTaily or grapes, as well as in their leaves, the same Ibrrms ' are fou . a The bunches of grapes, as well as their berries, t; are all t : In, same characteristic form. Take even the grh?..os -—in M’;i- 1:, nsny he included the cereals. Their long aed iiai t row h ■ . - Y n -.e all elliptical in form, though they may, in some i cases, be [-.T -ted at their outer extremities. TJiese long ieaves ' assume the ■'•rni of a eemi-ellipse, in their curvature iiom the stem er i^r-YYohes, from which they grow, towards the ground. ; So it is yvkh tl=e long blades of maize or Indian corn, the ^ugar > cane, and sorghum. The leaves, fruits and branches of trees, Y for the most part," have an inclination towards the earth, and are commonly pendant. Their tops are attracted upwards, I' 106 a'^: i are fro')sed to be dia-magnetic, and nnder the i'dluence o>.' the horizontal currents of magnetism that set aonatorially to the magnetic meridian; vddle the trunks a)' i ■■i..i:)iaits, re- psllcd by the rnagnetism of the earth, are attracted h}' the op- posite magnetism of the upper atmosphere, and ?Ae % orticallj. These t^^'o forces, varying in intensity, produce ali iho re.sultaut directions wldch their hVanches assume in theu development. Fruits of trees, being ellipsoidal in form, (which, is the^ com- mon form of simple magnets,) and generally pen , we might not now he compelled to begin anew the siudy of terrestrial, physics, after liaving abandoned the learned speeu lations of this celebrated philosopher How, in the animal kingdom, we will begin with man, wht», we flatter ourselves, is the highest development of animal lift. As he stands erect upon his feet, if wc suppose a vertical jdanc to he passed through his person laterally, the curved Hue so produced, tnngentiid to his prominences, would bo an ellipse. The revolution of that ellipse, on its longer axis, would pro- duce an ellipsoid. How, that ellipsoid is, during the life ol the man, a magnet, with opposite poles at its licad and feet, and various parts of his body arc , also separate magndts, but in harmony with the chief magnet. His legs arc a horse shoe 107 magnet, with the poles in the feet, and the five toes on each cf his feet constitute, for each foot, four horse shoe - mag- nets. AVhen, from disordered health, the magnetism is. either leg is no longer produced, paraij’sia of that limb v - ralfs, and the contractile and expansive power of the muscf?,- is no longer acted upon by the electricity of the system^ d no arms furnish another horse shoe magnet, and the five fingers jf each hand constitute, each, four horse shoe maguets, w tU f:. poles at the extremities.- The optic, nasal and auditory n- rves,- in each pair respectively, constitute a horse shoe magn j;. The genital organs are each a separate, hut very powert^ui anagnet, and are ellipsoids in forrd. In quadrupeds, the fore legs are a horse shoe magnet, as also are the hind legs. The split hoofs of the ruminants a -e also horse shoe magnets; so are the rounil hoofs of the ao-i’f.e, the ass, the mule and the zebra, with their poles pointing to the rear, instead of to the front. A lateral horizontal sec'l of a quadruped through bis head, neck and body, wov-ld o.^^elop an elliptical curve. . The jaws of animals are horse shoe magnets. A seipent, which is also an ellipsoich is a mag- uet, and when it is coiled, each of its coils preserves i' c elli^ soidal form. The same type runs through the feathei cd tribes, and the forms of the fishes everywhere partake, more or less, of the elementary character of the ellipsoid. In the investigation of this subject it will he found that the attachment of animals to the earth, and theiiTocomotiou upon it, are due to magnetism, and not to gravitation. . It will he observed, that in all animals, their bodies, which are their l.eaviest parts, are the farthest removed from the surface of the earth, which coiild not he the case if they were held to the earth by the attraction of their weight or gravity. As Kew- ton’s rule is that the attraction of gravitation, is proportional to the mass or weight, and, as the head, neck, body and thighs are the heaviest parts of the animal, they should bo nearest" to the earth, which it is known, they are not. ■ Fow, why is this type so universal — as well in planets as in whatever that has life upon them? Is it not because of mag- netism, that has developed this form and its modifications? Does hot the magnetism of the atmosphere control the move- ments of birds by its attractions and repnlsious; of the sea, which is highly magnetic, those of the fishes and marina animals which inhabit it; and of both the air and the land, those of the animals who live upon the land, and of the plants 108 which oro dcvolopc-fl in its soil? Magnetism, therefore, is an element of lito, in -plants and animals, and is one .of the motive powers of phinetary ami stellar -movemeuts in the universe. Let no\v rctuni to Moses and his book of Genesis. In i.lie 2(1 clmptor and 7th verse, he says: “And the Lord God formeti. muir of the slime of tiie earth, and breathed into Iris facet!)'.; i)! oath of life; and man became a living soul.” And ‘u the 2l - t verse, “ Tlxen the Lord God- cast a deep sleep upon Adam, aiiti wiioa ho was fast asleep, ho took one of his ribs and fio. ' uj) liosh f;.)r it.” And in the 22d verse, “.And the Lord i'(d built tiic rib wliich he took from Adam into a woma r;, n"d brought lier to Adam.” '\V'’hen wo remember the history o.f Misses, his birth of Israelitish parents, in the pro- vince of Goslu'u, bordering on the Delta of the river Nile; the at:. ‘mid of Jils motlicr to save him from the destruction decrc Oil 1) v" riiairu th against all the male children of the Hebrews, by plaei'tg :urn on the river ITile, in a water tight cradle made ■ of pai:yrr/s, among the water plants of that stream; his dis- covery bv li/liaraoh’s daughter as slie Avas proceeding to bathe in tlm ri-'mr near by; his delivery to his mother to be nursed and rc ir.id, till ho should be old enough to ho educated as the adept ‘d s >u of the I’riii^coss, who had 'discovered him iu the river; ids education by the priests, Avho at that period, as a- class, Avoro the iii.-yst learned persons in Egypt; his subsccpient aband.nim.ant of the court of Pharaoh, and flight into the desert, wlicri' ho passed forty years of liis life; his selection aa leader of bis -jieople in their llight from Egypt, and his resi- dence arrmng taom for. the last forty years of. liis life ; avo are not .sumo Iso'i that so learned a man, of such Amricd experi- ences, sf' aid have hocn chosen to conduct such a people as the Isr:.( ff)tc 3 out. of bondage, to a laud flowing Avith milk and honey. dn tbe l.cmplcs of Egypt, he had doubtless seen the priests oftciitiim-.i engaged in making their idols out of the slime of the I'iA'vi* mile. Perhaps he himself may have assisted in their man a fv.; rare. Ho must have had the lustory of his life im- parted t;,! blm, and the ooze of the river on AA'hich his cradle had re.itod must have been to him a familiar object. He kiieAV the p] art ic' character of its slime, hoAV easily it could be made toassaruo any form. And he AAms probably acquainted Avith the quahrios of the various materials composing it, A’iz : the cjarhonate of lime, from the bed of the river, the remains of flsh and reptiles, replete aauUi phosphates, and the vegetable tv. / • 109 matter, in almoa,t every stage of decomposition.' When, there- for*!, it was revealed to lam by the Almiglity that he had formed man out of the slime of the cartlx, he could readily understand that Divine power could faslxion^a mail our, :.f such luateuials, but the investing this man of ilesh mad ;l:' clay with life, by simply breathing into his face, was eucd ;i mn,ni-^ iestacion of power as must have confounded all his rensoning faculties. Let us see if we can form any idea of how this vitabzat’or- of the first man was efiected. Remember that this irj a reve- lation of a physical fact, and in communicating it to - ankind through the medium of Moses, the Cjroator did not ; can to make any secret of it, but has left it to us to -disco vcir if we can, without discrediting the act, or disbelievirg thr revela- tion. Let us suppose the first man to have boon made out of the materials mentioned, lie is complete in all his organisms ; they are all prepared; and ready to work. as soon as sdtality shall be imparted to them. This is done by “ breathi xg in his face the breath of life,” and “the man becomes a living souL” iNow, the first inquiry is, what is the breath of life ? Accord- ing to Moses, light had been created, the earth had received its form, the three kingdoms, animal, vegetable and x nnoral, were defined, and their functions were being performed, an atmosphere existed, and we may suppose that it ivas consti- tuted to fulfil all the conditions which appertain to it at the present day. Its elements were the same then as now. Light, which from the beginning had been passing through intersteh lar and interplanetary spaces, with its inconceivable velocity, had, on entering the denser medium of the atmosphere, pro- duced enormous friction, by which electricity, and subse- quently magnetism, had been evolved to perA’cn the parts assigned to them in the Divine economy. T. f eu Adam, there- fore, was finished in his structural condition, and tlio blood lay in his heart and lungs, arteries and veins, without motion, but ready for use, all that was necessary was to fill his lungs with atmospheric air, negatively, electrified, and life at once became established in his system. This was done by breath- ing in his face the breath of life, that is to say atmospheric air, which, conducted by the nostrils and the mouth through the windpipe to the lungs, and through the eyes and ears do the brain, and meeting there the blood oppositely electrified, the conjunction of these opposite electricities produced heat, which, eonsuminw the carbon of the blood in the oxygen gas of the atmospheric air, formed carbonic acid gas, thus purifying the 110 blocd .v^ It'S carbon, imparting to it a beat of 100° of temperntnre, pof itl ; 0 ' -lectrificd, and expelling from the lungs, through the movii'- ' nostrils, the carbonic acid gasAvhich has been ihus formo L The blood, after having been thus purified, rushed into iieart, driven by the positive electricity of the lungs, and fro vractioa of their muscles prodyr-e fVh'ijiSn and ! evolve nu ei^^etricity opposed to that which Las fu t Mmm hi motioti, a- -:, ;n. the same time, the conjunctic- «L' Lie- - oppo- site eh- : Iiioji aloo develops magnetism, wL'-ii once is acted voou p;, the superior magnetism of the eani<, ao i hen. e you ha, r a ;> g lifted from the earth. and anidhor pt ; - i upon it, in 1 cori -o ion, hy the force of magnetism, m l tb;.;. is ',‘e- peatui 0 ’ ; : : en aemued at the will of "the tuiinud. The cf -rhro :-od naturalist. Prof. Louis Agassiz, in Ids 'ecturea onEmijj , olOoV; stated, that tlio beginning of any o; l :ife vras i;i an egg. ).a - see if we can co nprehendits traotM-rotar.-on in:a > life. "Hie sevos are oppositely electrified. In tin,: Li-oton race the femaiesgirum .the positive and persistent ci'f' r-iotr.r of ihoir demands, may he termed positively electrif-a. TLo ma-es, . ■ from ti>eir h;ihit of negation or denial of the t o-mia of -he females, JP. I ih h is of too couimon occurrence, ji'av be terme i negatively electrified. These -opposing cordoions crer isi sexual attmet ion ; when a coumnetion of these eiM.op.'te ewe- tricities oc-oiirs in the act of coition, a certain d( - ci heat is developed, am] magnetism is ai lo evolved— the - , ler. gaged from the oveiri im is magnetiziol and positively J. t; - n- d, aud through tiie Eallopian tubes, enlarged by be .^, 1 ,'; of the coition, is carried into the uterus, prepared to receive if,' Thus, viiahond by the electricity and magnetir-m noo: been imparted to it, its own heat, and that of lim ohorus, ni which it is deposited, continue to preserve tho hfe which Las' i ■ thus been culled into being. Such, also, is the commence- y meut of animal magnetism. I Du Bois Tleymond states “that the electricaf o-.-r-rent man:- I fests itself in different directions, in the im.-i.a ; - different h animals, and with greater intensity in some . duinlr than m §. others. The electro-motive forces thus operating in the m:-.-?- cles depaud upon the opposite electrical [? mam- ■n-'’ oondi tions exim: eg between their longitudinal and tw^c .v^foe sum y tions.” fcv;- duo, with respect to the nervous 8ysv:on, he stati s that the nerves are subject, in their sectional arrangoruents, to the same law as the muscles. This must he understood, hov- fV ever, with reference only to the exercise of their inherent elec- > tro-motive fcirces. In transmitting the miiscuiar current the . nerves perform the part of inactive conductors. It ,8 not in fe .the whole, or a large part of a muscle, that an electrical cur- rent can alone he shown to exist, but that every nu.rticle, the iDorest or fragment, _ evorr what_!i»ay hr luio V . IB eg’icvily obedient to eJeetrical i'jverv rnovemoet; look or gcstnre, every I'aii or pieuBure, every en)otion however tranvo-i lians ovf' V tltought nhexpressed, or word uttered, v-. ed'v at fomitanied by tbo msturhunoe of e)eeir..-pu TiicBe, ii' Avevcr, are so much more feeble rlia<\ any wr have hitherto become acquaiuted, ihat in the ’ ^ roosc active, during a week, or perhaps a moty •, lativa etfects may not be equal to those evolved : j Mow of the hand upon a table.” CO .1,' ,j; ' i I i ' i ai\' ^vil : a! i;ci ii/idcrcd ition of ,iid per- r '1 assur- e ibrees. li which I lest and r cumu- !<:■ smart Much specnlation has been evoked and varinas ,:pc:’uuents at. different times instituted, to discover and e>q bv- * i !k- cause of the uniform normal heat of the body of a heaitby tViclt per- 30U, hut heretofore with unsatisfactory results. hTotvy it "jeems V - me that the exi'ilanation is not a difficult one. .u ^yul be f=duudod that the relative capacity of the lungs -o farmsh at- mospheric air to oxidate the hlood_, and of the bieart to supply the proper quantity of blood to lie so oxidated in dio tiuigs, is. constant V;; a healthy adult. When, therefore, the lungs are filled to their greatest capacity, with blood ami atmosphonc air in diffusion through it, the meeting of the imgalme elec- tricity of the air with the positive electricity of tae bnood in the lungs, develops heat and magnetism, and fho omdated blood becomes positively electrified; the carbon of the blood unites with a portion of the oxygen of the air in iiie .amgs, and becomes carbonic acid gas, also positively eioctrifiect. This change also develops heat and magnetism, having^ been produced by the meeting of opposite electricities: a portion of the water of the blood, separated from it during these clianges is taken np hv the carbonic acid gas; and the carbonic acid £ras and the oxidated blood, both being positiv(dy electrified, romd each other— the blood back to the heart, to be thence diff rihuted by the arteries through the system, ivhim the car- bonic acid gas, and the. -watery vapor it contains, are expired from the lungs through the mouth and nostrils into the atmos- phere. This repulsion of the, carbonic acid gas and watery vapor from the lungs is obvious to every one. For who is there that can hold his. breath even for a single moment t A. greater poiPer than man’s will forces them from tlie that is the repellent power of positive electricity. Ihe oxi- dated blood is driven into the heart by this same repellent force. ■ It is the electrical action, therefore, in the lungs of the at- mospheric air and the blood intermingled in constant relative 113 ^| iAnatios, that produces the unilbrm temperature, in all Ltl i r !3, of 98° Fahrenheit in a healthy adujl person. , Electricity is the cause of the fluidity of the blood in th' and arteries. Venous blood taken fronx the veins, ami eft to itself becomes solid, and separates into two distincx par.::; tlie serum, or watery, being over and' upon the clot or o igalum. The serum is chiefly water, holding albumen in sol*; iion and the salts of the blood. The clot contains fibrin cokring matter, a little serum and a small quantity of salts. Pi k't- a finger with a needle, a small drop of blood exudes. ' It i ^ negatively electrified ; on being exposed to the air its nega- tive electricity instantly unites with the positively eleetritr.u . uiv in contact, with the warm surface of the finger, heat is p-oduecd by their conjunction, the watery part of the scnini is. evaporated ‘by the heat and the distributing electriciiii.s ; M.i-d the clot remains to cover the puncture made bv tlie' needle, and to protect the blood in the vein from further injury by the action of the air upon it. How many lives have been saved after unconsciousness, from the loss of blood, in woixnds, has seized upon the sufierer, l)y the escape of th; svnvn of the blood through evaporation from electricity, anu hio deposit of the clot upon -the lips of the wounds, closing toeru and preventing the further flow of the blood throngh them, and thus allowing nature to gather up its remaining strnngtu, and to restore the patient. How thankful we should be ro the Creator for this siiiiplc, wise and benevolent proA'.i- siou for our safety in the occurrence of blood-letting injuries ! A?i, eminent surgeon of my acquaintance has informed me . in cases of death’ produced by lightning, the blood ro- feiaiurA fluid in the veins for several days afterxWds-; whereas. gsesB of death from disease, tlie blood coagulates soon aitor- ar.l,;. He has known a ease in which the blood remained in the veins four days and several hours sub.sequent to* i,yi_eath of the man by lightning. This- ^oos to show that in opco of_electricity from the blood, its flow in the arte- Mtid veins becomes retarded, and its coagulation, or cx en " ening, would suddenly terminate the life of an animal in oso is fimec-’ Her attendant, astonnded by what at first re U nught was intended as a.grek indignity to the lady, war a..oMy,o re- sent it when he heard the explanation whicli accomp:.Vi^l m. .The Emperor Nicholas; for k was he, ^^f’lto.ruo hn..ry nr, 30 and hice of the lady with his hand filkd wndi sno-r to re- store, by h’iction, the proper; circulation of the blovu end thus prevent the great injury to the lady’s face whnhi the luss O' her nose would occasion. lie spoke encouragingly to a-n’, aiii... calhng an attendant he sent for his surgeon, and atten mo cir- culation of the blood in ber face was rc-cstabiished, she wa^ re- turne;l to her apai’tments, wliere she received e’ on ati-ntiou; ■bv the Emperor’s orders, and'in a little while she was- oplirely restored VXVJ. w . Iow,'.why did the Emperor rub her nose .... 1 face is iiand with snow ; and why did he take off- ms glove fnmi ta perform that office ? It has been long known, that frozen limbs can be restored to tliCir normal condition .of healthy vigour by the applicatioii of snow or pounded ice to the part^ aflected, when quickly rubbed with the human hand ; but it is not so well knov n why such an effect is thus produced. Let us essay an explanation of it When a limb, or member is frozen, _ the carcuiation of the i)lood in it ceases, and the life of the Imib or niem^ier is suspended; and unless its healthy action is speedily rcsiored. fill I >.J I *111'/ i^v|^PW>^'i'^i||,iPiJimMi9WUI^ tlio part -afFectcd loses its vitality, gangrene sets in, and ampu- tation becomes necessarjn The .animal electricity tlmt it con- tained has disappeared. I^ow, the human hand has one kind of electricity; snow or ice has the opposite kind of electricity. When these opposing electricities are brought together in con tact by frictiop, as they were in this instance, heat and mag- netism were evolved, wliich Imat warmed and expanded the i’rozen nose, and associated with the magnetism that had been developed, excited air electrical current in the coagulated l.)lood. in the veins of the nose and face, which then began to How in its natural course. When this friction is thus con- tinued for a sufficient time, the health of the limb or member is restored, Now if heat from combustion had been applied in tins case, instead of heat from electricity evolved by fric-. tion, as above described, it would have resulted in the morti- fication and loss of the lady’s nose. It has been abundantly shown, by experiments made by distinguished scientists, that, under the iniluence of weak cur- rents of electricity, salts can be resolved into their component elements. In this way a compound can bo separated into its constituent acid and base. It has also been shown, by Becquercl, that if an acid and alkaline solution be so placed that their union is effected through the parietes of an animal membrane, or, indeed, of an}^ other porous diaphragm, a current of elec- tricity is evolved. This has been found to be true with all acids and soluble bases. Now, Dr. Golding Bird asserts, that with the exception of the stoniach and ccecum, the whole extent of the mucous membrane, is bathed with an alkaline mucous fluid, and the external covering of the. body is as con- stantly exhaling an acid fluid, except in the axillary and pubic regions. The mass of the animal frame is thus placed between two great envelopes, the one alkaline and the other acid, meeting only at the mouth, nostrils and anus. Donne, has 'shown that this arrangement is cjuite competent to the evolution of electricity. ■ ’ . The blood in a healthy state, exerts a well marked alkaline action on test paper — but a piece of muscular flesh containing a large proportion of alkaline blood, wdien it is cut. into small pieces and digested in water, the infusion thus ob- tained is actually acid to litmus paper. This curious circum- stance is explained by the fact announced by Liebig, that, although the blood in ■ the vessels of the muscle is alkaline from the tribasic phosphate of soda, yet the proper fluids or I secretions of the ■ tissues exterior to the capillaries are acid ns from the presence of free phosphoric and lactic acids. Thus in rvciy mass of muscle, we have myriads of electric currents, arising from tlie mutual reaction of an acid fluid exterior to the vessels or their alkaline contents. It is thus very remark- able, that a muscle should be an electrogenlc ap'paratus, and ■ that we should have two sources of the clegtricity of the muscles — the eJEFccts of metanuvphoses of eflhte fibres’ on the one hand, and on the other the mutual reaction of two fluids in different chemical conditions. The agency of a muscle iugenerating electricity can no longer bo denied. In the course of twenty-four hours a considex'able propor- tion of watery vapour exhales from, the surface of the body. This has been differently estimated, and is liable to great va- riations — but from 30 to 48 ounces of water may_ thus bo got rid of from the system; The evaporation of this amount of fluid is sufScient. to disturb the electric equilibrium of the body, and to evolve electricity of much, higher tension than that set free by chemical action. This evaporation may proba- bly account for the traces of free electricity generally to be _de- tected*m the body, by merely insulating a person and placing him in contact with a condensing electrometer. Pfaft’ and Ahrens generally foupd the electricity of the body thus ex- amined to bo positive, especially when the circulation had been excited by partaking of alcoholic stimulants. Ilepmler, another observer, found that in 2422 experiments on himself, his body was positively electric in 1252, negative in 771, and neutral in 399. The causes pf the variations in the character of the electric conditions of the body, admit of ready ex- planations in the varying composition of the perspired flxiid. P' 'r if it contains, as it generally does, some tree acid, it, by its evaporation, would leave the body positively^ electric; whilst if it merely contains neutral salt, it would induce an opposite condition. The accuracy of these statements can bo .ea-sily verified by ?neans of the electrometer.” o It is an established fact that, independently of combustion, chemical action. or evaporation, the mere contact of heteroge- neous organic rnatters is competent to disturb electric equi- librium.” AVhatever may be the influence of electricity as an agent in exciting the function of digestion,' it is now pretty distinctly . .made out that the function of digestion. in the stomach is an action allied to simple solution, of which water — a' proper temperature, [always associated with eleeti-icity] — and a free acid, the hydrochloric, phosphoric, or both, are' the active 117 audits. TT^e possess sufficient evidence to induce us to resrard a current of electricity as tlie means by Avhich the saline 'con- stituents of the food ‘are decomposed, and their constituent acids, the real agents in digestion, set free in the stomach, the soda of the decomposed salts being convej'ed to the liver to aid the metamorphosis and depuration of the portal blood, and cause the separation of matter rich in carbon in the form of a saline combination in the bile. • It also appears, from various expteriments, that in all cases the secreted matters are ahvavs in an opposite electric condition .from that of the blood from which they were generated.” Chemical action is merely a synonj-m for electrical action, hence in all tlie functions of the animal body from its birth till its dissolution, we may observe the influence of electrical currents, the development of magnetism by the conjunction of them, oppositely electrified, and the production of heat. In the first inspiration of atmospheric air into the lungs where it encounters the blood oppositely electrified, lleat and ■ raagnctism.are evolved, and the purified blood has one' elec- tricity which .repels itself into the heart, and thence *v the arteries through the system. When it reaches the capillaries it has lost more than two degrees of its temperature, and being forced through the capillaries into, the veins as well by the repulsion of the electricity of the arterial blood, as attracted by the opposite electricity of the veins and the blood they contain, die temperature is increased till it reaches 98° of Fahrenheit’ which it carries -with it to the heart. Muscular exercise actively employed by the contraction and expansion of the muscles, and by their 'friction among them- selves, develops large quantities of electricity, which requires a corresponding quantity of the opposite elckricity of the air •to neutralize it, hence the inspiration of atmospheric air into the lungs becomes more rapid in proportion to the activity of the exercise, great heat is developed in. the body by' the con- junction of the.se opposite -electricities, which expanding all the tjssues of the body’, liberates the water contained in them and in tiic viscera by exos mosis, which then exudes throngh the pores of the skin, as perspiration, carrying off the surplus e|ectrieity that has been produced by the violence of the exer- cise, and relieving the body from the further inconvenience of its increased heat. This perspiration is acid in some parts of the body and alkaline in other p>arts, and. furnishes the most iramodiate means of getting rid of the excessive, free currents of electricity of the body , at all times. IIS Dui'lr.g an attack of fever, vliilo the patient is sufiering from tlie great interior lieat of his body from disturbed elec- trical action, why does lie continually ask for cold water ? It is because the cold Avatcr, oppositely electrified to the over- heated organs and viscera of his body, is demanded by the instinct of his nature, which requires it, so that the increased heat developed. by the conjunction of these opposite electrici- ties rr;ay still more expand the tissues and viscera and liberate the water therefrom which, mixed with the water drank, would carry otf in perspiration the excess of electricity and restore the body to its normal condiiion. For this ycasop, cold water in largo quantities should always be prescribed in cases of fever, to carry off the surplus electricity, by the perspiration it induces, as Avell as to supply the material for the very perspiration that it is intended it should produce. Warm saline or acid baths, by expanding the pores of the skin, and thus promoting perspiration, are natural remedies in cases of fever or of violent inflammation. Perspiration, therefore, alkaline or acid, is the remedy for excessive elec- trization — and just as the perspiration is either alkaline or acid, in those places of the body where in its natural state it should be the reverse, ought the X'hysician to be able to diag- nose the causes of this abnormal condition, and to restore the electrical equilibriuiu in the system. The sexes are oppositely electrified— -hence their mutual at- traction for each other. Fowgive them the s;n iv; clectrieitiLS,- and runtuai reqmlsion immediately results. Let us ponder avs'hi’o oil this subject. Every one must have observed iu the prers of this country, alrn(i.st daily, and iu every jaart ot it,^ acemauts of the most outrageous, cruel, and in some ca.sos ot diabolical attacks of men upon woinen, and occasionally, of women uxion men, generally wl len they bore toward caeli other the relation of husban'd and ivifo. V\^ben they have been first acquainted with, each other, their electricities being oiq>o- sitc, they were mutually attractctl to each other, their acquaint- ance grew into esteem, and ripened into affection and love, and they became man and wife. The animal systeni develops electricity, magnetism and heat in its functional aefions— the kind of electricitv and magnetism are ' dependent upon-- the ' habits of life, the diet, the occupation and association of the indi vidnal. 'When these are similar similar electric and magnetic conditions of the liody will result. It has been shown that the ne»-ative or masculine electricity of the man is. reversed, ami becomes positive like that of the woman under the excitement of alcoholic stimulants— in other words, for the time being, 119 the TTifi.r l>r-eomos a woman, and is converted into the onl >" thing wi h lx the British Parlianie'nt, in all its great potentialitv, could not do, viz ; make a man a woman, .or a woman a nia::. This, alcoholic stimulants have always done, and are now doin'.; ever}’ 1 ry. dTien this change in the condition of his electricity has :-'r'‘iTed, his attributes become feminine; he is irritable, irrationa', excitable by. trivialities, and when opposed in hi:) opin' n; 8 or conduct, becomes violent and o'ulrageous, and if, ■ in thi ; n, ;.;>d, he meets his .wife, whose normal condition of electri'.ily is like his present condition, 'positive, they repel each >. ‘d': r, become mutually abusive, engage in' conflict and deadly ; i rii-b and tbe newspaper of tbe next day announces tho- verdi : -. c - tiw coroner’s jury on the case How many such, in- ly cidcio c are occurring dai ly in almost eveiy part of our extended country - and wbo would expect to find tbe discover}" of- the moving cause, of all, tbesc terrible crimes in the persiflration of . the c’ir..iiuari, and yet science has shown that, the metamor- phosis of a tvian into a Woman by changing the negative coh- ditioii of his electricity into the positive clcctricrity of the women, witli. all its attributes, is disclosed by the character of his superinduced by the use of alcoholic stimu- iaiits ’ .Xt is a very curious thing to note, that among the Per- sians, mcjlkthc most ancient of peoples, the ordinary saluta- i.iou cr ' bo meeting of friends, is, not as among the English, ■ H-v.: ? o you -bo ? ” as if your. life was one of incessant labor, or as i-wong tf>e Prencb,.‘‘ Comment vous portez-vous ?” How do y carry yourself? ” as if it wws a. great exertion to move at ab — i,ui: 'Ebow do you perspire? ” In the lapse of ages, :i :vst O'- i of knowledge useful to a people, is neoessarih- ac- re ynired-fy iboir experience, personal as well- as nation a.!, jn dm hoi: and arid climate of Persia, the people sufler, and bavo ■ aPwv ■ sufibred, greatly from tbyers, eruptive disease;: of iho skiU; as we!i as from those of a dysenteric and choleraic char- fl, acter. Their experieuco has taught them, in . their dhioases, that rfc frst relief from sufiering that they felt, was h-- the re- turn of their perspiration to their skin, and as long as ihat perspir-ation .could bo maintained, just so long was tlicir relit f ’ continued—pb cr.ee they came to regard it as synonymous with a state of g'.iod health, and the salutation among friends on meeting was inti’oduced and became common among the b people. , Lot no woman, hereafter, delude herself with the idea that * she cab rotf.rm a man addicted to the use of alcoholic, stimu- lantr. by marriage. Should she attempt it, she will fall a victim to bie deiusion, as many of her sex have done before 120 ' or, as f lio willlind that her wiil is controlled by her r: r.pr-n' ■lositive oleclricity, wliich is of* the same character iis tliat bt the lann, her husbancl, and that, in spite of herself, the two w’U e- nintually repellent, and their association as man and wife will he utihappy in the extreme. Observe a drnnken man with a male companion wlio is sober; their electricities are opposite ; how loving the drnnken ' man is tb his friend ; he caresses him; locks his arm in that' of his companion ; hugs him ; in France he would klsr him; jirattle.to him- with the simplicity of a child; talks iK .wcnse yrith the incoherence of dclirinm ; and is as good hui-norc'- raid amiable as possible. Ilis. wife appears on the scenr ■ his nianncr changes instantly; she tells him he is wanted atimnn:; and asks him to. accompany her there ; ‘he replies, “ yon go tz yn ass, don’t you see I am with George,” naming his con pauion. The wife urges him to go home, and not expose himself in nie - public streets in his bo'ndition. He is ■ exasperated ; tlio^o re- pellent electricities are in action; they become angry; vio- lence probably ensues, and the police interfere. Let no woman ever venture to remonstrate wdth a drunken nian ; her own electrical condition forbids it ; such remonstrance irritates the man, develops bis anger, and leads to violence ; and whm it is remembered that woken arc particularly the objects of bratal r.ttack by drunken men, as is made manifest by the pul;!" cation in the daily press of the country, of crimes that have been committed, it is obvious that their safety will be jprometed by their silence. . ■ The remarkable variations in bis own electrical condition, ■ reported bv the observer, Ilcmmcr, as' deduced fromjns e^xTcri- ments upon bis own body, go to show that every iiKudouj in • human life might be trace'd to its electrical condition ; all the passions are excited by it, and are skhdued by its reversal: all tlie emotions are necessary consequences of it, and it not probably going too far to say that the intellectuality of man is largely 'due to'his electricity and maghetism. ■ We have thus shown that from the impi;egnation of the ovum of the warm-blooded animal, through its whole existence, clcc- tricitv, maqmctism, and heat, arc the essential, elements^ of its vitality; and that starting from the first man, Adam, it,. was not until the Creator had “ breathed into his face the breath w f life;” or, as We. interpret it, had brought together the atmos- ikeric air and the blood in bis luipgs, oppositely electrified, I'V breathing that atmospheric air into bis face, t rough his uioutb, nostrils, and eyes, and thus bringing it into contact 121 vfitli the oppositely electrified blood, that life in Adam ^<"3 cstabh - lied, and the law of life made universal for all li‘ descendanta. It is curious to observe tbe marvelous provisions ma^ie by tbe Jreator to relieve tbe human animal from the ex. oss of elcciric-al action in his system from whatever cause. The bral being tbe most important of the organs, and contained in a bony structure called the cranium, or skull, composed of severed par:s united bj" serrated edges, and subject to a certain degree of mobility at those edges, to protect the skull from fracture by t) i ial, accidental blows, or pressure, is the first organ lo h-i relic.'cd from increased heat in the blood v:hich circulates there.- Perspiration first breaks out on the forehead, r cur tbe temples; then at the uppermost suture, or serrated edge, =>n the top of the skull ; then along the temples ; then behh-d - he cars, i;o relieve the cerebellum and the organs of hearing; th en abo> o and below the eyes, for the relief of those orga'is; tb m- along the nose and corners of the mouth ; then under t ae jbie o to re'^eye the glands of the mouth and throat; the ihornx, ur chest, where the greatest activity of the circulation of the bloi; ■ occurs, is relieved by the perspiratior- in the armpi'-Sr unde, the shoulders; while the abdominal region is protected by iivi exudation in the loins and groins, and the pelvis and Lips have their guardian in tbe pubic region; the u->per log io the angle behind the knee, w’heii it is bent ; the lowc- log and foot find their security in the perspiration that exudes bet\veen tbe toes, as the lower arm and hand are protected by it, -'is it escapes between the fingers and in the palm of the hand — ^^ail these sal utary provisions are independent of the wfill of the indi ^'idual, and are so many safety valves for his preservation from ivjjury, in too many cases, from his own in^rudcnce an folly. . It is to the female of ever}' species that the Creator ha.: conib.-ou the care and perservation of the young anin'vl, n.a well as the continuance of the species to wlricli she m \v be- long. ~We all know how pow'erful is the emotion of matorna' instinct ; it needs no illustration. Am*!iig all animals'but man the season of reprod'icrio;-; ir deper,f:ent upon climatic infiucnces— upon the temperature of the season, w'hcn the young animal is to he ushered into li fo, and ;m the products of the earth necessary for the nn-thrr’ during the period of its dependence upon her for sustenancin as well as for its owm support afterwards. W e will illustrate by a common example. . We will suppose 122 • l il season for rcproclnetion with the domestic c^.c has 'veil: Kpe is at pastime, and unconscious of the clianicc in i.er CL'ftilition which is about to happen. Suddenly, there yins to he given out from her body a strong effluvium — it e ii roucs'ls her and accompanies her in evcrymiove.ment. It fills the atmosphere near her — ^ivafted by the wind it is ( arried t a great distance. A mile or more to the leeward the < . \v, a bull is feeding among a hundred cows, in tl;e pricturo field; grazing quietly he is observed to turn his head towards t‘je direction from which the wind is coming. It marlcs tho fret approach of the effluvium; he turns qnickl/ around towards the' wind, raises his head high above hi-- fody and drav's a long inspiration of air. lie recognizes the tVagi ance, it is to Idrn an invitation. He sets out in a rapid walk in the direction from which tho wind is coming; then he quickens bis pace into a fast trot, and, as the welcome perfume incrcasos in strengtli, he breaks into a gallop, and then into a fidl A rbneo, a barrier, intervenes ; raising liimscU' on liis l.biid IjcoIs ho throws bis forehand on the fence and breaks it ic the groin id. Eenewing bis speed bo arrives in the iicld in wliieh Ibo cow ds quietly grazing — among a tbousatid cows. Ho follows the fragrance directly to the object of hi:- visit. How, V'hat docs this ba^te mean? "Why docs be loavdii ' own Tomtui-c, a mile or more away, to rush with such sf cod to (vriie ■ fKlds ? Tlccausc a new life is to be developed, and the muis; >ci-co]e elements of it are heat, electricity iuiu mag- uetdr u The exercise of his muscles in running has prodncecl tVktion, .fdetion has developed electricity, positive, ivldcli de- rnouds negative electricity from increased inspiration of the- atiric-sjhere. His imagination has been excited by trie pun- gcncT of the -grateful aroma he. has breathed, lie arrives' at ti:G co-=v, dra."s u long inspiration, licks heron the iicckwith ],.$ rough. f.»ugue, and upon her loins, and makes an ofFort, as b upitcr is said I o have done to Europa, after crossing the Bos- phorus. The cow recedes from him, and he is disc pixuiitcd — sb.' is p.ot ready. Again and again -he proffers his divotion — Ft’ll rqicetcd. "The cow, in tlie meantime, recedes from him a : paces, aiid\hegins again to graze. ^ Every momeut, how- ever, her maturity of passion is approaching, the circulation of her blood increases, stimulated by his proximity a ad the oxlour given out from his body. Heat and electricity iu her V»ody aro developed by a quickened circulation, and when tho instinct of her aiatiire has been fully aroused she coinmuui- cates to him, iu a mysterious way, her readiness to receive, iu ii'O *angTiagG of the Latin poet, “ taurum ruf.ntetn in ilic eleinents of life are there, cl cctricitT, magnetism ancL -icat, and at the end of the period'of gestation, a new life is added to tlie herd. . Among birds and ponltr}', the requisites for reprednetion are similar. In the poultry yard observe the gallant cock. Scriitchingon the ground he finds a grain of corn, br.potdianco an insect; he gives a chuckle and one of his hens api>roarhc -3 to receive it. She picks it u]\ and comprehend:' ’n the generous motive of the gallant bird, she starts off in s’ r^m to enjoy the gift. The cock piu'sues, and after a si— y and quick race, in Avhich friction, electricity, heat and mn o', q.siu are developed in each of them, slic .suddenly stops, an en'to-a'-.o follows, and an egg .is impregnated, which in due tirue- is hatciicd into a chicken. SoTnetimes, the cock pretending to have found some choice niorsel when in fact he has not, calls a hen, who on aj-oroac*;- ing him discovers the cheat and starts from him on a rnn to be purlued by him as before, and with precisc’y a -bnilar rysnlt to the last mentioned. So that to be a gay docif ■, cr of ■the female is not confined to base man. ■ In the reproduction of all the varieties of animal life from the enormous whale to the firefly, wldoli in the Icvguage of Tola Moore, ‘Mights her mate to her cell.” and frondi*: f b the tiniest insect, the like conduct prevails^ viz': theexerei: v i f the rriu-' Ics producing friction, and evolving clcctriei fy, magr;etism and heat, to vitalize the ovum in its impregnation. The whale requires three-quarters of an hour to be • -sod in sportive dalliance around his mate, before a su". ient degree of electricity, magnetism and heat can be attu . ,d to impregnate the ovum of the female. I have been credibly informed by a very intelligent man, wiio was for many years ‘ engaged in the whale ti.sher;- ::c tlie Southern Pacific ocean and Australian seas, that while cruis- ing for whales off the coast of Australia the boats of Lis ship pursued and captured a large sperm whale that made :*0 bar- rels of oil. That when first struck with the harpoon lie went down with great velocity, carrying with him an immense length of line, and that befoVe he arose again to the suj-face “ to blow ” one hoxir and iioenty-three minutes by the shijr -- chro- nometer had elapsed, which fact proves that it is not iiecessury 124 for a Tvhale to come to the surface of the water at ^hovr iutervals of time to breathe, as naturalists suppose, ti.- from the lapse . of time mentioned while he was under the water he evidently had supplied himself with atmos- pheric air for breathing purposes from the water, as it was impossible that any pair of lungs could have inhaled and re- tained sufficient air before he went down to sustain him for 60 long a time under water. The true explanation; probably is, that the whale came to the surface to blow off, with his car- bonic acid gas and watery vapour from his lungs, the Bur[du 8 electricity that liad been evolved in his system by the imiuense muscular action he had displayed in his descent from, and subsequent ascent to the surface, as ' by no other method could he have gotten rid of it. Among terrestrial animals nothing is more common during the beats, of summer,' wheii so much electricity is evolved will tin them by their inspiration of air, the circulation of tlieir "blood, their digestion, secretions and muscular action, than b:. see them in herds standing in Avater up to or aboA^e their knees to relieve themselves of their surplus electricity by the conducting power of the AAmter and thus to cool their bodies, whose heat must ascend into the air, and could not be con- ducied to the earth Avhili^ their electricity could, by the AA^ater in Avlnch they stood, be rapidly conducted from their bodies to the earth. Such is likcAvisc the cause of the habit of AvalloAving in muddy Avater of all the pachydermata, tfora the mammotu through the elephant, rhinoceros, down to the common pig. All fatty or oleaginous substances being anti-frictional, as is illusi rated in every day life in the .axles of our vehicles and in machinery having*^ any rotating associations, prevent the ca’-oIu- .tion of electricity, aiid consecpiently of he, at. Hence soino extraordinaxy faks -appear in the animal economy.' It is known that the Avhale, one of the A^arieties of the cetacea, nurses its young from its teats, AAdiieh arc external on its body. It is therefore classed, by naturalists, Avith the mammalia, to which the human species belongs. The Avhalc inspires atmos- pheric air, Avhen floating on the surface of the Avatcr, and also abstracts it from the Avater itself AAdien swimming beneath its surface. The Avhalcs are Avarm blooded, and the conjunction of the negative electricity of the atmospheric air they have .inspired, with the positive electricity of their blood, produces heat. This heat and the accompanying electricity, Avhich is 125 d.'ri‘/ed from tlie friction of their blood in circulation, and of tiu;ir muscles in exercise while in motion, would all he rapidly V inducted from their bodies by the water of a loAver tempera- L-'i’e, ill which it moves and lives, but for the great thickness of the blubber or fit Avhich encompasses them respectively, and the immense quantity of oil contained in their skulls, that arc- non-conductors of electricity, and serve to insulate it as it is ovoh^ed. How then, in the rapid passage of a whale t: rough the Avater,-is the enormous quantity of electricity evolved by the friction of its organs, muscles and blocl, in t’'.eir respective motions, to be got I’id of since it cannot • cape frma its body on account of the non-conducting power of die robe of blubber which encloses it ? The whale, in breathhig, takes in a large quantity of Avater containing atmosphee'e air, Avhieh air, having one electricitj^, is received into its respira- tory system, where it meets AAuth the blood oppositely electri- fied. This blood it oxygenates, and by the positive electricity of its lungs and heart, this blood, similarly electrified, is drh'cn Jhrough the arteries, to carry to every, organ of its body its renoAmting and vitalizing material. Changing the character of its electi’icity by induction as it -.passes into the veins, through the capillaries, it is taken back to the heart and thence to the lungs by the attraction of the positive electricity of those organs, to maintain the life of the animal, and this process is continued during its existence, How the air Avhich the AAdiale has inspmed, AA^hether from the atmosphere iiicctly, <o luiving anointed Ms person before starting vritb the oil of p^i’poises, wliicli enabled Mm to retain bis electricity and beat in bis body, and thus to accomplish bis feat. ISTow, in cases of shipwreck, it is obvious that when people are thrown into the water, no mere floating apparatus, called “Life Pre- servers” arc of any value to prevent the escape of the elec- tricity and beat of the floating person ; but that be is liable to bo drowned in a very few minutes by the escape of those elements, of life from his bodjy notwithstanding he may con- tinue to float for hours afterwards. The’ Esquimaux and other Arctic tribes of people delight to eat oils, blubber, and other flitty substances, having, been taught by their instinct that this fatty diet serves to retain within them the heat of their bodies-==^but how? All fatty substances are aiiti-fric- tional, and non-productive of electricity. The viscera and tissues of these flit eating people become invested wdth fat, retarding- the evolution of electricity in their system, and by thus diminishing their interior heat, preventing the secretion of excessive perspiration, by winch their electricity would be carried'dff frorh their bodies, and the consequent reduction of. their temperature. The people along the shores of the Mediterranean sea, in the south of France, Spain and Portugal, delight also in oily foods, as a preventive of the excessive secretion of perspiration, without however understanding the rationale of their diet. The first Jfapoleon, in a ■ conversation with Corvisart, his chief physician, said, that “ he had no faith in the art of medi- cine; but that he placed a high value on surgery. Anatomy had developed a knowledge of the human organization, and post mortem dissections had displayed the effects of disease, or of injuries to various parts of the human sj^stem, by which the surgeon could .profit, but that no such valuable ^^aid was offered to the physician, who had to grope his way as best he could, in his attempts to discover the cause and the seat of the disease, and then to adopt an experimental treatment ti.> remove it.” “P>ut,'’ said Corvisart, “ Does your Majesty never take medi- cine?” “Ko,” said ITapoleon; “When T am disordered, I abstain from food, mount my horse, and ride rapidly sixty miles — on my return I bathe, sleep soundly, and the next day I am well.” The rationale of this treatment is as follows, viz : The OvCtivo exercise on horseback produced friction in many of his muscles, which friction evolved positive electricity : thi.s required renewed inspiration of atmospheric air, negatively ' 128 % olectrified, to restore the electrical equilibrium ; the union of tliesc electricities developed heat and magnetism, Avliich con- ducted to the stomach' and intestines served to digest the food previously talcen, and which, having remained undigestO'i, had occasionJd his disorder. If any excess of electricity remained i,: his svstem after his return to the palace, the warm bath conducted it from him, and soothed him to sleep. Solomon, the wisest of men, has left, as one of his legacies to -mankind, the maxim, “spare the rod and spoil the child.” Now let us examine this. Wheu_ children were misbehayod, were destructive in their inclinations and conduct, rebellious to authority, and were otherwise troublesome to parents or others having the charge of them, Solomon, being a keen observer, of effects, recommended personal chastisement with tl’iC rod, and naturally attributed their better deportment after the punishment, to the fear of the child of its repetition, and perhaps with greater severity. This was possibly a natural r onclusion on his part, at the age in which he lived, and may be so considered even at the present time, but there is another explanation, more philosophical and more scientific. It is as follows, viz : 'Whou people are in good health, they are usually y cheerful, in good humqur with themselves, and amiable to ;| those around them; they do not think of or attempt to per-' | T.etrate mischief to others, their electricities are in equilibrium, | and they deport themselves properly. Now let one or other ' f of their electricities be in excess, irnmediately their disposi- | ■^ions bectime changed; no longer amiable, they see every thing | and person through a disturbed medium; they become sullen, | cross, crabbed, quarrelsome and disagreeable; the least dis- ,| appointment ruffles them, and they proceed- to behave ill. ■ | Now wiih children, when the rod is applied vigorously to their | rw'.rsons the friction produced by the blows evolves electricity r gatlicr iuto^ shoals till they are al)Out to portorm the gTan'*.st action ot their nature, and that till then each animal hves a separate and iridividual life; but this does not suggest the attraction wliich, brings them into this association. I will venture upon an explanation. Their instinct teaches them that tlioir eggs, wdmn ready to he discharged from their bodies, must be deposited in warmer water thuTdtliat in which they habitually swim. Having but one electricity, fh^ netrativc; which is the same as that iu wdiich they live, no vivi- ficriuoa' of fheir eggs could take place if duly cornininglcd with the milt of the male fish in mid ocean, but attracted by the warmer waKu' of' rivers, at their sources, or iu lochs or haws sliclterod from the waves of the sea, where iu their shallows.vegctablo food is always growing at liotto.m for the support of the young fry,' when they shail be hatched, they hasten in immense shoals for mutual protection from, their cne.mics, to these lyin-gdn places, where the eggs or roc of the female, and the rnilt of the male are contiguously deposited on the rocks ov in the gi-avcl at the bottom. The positive electricity of the warm water derived from the fric- •tioiud action of suidight upcm the rocks an:.l sand on the . bottom of the shallow waters iu -which the eggs of the fish have been deposited, as w'oll as upon the eggs themselves . coniiug in contact with the negatively cloetrjlad eggs and miit evolves heat, and Avith it magnetism, and iu dne time the young fry m'c fully .developed, vhfified liy those elements of life, breaking thc outcr membrane or shell of the eggs con- taining them, already distended and thinned l>y -the growth of the erabr}-© within, emerging into full life into the elemeut where they are to have their being. Of course, the hatching of the eggs of fish is not unifonm as to time in ditferent species, some requiring a longer period than others to attain the maturity of their development. Here we have a rcmarka,blc illmstratiou of the production of 131 I,', ? [ !■ life by electricity and magnetism, outside of the bodies of the parent fisli ; while perliaps in almost every other class of animal life it is developed within, the body of the female, after ipipreg- nation by the male animal, showing most conclusively that these imponderables are ahvays present as' well at the commence- ment of life as daring its continuance, while it has Ijccn demonstrated time and again, that whatever decreases the vis vUce ,o£ an animal diminishes also the evidence of the eiec- tincity within it, until after death it ceases altogether. Are we not riglit, therefore,' in concluding that electricity, magnetism, and heat arc, in.ccrtaj.n relations to each other, elements of every life ? ‘ Oxygen gas'is a supporter, of combustion, as it also is of life, which in fact is one. form of combustion. It. is negatively electrified, and it is hecause it is so electrified that it supports both life and combustion. Let us illustrate this.- The atmos- phere, composed of nitrogen and -oxygon gases for -the most part, with a slight admixture Of other gases and watery vapour, which last contaius a largo portion of oxygen gas, is nega- tively electrified. Wood, coal, and vegetable substances, iii a dry state, are positively electrified. Kow when wo have on our hearths wood as fuel, aud from the condition of the wood 'as Aveil as that ot the atmosphere the combustion of the wood is slow and sluggish, wo apply a pair of bellows to hasten it the common explanation of tliis use of .the bellows is, that it brings more oxygen gas into contact with the slightly kindled wood. than tie atmosphere naturally furnishes, aud hence the combustion is quickened. This is' true, hut it also brings associated with the oxygen gas its negative .electricity, which coining into union with the positive electricity of the fire aud the wood already slightly heated, produces increased heat, W'hich the additional oxygen gas thus supplied nourishes into flame, and the fire is properly kindled. Potassium thrown into a vessel of oxygen gas, hursts into the most brilliant flame from the same cause, the potassium being positiv'oly electrified in a high degree and so it is, hut in a lesser uegroo, with the other metalloids. In regard to the non-produciug and non-conducting powers of electricity by fatty or oleaginous substances, a very ren7.ark- ahlo fact. has been developed in relation to the' human family. It has for a long time been observed that in countries where the sugar caue has been cultivated, aud where sugar has h.'cu 132 Titminfiictured from its expressed juice, the negroes cmploved ill ]l^^llvillg it groAr enormously fat from the unrestricted rise of tlie w:anu juice of the expressed cane during the process of hoiling. From this food, like the whale, they become sur- rounded by an envelop of fat, as do also the .interior organs of iheir bodies. This fat is anti-frictional and pr.events the ev'/oition of electricity, which in the absence of the fat vrould be developed. Hence these labourers could no longer be pro- crea':'';e, and as their labour was A'cry exhausting, the neces- sity for a new gang of labourers every four or five years be- came established on sugar plantations. This fact, in sugar producii;g countries, has kept alive and continued th.e negro slave trade to this day — and where it has been abolished and the cciolie trade substittited for it, the same results obtain. dSTo ux;.men are sent to the plantations with the coolies, for they become like negroes, virtually emasculated by . the absence of their electricity. So that Ave may attribute to the loss of electricity in the producers of sugar the great obstacle to the abolition of slaA'cry for so long a time in the British West indies, and at the present moment in the Spanish Islands, in Brazil, and elscAvhefe as it exists. The same deteriorating iiiTucnces upon their organization- -from fatness, in other portions of the human race, appear in' various parts of the world, preventing the development of their electricity and magnetism, by which their animal fuiictions are impaired, and their intellectual faculties greatly weakened. The Esquimaux, Fins, Laps, and all inhabitants of high northern climates, I'equiring a fatty and carbonaceous food, are examples of this character. The inference to be draAA'n from this remarkable fact is that such persons as arc opposed to an increase of population, and who resist the in- junction to the Patriarchs of “going forth, multiplying and replenishing the earth,” should select for their companions in life the fattest persons of the opposite sex that they can find, and they will be rcAA'arded by an immense reduction in their household and educational expenses when compared Avith those of their neighbours 'AA'ho chance to be of a lean kind. In connection with this subject of continuing a species of animal, I may mention that in Europe, as Avell as in this country, a A'ery mistaken notion exists as to the best as^e at which cattle should be propagated. The prevailing idea is that heifers should not be allowed to bear their off- spring before they are- four years old, and in the state of Penn-' 133 svlvania they are not taxable before they have attained that age. Ihov', this is a fallacy, asJ have al>undantly tested dur- ing thc last twenty years. I have thought that nature wtis the best guide in such cases, and accordin^dy, as iny animals are always well eared for, my heifers are sufficiently developed ■and matured when nine months old to receive the mas -uline im]U’Cgnation, and to undergo, afterwards, a 'healthy gestation, and to produce their young when about eighteen months old. system of breeding, there is a saving in the expense of supporting young heifers during two years and a half o^-er th e conimou method. My'hertl of cows thus produced will com- pare favorably in size, produce of milk, cream and butter, and hcalthfulncss with any herd of similar numbers of cows in tiiis country. I (do not remember to have had a sick cow or h-eildr during the last twenty years. But I have exceeded even this early_ propagation of their species. Last year a tmung heifer of mine, only four months old, manifesting a desire for copu- lation, w'as permitted to receive the male impregnation. Khe duly eoireoived, and before she was fourteen unonths old she bore a healthy male calf. The heifer herself, appareiitlv, was not incommoded by the event, and continued to enjov'cxcc -- lent health; aud.some six weeks after the birth of her l-.dtsl.j again received the male impfeguation. This heifer was r-jaro I . uu(ler the stimulating influence of the associated hlin^ ami ' plain glass, wdiich had hastened its development three years and a half. liTow, apply this discovery to the rearing of d o- mestic . animals throughout the world, and begin to eshmaic the benefit to mankind to he derivecl from the reduced ex- penses in producing them and the great gain that will reside in hicreasing the number of animals to h*e raised in any given- period of time, and some faint idea may be formed of the gre-at value of this discovery in this single branch ' of human in- dustry. A wide-spread error in agricixlture exists in Europe, as well as ill this country, and has'' even hoen vi^diitaiued in hooks of science. It is “ that underneath large trees vegetation droopts and languishes, oven ivhen the shade is not v'ery iuteiisc.” Some years ago I had occasion to p)lough up the sod which covered a small orchard of apple and chestnut trees ou my farm. All the trees Avere old and large. I caused the field to he AA-ell manured, even to the bottom of the trunks of all the trees. 'When the ground Avas well broken up, I directed my farmer to mark out di-ills for sugar beets, and to plant the seed 134 cio;-:':' up to the trunks of all tlic trees. He looked at me with astonVshment, and said : “ Why, sir, plant so close to the trees ? ever grows under tlVe shade of trees!’’ I replied ' that I iiad heard such a statement hoforc, hut that I did not tbirdc it' to he well founded. I had seen too many weeds, sucioTS and hramhlcs growing luxuriantly uiuler trees all over the ( . .nntry to attach any credence to it. “ Do as^ I tell you phiei: ihe seed close to the trees, and leave the result to take' can : ‘ • t itself.” My farmer v/as so much astounded hy what he comidered my foolish directions, that he went over to' some fanie-'rs who were planting tlicir seed in neighhouring Holds, and rdd thonr of the ahsnrd directions I' had given him. In the fulness of their nciglihonrly kindness, they came over to me +0 oulighten me. on the subject of farming. “Your man tcHs us s;nd one oftlicm to me, “that you have told him -to plant su’wrr beet seed close to the trunks of your big clmstnut trees. Wo have come over fo tell you^ -what ;)X)U may not knopp that no p'anfvvill grow under the .shade of trees, and to dissuade yodi t'r-om attempting to make them grow there. ^Vo have . hcon [arming 2,5 yca 3 .’s, and our fathers bcforc.us all their lives, anu v-c have never heard of such a thing as_ planting for a crop under the shade of trees. Pray don’t trypt.” I thanked tholu for their solicitude, hut told them that “ it\vas an c.aperi- mcai : if it should fail, the loss of a few seed and a little labour were ^.11 that would ho involved in it; and if it should succeed, it ^ ••■■dd explode and banish a very mischievous ami expcmsivu falhu-v in agriculture;, little hurm was to he appreheuded from it.” 'The tanner tiiidiug mo kctcrniiiied, said, “You gcutlo- m'on from the city, come into the country, buy land,^ p'cet exiiiu sive huildiugs, purchase high priced stock of all kinds, and '' “. cry new tangled tool or labour saving machine that is advertised, hire people and go to Avork, and think yoiv are fame rs; hut I have never known one of you to make CA'cn his expenses out of his farming. You had all much hotter do as^A'cmr ncighl)ours do than strike out into new paths.” I said him^ “your robuke is just, and what you say is no doub.t true; I acknowledge it to he true in my ease. I knoAV Tcrv iittle of anything, hut I could not think for a mpmeut of takin ^'- up the time of my farming neighbours by asking them how Ui manage my farm; I must learn it as host I canAvitliout taxing their nciglihonrly kindness, and this experiment of mine^is one of my early lessons in farming.” Piuallj, these 0 -ood people took their leave, and my beet seed AA-ere planted Iccm’dmo- to my directions. In due time they germinated, and 1?ogan to grow, and to the surprise of my farmer tlvo plants as tlv'y grew became stronger and larger at. the l.»ottom of the tr ui ilc-'’ of the largest frees than the other plant.s were in the o[)ei\ spaces in other parts of the field. This ditference continued to increase as the season advanced, and when the time, had arrived for gathering them, the greatest contrast, was pciceptible between those that had grown under the shade of the trees, even of the largest, and those which had grown in the open sunlight. At thi.' tinm the same Idnd neighbours who had visited me, in the previous spring to advise me against planting my secd. undcr the shade of the trees, Avere gathering their an tumn crop>s in the adjacent fields. T went over to them and a^ked them if tiio.y would like to sec my beet crop, and on tlfclr ex- pressing a desire to-see it, Ipnvitcd them to accompany me, and Wo proei o.dcd to the field. Gn otu* way I asked them whcr<; thoY thought the best hccts avouM he found. . “ In the open snn.l>gb.t to he sore,’’ was .the ansAA^er; “nothing ever groAvs nttder the shade of trees I” I madeyto reply, and soon after avo entered the field. As avo passed along I Avas amused at the astonishment depicted on their countenances,. as .they exaii.d.u'-d. the beets in different- parts, of the £cld. Presently ofie oi tuexa^ nu!7 ex- pect mo Avho have no experience in farming, being fr nn the city, to do it ? I knoAv nothing about it, hut I Avill toll you what I think. ' I AAdll illustrate my meaning by an ex:.rn,plo : suppose you should take t.AVO men, both healthy, strong and vigorous, and both very hungry — one of them is six feet tall and very broad and muscular — the other man is five foot six inches 'high, and also muscular. Suppose you place them at a ) .136 table ami -j iut before tlieni food sufficient only fox* ono X ixat: of {ivcvsge si/'.c and sti*engtb, and tell tbcm to cat, Isow x'lincb of the food ; do you'thinkthe little 'man rronhl got?” “ Y.'ell, I ' gues.s not a great deal of it,’’ said one of the nxen ; to ^^■l;icil the others fisKoited. “Xow, suppose youhadput outlie i able xaiough food tor br)th, would they not fisc from the table refreshed and rein vigoratod, and ready for their woi’k ?” I said to them. “ Well, ye.s, I should think so;” Avas their answer. ‘‘hTow,” said I to them ; “the first supposition illustrates your mode of farviting. Yon -manure your land lightl} , furidjdiim': food enough only for your ci’op, and nothing for your hnnbn them, than other plants iu.the sunlight AA’hich haA’e no such -xjrotcctio)! — and you know that m6islui;e is necessary to the grcAAdh of plants,” They thanked me for my ex'planation and went tlioir vviy con-' fouxided. Since then I liaA^e cultivated under AU-ry large trees on nxy hiwn, plants and flowers of many discrijAtions Avith great succc.sa, and the cultivation has greatly benefited the trees thcxnsc lves. I would recoxnmend to all having trees on their lawixs to eultiv’ate the soil at their bases iiV floAvei’ing x^lants, if they desire ornaments, or in vegetables if they need them for food. To holders of small patches of land, this information may ju’bve to he of great comfort and convenience. This little narrative brings me to the mxhject of the forma- V. 137 tion of dew, wdiich I do not attribute to condensation of the atmosphe:’e bolding it in suspension, but to tb.e ; opposite cau.,c, viz; the expansion and rarefaction -f flic atmosphere by heat, its ascent upwards andpts abandomnen' of the water ivliich it had previously held iii suspension. When, in ihe rotationmf the earth upon its axis, any e'ivcr area of its surface is -no longer illuminated by the su n s ra -,,-,, ■; or, as iji common language, it is said; -“It is sunset;'’ the ■’avs of sunlight do not illumine the atmosphere that is over such an area of the earth’s surface, and, as' the night advances, thof atmosphere becomes colder and more magnetic with hr- increase of cold by induction. Columns or. volumes or th:e cold air are th.cn attracted to the earth by its 6-y ;ofth.i .magnet!; ng and descend towards it. At the same tinle the in couto'd \_dth tpid just above the eaith’s surface, liovinn l;?er; heated during the clay by the electricity evolved by surhli-hr. and being, positively electrified, ascends to meet the eohr aii-’ descending from above, negatively electrified and epposltcdv' magnetic; the conjunction of these opposite elevh-ioifo- ■ produces^- addif tonal heat which so warms the air ftchghtoh with mqlstUro that is. descending from above, that its enfian- sion ana rarefaction wll no longer admit of its hoiditii’ ;,■> suspension too watery vapour that it was bringivu’ down wig; • it; it conserniently ascends alone, leaving the globules of v;afer which it contained to be carried to the earth by their nv.ignec- i-sm, anu to insensibly settle upon the grass, leaves, eax il;. &c., and torn': what wo call dew, hoar frost, &c-, according to t'U' temperature of the earth’s surface at the time of sucirdcposi- ' tion. This occurs iu a cloudless sky. • Wlien ihe clouds are floating above us, there is no dew, not because, as we have been tan^t, that the radiated heat fro.-^ the earth is reflected by the lower surface of the clouds to the eai’th, thnsbkeoping the air in contact with the earth too war :n to deposit its water as dew, as that is an absurdity, since hear reaching- the lower part of any gaseous or vapomy fluid, woua.l at once peiictrate and permeate such gases, vapours or clouds and expand, rarefy and disperse them ; hut because the inter- posing clouds would prevent the descent of the volumes of cold . air freighted with moisture above them to the earth below, and consequently there could he no deposition of water or dew from them. Cold does not condense the atmosphere, for if it did the density of the air would be much gre:aer in winter than in summer, which we know is not the case. Be- 138 sides, ti\o rarity and tenuity of tlie air at great elevations, vrlicro evtreme'cold prevails perennially, contradicts this as- ' ’ sumption. Nor has the air any weight— gravitatioms sui> . pofi'd to act only in one direction, viz : towards the centre ot the earth while it is known that the air presses erpmlly m all directions, upwards from, below, laterally and downward from above, hcaee it cannot he’ acted npoii hy grayitahon.^ xhe . harometric pressure of the atmosphere iii its variations, is clue in all m-ohahility to magnetic attraction and repulsion between the atmosphere and the earth. The same reasoning appUes to the waters of the oceans. They are fluids xn'essing Jihe thearr hi all directions, npivards from below, laterally and down- wards and rest upon the earth hy the attraction of tuo earth s ma-^-nctism, and not hy gravitation, since their ..upward and latclral pressures are antagonistic to the attraction, of gravi- tation. Every drop of water is a magnet. When the globules n>'o vertical their poles are at tho-toci of their forms, the lovmr polo attracted hy the • magnetism of the air above and its upper pole attracted towards the maguetisui of the earth below. These dowmvarcl and upward attractions corresponding repulsions dislocate, from their great .mobility, other ^dohnles of the water, and force their polar magnetic or ressures lljnough- ■, iih each . These ;o water, the con- av^s hriio horizontal 'or dia-magnetic, ancl.tlpe e-ervvd - ere varying in tension, develop magnetic.for/;e.-: out ihc mass of water, acting at every possible angl e ^ other and producing everywhere opposite rcsistaim.^ rriao-notic cluumes induce electrical disturbances . ,ui t residing' in the development nf heat hy fnetion a-nd innetion of opposite electricities, causing ni all latirudos those iurrmits of evaporation associated with electricity, which we find af' dbmcratcd in the atmosphere as masses ot clouds, fogs, mists These masses of clouds acquiring their electricities bv induction, become oppositely electrified accordmg to tlieir elevation in the atmosphere above the earth, and as they armi'oaeh each other in their movements, an electric discharp takes place, a decomposition of the watery vapour oeenrs, the Imlro-cn ^s is burnt in the oxygen gas ot the decomposed i?abw°di«pWing that bright yellow light peculiar to hydrogen, in flashes so dazzling that if they were not so eyaneseGnt no w forces of the atmosphere, descend to the earth as s -' I'ncal drops to meet and mingle with the magnetism of t'e* ■: u’tli. These drops of water are what we call rain. . If it were not for the upward pressure oftlio v^-atcr- c the 'ocean from their lowest depth, how long would the ci ;; h of earth beneath them, (computed by physicists to be rcho :-. ir to tlic mass of the earth no thicker than aji egg sir 'll iss as lien compared to the mass of albumen that it contains,) he a ble to sustain the pressure dowiiAA’ards of a mass of water fi'oui five to ten miles in depth as it moves in its tides, its currm-rs, and. the rotation of the earth upon its axis, and as it rolls, in it:: rbit ? AVould not the momentum of such a ma.ss.of Avators b ^ , put in motion, in the course of time tliat has elai> -cd sii; ' they Avero gathered in seas and oceans, Avear aAvay so m uc : c * the earth’s crust as to allow” the Avatets to flood the iutc ri •: Arcs of the earth, aod produce explosions that would slii -o t the planet into thou.sands of fragments? Ami does m tliiB lurnish^another argument against the d.oetrir-o of grav'; . . .ion? Tlie same principle apjilies relatiA'e to the upvT.rd pr >; i.re of the atmosphere. In the cases of the waters of tbc v ^ and the atmosphere — both being fluids, difiering ho w . V‘ r • Tielr tenuity, their molecules havei great mobilityam oug ;-.h..':..;o...]ves rcspcctiAxdy, and. from the irregular and unequal lip'; ... .1 and doAs'uward magnetic attractions and repulsions, tbe.'e mole- cules are displaced and turned aside, changing Iho uiv. ctions ot their poles and their axes, and thus becoming din-m ignetia or horizontalh'' magnetic, creating thns: the lateral prV -sures exi.sting both in the Avater.and the atmosphere. d\’'lieu, from the mobility of the molecules in the crust of tlio earth at the period of- the planet beiiig lauiiobo'l into space in its rotary motion on its axes, ai;d its pvogr.-sjivc motion in its orbit, the ecpiatorial diameter Avas, by m 'uuetic attraction and repulsion, increased tAventy-six miles nr tro rhan the polar diameter, the same influences repel) c^d tfom the polos respectively and attracted to the respective opjiosite poles the waters in the arctic and antarctic basins till they met in the tropics. . . The upward pressure of these waters, their polar currents of, cold Avater at great depths, and the rotation of tlte earth . on its axis from west to. east, haA’e united in forcing the masses of oceanic waters to the AvestAvard till they impinged upomthe eastern coasts of America and of Asia— aet’ou and 140 re-action lioing equal; those waters, after their impact' with these cuijstf! uixd. tlieir coutiguous ialands, were reflected hack again ::.>v:!ird 3 the western coasts of Europe and Africa, and mooting uiidway .in oceans, the- succeeding waves of those waters have risen above the general level of the oceans a few feet, which has been called a tide, and which has been attributed erroneously to the attraction of the sun and moon instead of to the forces which I have mentioned above. The impact of these waters in mid-ocean throws back to the Europoau and African waters, coming from thence and to eastern h.tucx’ican and Asixxtic coasts, the waters attracted there by die' rotary motion of the earth on its axis — and thus they f(vrc(>back in all these continents the waters of the rivers emptying iiicmsolves into the oceans, creating in them the tides,' the causes ofl which never before have been satisfactorily explained. These tides, therefore, are the results of the magnetic attraction and repulsion of the waters and the coasts of 'the continents where they are seen and felt — and are not affected at all, either by sun or moon. ' The *cxi.iTent8 of the , Mediterranean sea — ^the upper one inwards is the result of the pressure of the Atlantic ocean in its roiiux from the mid ocean impact of the oceanic waters, the lower current running into the Atlantic ocean— is pi’o- duced by the upward pressure of the Mediterx’anexxn waters and tli'.- niagnetio attraction of the colder polar current at great depth tow ards the equatoi’. The heat of the earth ascends perpendicularly to the hori- zon.' It cannot, therefore, be deflected to any considerable extent in producing winds or cui’rents of air. These result from electrical ^and magnetic attractions and repulsions — the upward pressure of the air, which is nothing more than the magnetic repulsion of it from the earth — having their similar poles of magnetism adjacent, until .by induction the polai-ity of the air is changed in the higher atmosphere, where, heiiig intensely, cold, it is attenuated by the repellent qualities of its Eomqgeueous magnetism, and not by the low degree of its temperatufo,- which happens to be coincident wuth its mag- netism, but is incapable of condensing the molecules of the atmosphere. '"SYlieix we remember the law of attraction and repulsion of 141 ms'gnefism, viz: that it acts irsversely as the sq.vii’c of the ch.si-anec, and that the earth, its oceans and- its' atmcsph ove. are all magnetic, and mutually attract and rep-1 each otiier accord- mg to this_ law— which, by the way, is the-.sanie -aw that ^ Is ewtou assigned to the gravity of matter— and Avh ai we fur- ther remember that they are all in contiguity with ea';I v'xer v/e cannot fail to conceive that thi^ planet hr.=< .,1 the forces within and around it that are necessary fcu' ti,e per- formance of all its functions without attributing tliem to the actions of such distant orbs as the sun and the moon. If the moon, as our astronomers assert, exerts a greater isifluence upon the tides than. does the sun, owing to the giaruor dis- tance of the sun from the earth, by a parity of reason in cq how much more influential must the earth itself he w‘nh is in contact both with its waters and its atmosphere. Aii fluids Tvben acted upon by unequal forces assume a spiral c-.nrse, a 3 witness the whirlwind in the atmosphere, aiid the vllrlnool and eddying currents in the waters. The currents of the oceans are spiral curves modified in their curvatures by the fixed as- well as movable obstacles they encounter in their several courses. When a wave at sea has reached its crest, why does it curl over and break into spray, as it descends into the :>-f>ugh of the sea? If the moon lifts it up why does not the ’nocirfhold if up ? Wlieu a wave breaks on the shore, why does It cling to the 'eai’th, and recede in contact with it as thoundertow,fre- quently carrying with it to destruction the- incautious or un- skilful swimmer ? Why does not the moon keep tlds water cn the surface instead of suffering it, though it he warmer tlian the water at greater depths, to seek its company against an assunied law of physics, that the warmer fluia floats upon the colder ? Wliy, in the whirlpool, does the warm surface water rush down its spiral coils to meet and mingle with the colder water of the greater depths ? And why does this cold water ascend ill counter spirals to meet the descending warmer water? This action is not caused by gravitation ; it is magnetic, and so it is also in the whirlwind. The warm air of the lower atmosphere, in contact with the earth, is taken up in its spiral coils, attracted by the opposite magnetism of the upiier air, which descends in opposite spiral coils to meet it in its* ascent, and together the column of whirling air, repelled from its 142 Gom’cc and carried over the surface of the earth, but in con- tact V, itli it, vii h a resistless impetuosity, by the electrical curi\ 111 v/liich lias developed the magnetism of the column, devasmres and -^c^>t^ln7S every obstacle that lies in its course, till the magnetic equilibrium is again attained, -wheu a calm ensues. In tlicse hsstances of the whirlpool and tlie whirl- wind, the assumed law of gravitation is violated by the ascent of tVic. Avarm air into the colder upper atmosphere, as well as hy tl e descent of the warm surface water to the deptlis holow; thus proving that the motions of fluids, whether gaseous or liquiO; are controlled hy magnetism. A balloon charged with hydrogen gas, and released from its fasten.: /ig to tlie earth, ascends rapidly into the upper atmo- sphci c — the region of intense cold, wdicre, as we arc taught in the scnools, it should he condensed, and the sides of the halh‘ >1: should ho^ioose and pressed inward by the condensing power of tlic cold in that elevated region. x\ccording to the doctrii c of gravitation it has ascended because it was filled with iiVdroL’on gas — the lightest • substance in nature — and evorv light substaucc floats upon any other substance heavier ■ than itself. Inow, let us sec what'actually takes place in the balloon, jPp’S', The hydrogen gas is positively electrified, and is at- tract al to tiio upper atmosphei ’6 hy 'its opposite electricity, which is negative. , (SW-c-.v/i, 'The balloon itself is painted and varnished with giimo to retain the hydrogen gas, which pigments and varnish are ai jo positively electrified smd assist in raising the balloon. Third, The higher the balloon ascends- the greater is the at- traction of the negative electricity of the upper air for it. Presently a conjunction of these opposite electricities of the upper vir .Ind the positively electrified gummed surface of the halhroo ocimrs, heat and magnetism are evolved, the canvas of tl: balloon begins to expand, and within it the hydrogen gas also expands to fill and to tighten the canvas. The at- traction from without and the expansion of the hydrogen gas within distend the canvas to its fullest extent. Should the ^eroiiiiat not. at once opcji the safety valve of the balloon, and 'liberate a portion of the hydrogen gas within it, these forces would burst the canvas and precipitate the unlucky aeronaut 143 -to tlio o n-th, a catastroplic whicli reallj happened in J£ri.e;., only a few days since. TIio ascent, of the halloon, the expansion of its canvas an i oftlie hydrogen gas within it instead of their condensation bv •the extreriie cold of the upper atmoopherc, the bursting of d*e halloujx — ail contradict the 2s'cwtoniau theory., "We will now explain why the temperature on the surih 's of tlie earth is greater during sununer, though the sun ns then -at its greatest distance from the earth, than it is in winter, v.hen the distance between the earth and the sun is at the least, being three millions of miles lees than it was at the sumnier scdstice — viz: June 21st. On this day the ravs ot sunlight, vertical at the tropic ot Cancer, impinging'through- the ann ' -phere upon the surface of the earth, with a velocity of 18hyt ) luilcs per second, produce groat friction. This friction is the result of the impact of all the rays of sunlight upon tiiC earth’s surface. This friction evolves ,mor'o elec- tricity in the contact than it docs in winter, when the ang!-j of iiic; .leuce of the rays of light is very much m-uc acute, and a 'hoi-ge portion of the rays of light arc at >hat tirne reliecicd and refracted into planetary space, witliout •deveiop- ing tho electricity either in quantity or tension, winch- tho whole quantity of rays of light would do if they reached tlie earth directly. Consequently as the electricity evolved is less in wintor, tlie heat which +his electricity produces in coujnnc- ' tioii witi-; the opposite electricity of the earth’s surface is much loss, and the temperature is therefore lower iu ’.yiuter than- in summer. - , Besides, the vertical impact of matter upon matter, as of ligur ' upon t: ic -dmosphere, or upon the surface of the earth, is always more vit .[eiit, and produces more friction than its impact from a?? acute angle, or as it is called a “ glancing blow,’’ would do, hence more electricity results from the friction produced l>y the vertical impact of light, than there -would be frou- its ini~ pact ox tin acute angle. The.declinacior. of the sun, th ' o- fore, by coii.^tautly changing the angles of incidence of iis ligiit, as. It entt^rs our atmosphere, and impinges upon the eartli’.- s; "- face, iS the cause of the changes of the terrestrial temperature at the several seasons of the year. Hence the more vertical the light, the more friction is developed in its impact with-cho earth, and the more electricity thus evolved, and the more - heat produced by the conjunction of the opposite electricities from the light and earth. 144 •\t the height of five miles or more above the earth, when of clouda oppositely electriiied come together, great I'eat is evolved by tlie union of these electiicities, and with it is also developed magnetism ; the air of the cloud thus heated becomes positively electriiied, aud greatly expanded by the l:i;.it, it rushes upwards attracted by the negative electricity of I’iC atmosphere above it, abandoning the watery vapour it had •.•ontained in suqjcnsiou,' and which absorbing tlie magnetism developed by the union of the opposite electricities begins to irill towards the earth, not by gravitation but by the magnetic repulsion of the surromiding air, and the magnetic attraction < f the earth itself and the waters on its surface. At the same time, wben this conjunction of opposite electricities occurs, much of the watery vapour that the clouds hold in susponsiou is decomposed by the superior attraction of the intense elee- tneity for the hydrogen gas of the water, which is immediately burnt in the oxygen gas that had been liberated by the de composition of the watery particles of the clouds in the first place. This inflamed hydrogen burning with a yellow light, rushes to ' embrace again, its lover, oxygen gas, pursuing it iu those brilliantly illuminated zig-zag courses which we call flashes of lightning. Xow as these conjunctions of opposite electricities arc suc- cessive in a storm, we see the frequent flashes of lightning aud hear the rolling of the thunder, (which latter is merely 1b 3 noise of the explosions of oxygen aud hydrogen gases, v'hen acted upon by a current of electricity passing through them,) as they dart or roll through the atmosphere. The v.uucr thus formed, starting in sheets or columns as it may be, is at once disintegrated, by the repulsion of the magnetism winch it has absoi-bed, into atoms or globules, each ofwhich- is a separate magnet. These arc repelled by the mugnetism of the upper atmosphere, and arc attracted by the opposite magnetism of the earth aud its waters, and continue to descend to^vardc the earth, but the molecules of atmospheric air are also magnets, and repel and retard the descent of the rain drops as they fall, and these force's continue to dimmish their . sizes, till, on approaching the earth, they arc so comminuted, that frequently they become absorbed by the atmosphere and appear as mist and fog. . IS'ow,, if rain falls by gravitation, beginning,' at that great height of five dr more miles, to descend in the first second of time IG.l feet, in the next 32.2 feet, in third second C4.4 feet, 14o in the fourth second 00.6 feef, increasing, its velocity as4he time of descent and the space through which it passed as the square of the time, it would be found tliat its velocity and momentum, when it reached the earth, would be so ei-eat as to wash the soil into the seas, deuu<''r.g mountains and dis- integratino^ rocks, and destroying every living object on the planet. We see on a small scale the devastating power of a waterspout that breaks and discharges its contents when traveling only a short distance above .the earth. Besides it is P. to see the retardatory effect of magnetism upon the Hakes of snow as they fall lazily to the earth, each crystal Ot the snow flake, or frozen water, being acknow]cci^>-cd as a magnet endowed with its full proportion of m.^cnetic power. These facts, prove that neither the cTouds, that float in the atmosphere nor the waters thcv contain, which have been taken up by ovaporatiou from the rivers, lakes and seas, and winch .are again returned to them in rain, snow and hail, are aiiected by the so-called laws of gravitation. Conceive for a moment that the volume of w'ater of the it^iagara river which passes over the falls, should, by gi’avitation, descend from a height offwo, three or five miles- above the earth, the eoramoii height of clouds; then imagine the destruction that wmuld follow^ such a descent; and ;)X't vrater from clouds start in their courses- towards the earth in masses so gx-eat as to divindle 111 comparison the mighty stream of Magara at the falls, and yet only benefit results from' the rainfall. Why, then, docs the water from the clouds not continue to fall, as it has started in these enormous masses? It is because the Creator has beneficently provided against' such a calamity by investino- water with magnetism, %vhen its constituents, oxygen and gases, are combined by^hc passage of a current of electricity through them, iu the formation of water,, and the atoms or globules of w-ater, being each magnetic, repel each other, and are repelled from the upper atmorohere — also magnetic -and are attracted to the earth by its opposite ma^^- netism, allowing rain, snow and hail to fall gently and m small particles to the earth, lienee the greater the height of the clouds from which the rain falls, the smaller and "more attenuated wfiU be the rain drops in arriving at the earth. Mists and fogs, therefore, are as frequently the results of raiii falling from very high clouds, as they are from evaporation at the surface of the earth or oceau. Melted lead oa the top of a shot tower is positively electri* #- fled— the air around it negatively electrified. The lead in ■falling repels itself ami is attracted Ijy the opposite electricity of the_^air, causing it to separate and to assume the spherical form of shot on reaching the vessels to receive it at the bottom of the tower. So that we may attribute the spherical or spheroidal forms of rain drops, of meteors, and of the planets themselves, to the forces of magnetism. . Let us take a east iron spherical shot of the calibre of twenty- four pounds, and heat it to a nearly white heat; then let us select the lightest down from the common thistle that we can find ; we will then sliake some handfuls of it over the hot shot at the distance cf three feet above it. It will he found that notwithstanding what is called the attraction of gravitation, not only of the heavy shot but also of the still heavier earth on wdiich it is supported, the down will he carried upwards into the atmosphere fiy the current of heated air radiated from the hot surface of the shot, instead of falling either upon it or ■on the earth immediately adjacent to it. If, therefore, this heated shot repels some of the lighest flocculent matter of which ■we have any knowledge, and will not allow it to fall upon the earth in opposition to 'the radiating power of its heat, what becomes of the gravitati,on of the earth and of the other })lanct?, and of cemetary matter, &c;, to the sun, if this latter is an 'incandescent body of a temperature so high that wo cannot really, conceive of its actual intensity? If the lightest sub’^ ■stance, so-called, cannot be attracted by it through such .excessive radiation of its heat, how can it attract the lieaviest •planets ? "VVhat also becomes of its magnetism in the presence of. such intensity of heat? It is evident that this great heat could not co-exist with the magnetic forces of the sun, ■which ' are thought to control the movements of our solar system. Let us observe a l)oy on an August day, when the ther- ■mometer indicates 98° of Fahrenheit, in a room with closed •doors and window sashes so as to admit no disturbing currents of air, while he amuses liimself with blowing soap bubbles from the bowl of a clay pipe. "When the bubble is formed, and it is sufficiently thin, lie throws it ofl“ from the bowl of •his pipe. The circumference of the bubble interrupted by the bowl of the pipe, as soon as it is- detached therefrom, closes upon itself by magnetic attraction, and forms a nearly perfect sphere, while it ascends rapidly towards the ceiling of the room. Mark the play of iridescent colours on its surface as it receives the light from a window, just as the suu receives the separate 147 rays of light from the stars and. reflects them to the earth, ke. Now why does this bubble ascend in ^;he atmosphere ? The water and the soap of the bubble, as wel.l as the component parts of the soap are eachvheavier than the warm air of the room. _ The gas that fills its interior, composed of vapour and carbonic acid^gas from the lungs of the boy, is also in its com- ponents heavier than the same air, and is also probably of a lower temperature than the air, which is 98° of Fahrenheit, and yet the bubble, in defiance of the so-called laws of gravita- tion, ascends to the ceiling, instead of descending to the floor. If what astronomers tell us is correct, the density of the sun is about one-fourth of that of the earth, and cannot relatively be so great, volume for volume, as that of this soap bubble. Water is the standard measure of density; potash and soda in salts, component parts of this soap bubble, have each a greater density than water, while the oil associated with them'^in the soapy water is perhaps less than that of water, while the density of the soapy water is greater than that of the sun. Now the earth, with all its power of alleged gravitation, could not prevent this soap bubble from asgending'in the air. Xow why Avas this ? The globules ■ of soapy water Avere held together in the bubble by the viscous character of its oily par- ticles, which having an "opposite electric condition to that of ■ the Avater, attracted it to complete the circumference of the bubble when it wvas detached from the bowl of the pipe, while the magnetism of the whole bubble, repelled by that of the eai-th, caused it to ascend into the upper air by the attraction ■of the magnetism existing there. Now conceive of a soap bubble 1,400,000 times greater in its dimensions than the earth, to be placed in one of the foci of the earth’s orbit, and then imagine it to exert its gravitatino’ power upon the earth, and estimate the result. If the earth could not attract by gravitation this soap bubble in the room referred to, what power would the big soap bubble have to attract the earth by its gravitation, when their positions Avould be reversed ? ’ The undulatory theory of light is faulty in this, that every wave requires a resisting medium to lift it above the common level. In water, when any force disturbs its surface, the inertia of the water, against which the surface water is driven, offers a resistance by which the surface water is raised into a wave, but in all such cases the velocity of the force is small ; 148 wlion tho velocity of the wiml, for instance, is one hundred and fifty miles per hour, it carries off the surface water into spray, until sufficient time has elapsed to allow the inertia of the mass of water to resist the impulse of the wind, when waves are formed. Kow if tho ether of interplanetary and interstellar spaces furnished such a medium of resistance it would not admit of the passaj^e of light through it, with its inconceivable velocity of 186,000 miles per sc'crmd. If tho ether itself was luminous, some force of very low velocity must impinge upon it to. make its undulations, and to be undula- tions they must meet with resistance to become such ; besides all undulations occur on the surfaces of fluids, and extend but a short distance below the surfaces ; but ether of space has no dimensions, it is illimitable: no one- can say where is its surface; neither words nor figures can define its depth, width or height, and as all niotions through it are of inconceivably high velocities, it follows that there can be no undulations in it, as they arc produced by low velocities. Sunlight, on a bright July day, falling in its greatest in- tensity upon the calm and placid siirface of an expanse of water, piuictrates it and descends- to very great -depths below it, Avithout producing the ^slightest undulation on its surface, or movement wdthin its masses. .'Its velocity is so great that no ap[ireciablc time is afforded for the disturbance of the inertia ot ibc Avater. So it is A\'itli the ether of interstellar and inter- planetary space. Thin, subtle, and attenuated, as this ether may be supposed to be, the vcl()city of light in passing through it is so transcendently groat that there Is no time for the dis- turbance of its inertia, and consequently its motion is instantly absorbed by the masfe of the ether, without producing any undulation whateA’er, jSToav undulation is a superficial act. There is no Avave at sea of a greater depth below the surface than forty’ feet; all beloAv that depth is unaffected by AA'hat- cver, cause that may have produced the, superficial Avavc. The great Leviathan of tho deep, ninety or one hundred ’feet long and of other corresponding dimensions, plunges beneath the surface of the ocean when struck by a .harpoon, and Avith inconceivable speed rushes into tho depths below, yet he leaves no Avave, no ripple, to indicate the course he has taken, and the whalemen in his pursuit have to scan the horizon in every direction to ascertain the place, sometimes a great distance off, where he has risen to the surface of the ocean to blow off his surplus electricity and carbonic acid gas generated in his lungs. So it is Avith all the fishes and marine animals that 149 i ;v,. inhabit the great deep. Their motions, however slow or swift, p ; develop no undulations beneath the surface, and consequently ■ none appear on the surface; there are, therefore, no undula- I tioiis below a depth of forty feet from the surface. Geographers inform us that three-fourths of the outer crust of the earth are covered by water, only one-fburth bein^ dry |> land. Of this fourth part but a small portion is habitahie by ^ ■ animals, and a still smaller part thereof is actuallv occupied J . by them, while the waters of the earth are teeniing every- ■ where with animal life. Innumerable myriads of fishes, marine , ■ animals, and sea monsters are^ known to’ exist beneath the surface of these waters; their speed in pursuing qr avoiding b each other, as they rush madly through them, should greatly disturb their even surfaces, but whatever agitations may occur F in the depths of the ocean from these causes, no trace of tliem f ever is seen on its surface; there is no undulation from such ^ causes. ^ 'Why? The reason is obvious. Fluids press equally j. in all directions. The inertia of the great mass of waters is 'v not to be disturbed by the passage of even ‘innuraeralde i _ objects of small dimensions at whatever speed they may attain. The same principle obtains in relation to the ether of planetary space. This planet rolling in its orbit with a velocity of sixty- ^ - eight thousand miles per hour, through this ether, does not ; aud eannot disturb the inertia of the whole ether of space ; the r motion of the part displaced by the earth and its atmosphere ^ . is absorbed at once by the whole mass, and its inertia remains [ unaffected;, and so it is with all the planets, and even the sun : itself. The sun’s motion in its orbit being 14,400 miles per hour, the moon advaucing in her orbit at the rate of 65.000 t miles per hour, and so on with the rest of the planets, their y enormous velocities will not- admit of the disturbance of the h inertia of the ether of space before the planet has left the ether b far behind through which it has passed. The retardation of I eometary matter in its course is not due to the resistance of the h 1 through which it 18 passing, for if it was it would be y uniformly and continuously retarded in its whole course, and > ' not merely as it is approaching or leaving the neighborhood of the sun, but it is owing to the magnetism of the sun and s the planets, as well as of the opposite magnetism of the ether ^ acting upon its oivn magnetism, that such variation in its iv velocity has been observed. This r^ minds me, that when a planet is at its nearest point to the sun, it is moving with its ^ greatest rapidity in its orbit ; and when at its remotest point b from the sun, it is proceeding at its slowest rate of speed in its 150 orbit; but yet the orbit throughout its entire course is so bahinced that the rapidity is exactly proportional to the near- ness, and the slowness to the distance in reference to each, so that equal areas of the space included in the orbit are describcii by the planet in equal times, which is Kepler’s celebrated second law. The friction of the atmosphere with the ether in its passage through it evolves negativ'e electricitjq which is taken up by the atmosphere by induction, and thus it becomes negatively electri- fied. If the planets cannot, in their rotation around the sun and on their respective axes, disturb the ether of space in its inertia, how can it be supposed that rays of light passing throuj^h it with its velocity of 186,000 miles per second, can cause it to undulate ? Time is an element in the production of a wave, and in the passage of light through ether there is not tirne enough to resist the passage of light, in order to produce it. A musket ball with the initial velocity of 1500 feet per second, when shot from a musket will perforate a door hanging on its hinges without moving it, as there is not furnished sufficient time'to disturb its inertia before the ball had passed through the door. So in like manner a tallow candle discharged from a musket will pass through a door without disturbing its position, while if it should be thrown from the hand against the door at the distance of ten feet from it, its momentum at such low velocity wmuld push the door back to its frame. Kavs of sunlight, in passing through the ether of space, cany with thenrtbe negative electricity with which they wore repelled from the sun’s photosphere, and continue to be repelled by the negative electricity of the intensely cold ether itself through which they are passing, _ Now interpose a glass prism to the passage of a beam of this sunlight after it '"has reached us on the surfoce of the earth. This white beam of light is then refracted and decomposed, and each colour ' leaves the prism, diverging not only from the original ray of white light of wffiich they are the elements, but also from each other, as may be seen by observing the spectrum which they fonn. This spectrum exhibits these colours in the order of their susceptibility of refraction, the red being refracted least and the violet most. From its appearance. Sir Isaac Newton, wdio first analyzed it, thought that there w^ere actually seven primary or distinct colours in the composition of lia;ht, but since his day investigation and analysis have determined that there are but three primary colours, viz : 151 red, yellow and blue, and that Ibe orange, green, incligo and violet, result from a commingling of the primary colours in. ditferent degrees of intensity, as they form the spectrum. Iv ow, let us see what causes this refraction and decompofition of light by the prism. The glass prism was positively electri- fied when the sunbeam was thrown upon it; the opposite electricities of the ligh.t and the glass were brought into contact; heat and magnetism "were evolved by their union: the glass was expanded by the heat, which was immediately absorbed by the air ; the rays of light, changing their electri- cities by induction, become p:>ositively electrified and magnetic and repel each other, forming Newton’s seven primary rays, according to the diflerent degrees of positive electrizatior. and magnetization they have absorbed. This explanation will also account for the invisible beat rays outside of the spectrum, which hf some philosophers have been erroneously supposed to have come directly from the sun, associated with its light. Again, let us take two pieces of flannel made of wool, yf the same texture and' size; let one of them be white flanue], the other black flannel. Now white flannel has the same electri- cal condition as white sunlight, tliat is, negative. It conse- quently reflects or repels the sunlight, according to electrical laws. For this effect it is extensively used by the people of hot countries for articles of outside clothing to keep them cool during sunshine. Suppose we place these tw’o pieces of flaunel. in the winter time, on the snow, one hundred feet apart, the temperature of the air being at zero of Fahrenheit, and the sim shining brilliantly through a clear atmosphere, and let us watch tlie effect. In a littre W'hile it will be seen that the piece of white flannel is frozen tight to the snow, while the black flannel, haying absorbed all the rays of the sunlight from its opposite electrical condition, has become heated by the development of the heat 'from the union of these opposite eleetricites, and the snow has become melted under the black flannel. This experiment proves that heat is the result of the union of opposite electricities as in the associated primary rays of light, for the material composing the two pieces of flannel was similar, while the negatively'electrified white flannel repelled the negative white sunlight, absorbing the cold of the snow beneath, and becoming frozen to it, as the positively electrified black flannel attracted the negatively electrified wbite sunlight developing the heat wdiicb miclted the snow. Now as fevery object in nature has a colour of some kind, when the sunlight falls upon it, we can understand that the variations of temperature on tlie surface of the earth, 152 are the immediate results of electrical action upon it hy the ravs of light us light and. not hy rays of heat from the sun. We have thus shown you, that from the attributes- of heat, it is i)hvsically impossible for it to be transmitted to_ this or any other planet from the sun through an almost infinite sp-.ice . of ether at a temperature of —142° of centigrade thermometer. ■ We have shown you that the negative electricity of our atmosjfiiere is derived by induction from this very cold ether in the rotation of the earth on its axis, and in its motions in its orbit, carrying Avith it its atmosphere in its course. Wo have shown you that the atmosphere is held hi its pl-aee around the earth hy its magnetism- and dia-magnetisni, -\vliieh have hcen developed hy currents of opposite electrlc'ities in v'onjnnction, produced by the passage of rays of light thr(Uigh • the atmosphere, cvolvihg by their friction with it electrnnty of one kind, while the opposite kind of electricity has been , produced by the impact of rays of light upoii the more solid parts of. tlie earth’s crust and upon its waters as it developed ■iheir- evaporation. We have shown that the attraction of matter on or above the earth, is through magnetism to the poles opposite respectively 10 the hemisphci-es of the earth, that it is confined' to the crust of the earth, and that it is not the attraction of gravitation. We have shown that the upward pressure of all fluids, from capillary attraction in tubes to tbe upivard pressure of tbe' waters of the ocean that float tbe tonnage of the world, to that of tbe atmosphere which- holds it suspended above. the surface of the earth, is strictly magnetic. We have shoivn that the variations of the barometer at the level 'of the sea are. not occasioned by the varying -umight of the atmosphere, but by its magnetic condition, as those, of the thermometer are pro- duced by currents of electricity, ivliich permeate the glass tubes that contain the thcrmoinetric fluid. We have shown that .all terrestrial heat is derived from^ the conjunction. of oppoc.ite electricities, whether proceeding from tbe combustion, of inflammable substances, from friction, or from the contact of currents of air or of gases oppositely elec- trified. . . ' We have shown that friction of substances of low tempera- tures produces negative electricity, and increases the cold by 153 ' tlieir union, illustrated by two blocks of ice rubbed logetb ■? a!ul uniting more firmly at tbcir junction than in any otln r of tbeir parts. And tlien we have shown that positive el'i'C- trici ty is_ always associated with heat, and the opposite elec- tricity with cold; that their eonj unction produces heat or cold according as one or the other of the electricities predominates ,at the moment of their union ; that magnetism is also evolved by their conjunction, and that if much’heat is developed, the magnetism disappears and takes refuge in the nearest greater cold; that magnetism is therefore the antagonist of heat, and is found in its greatest intensity in extreme cold, in the highest part of the atmosphere, and in the Arctic and Antarc- tic regions. If the atomic theory he true, and the atoms of etlier bo spheres or oblate spheroids, we may imagine that light passino- in rays through the intensely cold ether, develops negative eloctrinity by its friction with the ether, and that this nega- tive electricity resides in the interstitial spaces between the atoms -of the ether until attracted by positive electricity of greater or lesser volume and tension, their conjunction would produce magnetism which wmuld find a habitat araoug those interstitial spaces, of the atoms of ether in the poles' of the atoms themselves. From tne mobility of the particles of fluids, whether liquid or gaseous, it appears that their tendency is to move in spiral curves. In the currents of ocean, 'sea, lake or river waters, • the frequency of their curved direction is everywhere matdfest, any obstruction to the general direction- of their currents, whether superficial, or at varying depths below the >:urntce, is sufficient to determine them into spiral curves of greater or lesser curvatures. It would seem that this attribute of fluids was intended by the Creator for the evolution of currents of electricity by the friction of these T.)articles of the inner curves of the spirals, and of magnetism by the passage of this electri- city along the spirals of the fluids themselves. This is an origin of magnetism, as well m the waters as in the atmos- phere. The great currents of the ocean, swmepiug in curves greater than a great circle of the earth itself, are only elements of immense spirals. The circular motion of an infusion of tea in a cup when stirred by a spoon to hasten the solution of the accompanying sugar, is hut an illustration of the same principle, and so it is with gaseous fluids. The tiny whirlwind that raises the dust in summer in our country roads, is but a 154 ;?f in : currents of atmosplaerie air, from tlio gentle breeze ( : 't flvi's 1:8 ill the summer beats to the tornado, hurricane, find miuhiy cyedone that desolate the oceans and islands in iii;;eiti opical regions. Thfs form, therefore, in which these fLu’ds are continually moving, is among the means adopted hy the Creator to develop electricity, magnetism and heat, oir and above the surface of our planet. “Let us for a moment consider the action of the two great currents of warm water on the opposite' coasts of K'ortlr America. The Gulf Stream and the Japanese current through' Behring’s Straits to the Arctic Ocean. Let us consider the Gulf Stream. On the Equator, in the Atlantic Ocean the mean temperature of the surface of the sea, according to Ifamtz,. 13 78.6°, the average maximum in latitude 6° north, is 80.3°, the highest observed temperature in 8° 1', iiorth,^ according to Kotzebue, 84.6°, and the mean temperature of the oea between the parallels of 3° north and 3° south, accord- iag to Humboldt, was from 80.1° to 82.4°. The mean tempera- ture of the air in the equatorial belt of the Atlantic Ocean between 10° north and 10° south, according to Lentz, is 78.8°.' Here' you have the surface water of the oceau in the Equatorial belt of the Atlantic Ocean hotter by 3.8° than air just above it. Kow, if. these respective temperatures were produced l>y emanations of heat from the sun, their condition of temperature should ho reversed, the capacity of the air to absorb heat being so much greater than that of water. This fact proves that it is not solar heat that produces the tempera- ture either in the air or water. “In July, the course of the Gulf Stream, in latitude 38° north, .shows the form of a tongue ot temperature of 81.6°, (at some places even 84° was observed.) This hot stream pro- duces itself as a double tongue, with a mean temperature of from 77° to 81.5° of Fahrenheit, (20° to 22° of Lcaumur,) to- wards the north as far as the 40° of latitude, and towards the east to the 43° of longitude west of Greenwich, that is, far beyond Newfoundland. In January, the tongue of 77° of Fahrenheit, (20° of Keaumur,) reaches to latitude 37° north and longitude 70° 30' west, and at the place where tiie east end of this tongue of 77° of Fahrenheit terminates in July, we find in Janviary a temperature of 62.5° and 62.8° of Fah- renheit, (14° and i5° of Keaumur.) “ Up to the meridian of the eastern end of Newfoundland, the Gulf Stream proceeds first in an east noi’theast, and then in an east direction parallel to the American coast, with aju average temperature in July of 77° to 83.8° Fahroalieit, (20° to 23° Reaumur,) and in Januaiy, of 68° to 77° Fahi'enheit, (16° to 20° Reaumur.) The highest temperature of the air ^frica in the same parallel ot latitude in January, is only 59°. - ■_ “At Newfoundland, the Gulf Stream comes in violent collR siou with the Polar Stream of Labrador, which nearly at a right angle sets against and penetrates into it like an immense wedge._ On the eastern side of the Grand Bank it is so powerful that, according to the surface isotherms, it pene- trate^ into the Gulf Stream from 150 to 200 miles southward'- of its general limits, and therefore entirely intersects the surface waters of the easterly stream for that breadth, which is the most important part of its course. The Gulf Stream, 800 miles northeast of Newfoundland bank, after having passed beyond this polar current, is loarmer than it is south of it. The influence of the temperature of this polar steam is le^s in January than in July. 380 miles eastward of Newfound* land, on the 50° of north latitude, the Gulf Stream has a surface temperature of 68° Fahrenheit in July, while in January, the Gulf Stream on the 50° degree of north latitudn has a temperature of 54. o° Fahrenheit j the thermometer shows at the same time at Prague, or at Ratibor, (in Silesia,) on the same parallel of latitude, temperatures of minus 24°, and sometimes still lower ones. The isothermal line of 54.5° Fahienhcit, (10° of Reaumur,) runs up in July towards Iceland and the Faroe Islands to the 61° of north latitude. There it meets for the second time the polar stream which on the east coast of Iceland again threatens to block up its way and to destroy it. In J uly, temperatures were observed on the north coast of Iceland of 45°, 47° and 49.3°, (l)y Lord Dufferin, 46°,) while off the east coast for six degrees of lono-i- tude, none higher than from 40° to 42.6° w'ere found. ° “According to Irminger’s data, and Lord Dufferin’s observa- tions, the Gulf Stream setting towards the north preponderates in July on the north and west coasts of Iceland, but on the oast and south coasts the polar stream coming from the direc- tion of Jan Mayen. “ Between Iceland and the Faroe Islands, the Gulf and polar streams are contending ngainst each other, and the result of this struggle is a sea divided into a great number of hot and cold bands, which fact is demonstrated clearly by Lord Bui- ferin’s cruise from Stornoway to Reikiavik in 1856, and fully corroborated by 'W’allich in the Bull Dog Expedition of 1860. 156 ‘‘ Tlie fact that the two streams in their contest appear as many bamls anJ- strata alougsitlCj ovcraiul beneath each othei,^ is proved not only hy the obsQi’vations of the tcmpeiatnio ot the surface of the sea by Irminger and Duffcrin, bat also by the researches of AVallicli in regard to the nature of the bot- tom of the sea. The latter found there volcanic stones point- ino- as to their origin to Jan Mayen, and at other places ophiocomfe of two to fve inches in length which could have beo-i carried there only hy the warm Gulf Stream. Besides, the drift ice penetrates here further to the south than anywhere else east of Iceland. * *' * * But here the Gulf Stream comes away erpially intact from its struggle with the polar stream as at Isewfouudland. ^Ye now know its further course in the summer from many direct observations as far north as Sphzhergen and 2Iova Zembla,and beyond the 80° of north latitude. . “ The mild Avintcr of the British Isles is well known. The mean temperature for January in London is 37.4°; at Eoin- bnr<^h the same; at Dublin 40.5°. ^ The further we go from cast to west or. from south to nortn, or, in other woids, the nearer to the Gulf Stream,the higher we find the temperature. At Dust, on one of the Shetland Islands, 500 miles north from London, the mean temperature, of the air in January is 40.3°, and that of the sea 45.5°, (East Yell.) The warm current of the sea is tempering the air. The lowest temperature observed in London was —5°, at Penzance on the west coast, fit Saudwick ou tlie Orkney Iskuids Madrid -1-13.3^ liaa been observed, and H-27.5^ at Algiers, Avhicli provides Europe with cauliflowers in .winter. “ On the morning of Feh. 8, 1870, the telegraph announced the temperature at llatihor, (in Silesia,) to be 25.4°, ’^'Lilo northwest of it, at Breslau, it was — 13°, at Berlin 0.4 , at Iviel 4-10.6°, and at Ghristiansand, on the south of Norway, 8° of latitude north of Katihor, + 30.7°. So high a temperature w’ould be impossible in Norway if the winds did not bring it from the high temperature of the Gulf Stream to the westward. “ Many persons suppose because the summer in Iceland is rou.o’h and cold that the winter must be dreadful iu its .severity of ?bld, but exactly the contrary is the case. Dr. Hendersou states, that ^ really shuddered at the thought of living through the winter in Iceland. How greatly was I astonished when I found the temperature not only higher than in Denmark, 157 ^here I had^Tieen during tho preceding winter, but also that tlio \Mnter m Iceland was hy no means more se\mre tlmn the ►-n cden Sheep and horses have to tak« care of themselves durmg tne entire year in Iceland; only cattle and the more valuable sadd e horses are fed in the stable during winter. How mipossible would It be in Germany to Idave any domestio animal in midwinter without shelter even for a few days only. It IS not to be wondered at that such is the case, because tne warm Gulf Stream provides Iceland with heat. Its mean temperature there is, even in January, 34.7° above zero, and tlie lowest iemperature noted during iwenUj years was onhi ^8:6°. Iceland is situated close to the Arctic circle, and in the lati- tude of Siberia. . Wjiile on the western side of the north Atlantic ocean, the polar ice reaches down to latitude 36° north, (the parallel of Gibraltar and Malta,) and the name Labrador is sufficient to climatic qualities of ail the land between 50° anti 60 north, there exists on the east side of the ocean alon «> the Is orwcgian, coast cultivated land up to 71° north, the nortlTern- most land of the world, in which, under the influence of the ‘ Gan btt^am, agriculture is the main occupation of the inhabi- tants. W heat IS grown up to luderoen, in latitude 64° north “ bai ley up to Alten, in 70° north, where sowina^ generally is done between the 20th. and 25th of J une, yielding in the short space of eight weeks to the 20th or 30th of August, in the average SIX or seven fold; the potato yields at the same place on the average seven or eight fold, in favourable seasons even twelve to htreen fold ; it thrives on the coast as far east as Vadso, on the J^aissian boundary line. _ At Alten (70° north) relishable cauli- liOiver 13 raised even in less favourable summers. Where washed by the polar current, there are, as shown by the various rankliu expeditions, under 70° north, but desolate ice deserts without any cultivation. There is on the eastern side of the ocean the flourishing and busy little town of Hammerfesf where only once the temperature has been as low as 4-5° and generally is not less than 9.5°, while, on the western side of the ocean there are only the poor snow huts of the ^Isquimaux in ^0° north. ^ 158 "Wliile Germany has to suffer the frigid air of — 24° and sometimes more intense cold in winter, at that same time !N"orway gathers a rich harvest under the Arctic circle, uot from its acres, hut in the warm waters of the Gulf Stream, as for instance at Ansvaer, in the direction of the vortex of the Gulf Stream ; there the herring makes its appearance aboutlho 10th day of December, remaining until the first days of Janu- ary, and then about 10,000 people congregate, and haul about 200,000 tons of these fish of a value of more than one million of dollars.” ■ The warmer air of the land near large bodies of water, whether of lakes, seas or oceans, is due to the difference of temperatures between that of the atmosphere and that of the waters, which being in contact at the surface develops one kind of electricity, which meeting with the opposite electricity of the air evolves heat and renders the climate of such localities mild, healthful and agreeable. “ East of the !North Cape, distant from it about 120 nautical miles at Vardoe,. the temperature of January is ; while at St. Petersburg, 620 miles south of the former, it is 4-15.1°, or 3.4° colder. Put the most important fact, testify- ing to the existence and the great volume of the Gulf Stream at the North Cape, appears to me to be the temperature of the sea at Fruholm, which in January is in the mean still -f37.9°. Fruholrn is on the same parallel ot latitude as Ust-Jansk, lati- tude 70° 55' north, in Siberia, and Point Barrow, in North America. The former has a mean temperature in January, of —38.6°, the latter of — 18.6°. Meran, in Tyrol, of world wide celebrity, on account of its mild and temperate air, nearer to the equator by 24J°, has in January a temperature of the air of 31.8°, Yenice, 36.3°, Vevay, 33.1°, Paris 35.4°, New York, 29.5°, Washington, 31.5°.” We will not pursue this subject of the surface temperature of the Gulf Stream to its ultimate northern development, but we will turn our attention to the temperature of the Gulf Stream, at its various depths in its course, as well as of the sea itself. “North of the isothermal line of 89.4°, (3.3° of Reaumur,) toward the pole, the temperature generally increases with the depth, while southward, toward the equator, it decreases. There is, however, no uniformity in this, : as Lieutenant Rodgers, in lS55,.foun.d in the Asiatic part of the Arctic Ocean there is on the surface a warm "current, with water of a low 159 Bpccifie gravity, bencatli it a cold current, and tlion again a warm cuiTcnt of licavier water, and all these strata ruuniug in opposite directions. , In entering upon the question of temperature of sea water at .diftereut depths, it must be home in mind that water is densest at a temperature of 39.2°, and that it arranges itself in the various depths according to the specific gravity in strata, either above and beneath, or alongside each other. From the place where the sea shows at the surface a tempera- ture of 39.2°, it will lose in temperature toward the pole, while in general, it will gain with the, increase of depth, but toward the equator the temperature of the surface will increase while it will decrease downward in proportion. Parry, in latitude 57° 51' north, longitude 41° 05' west of Greenwich, on June 13th, 1819, observed the sea to have a temperature on the surface of 40.5°, and at a depth of 1410 feet, m the Gulf Stream, 130 nautical miles southeast of Cape Farewell, a temperature of 39°. 140 miles northeast of this place, in latitude §9° 35' north, longitude 38° 6' west of Greenwich, Captain lluudsen, on the 30th of June, 1859, found the temperature of the surface 44.6°, and at the depth of 1800 feet, 43.4°, wliich corresponds with Parry’s measurements. ITallick remarks that on the parallel of latitude 63° north, not far from the south coast of Iceland, the temperatures on the surface, and at a depth .of 600 feet, differ in the average not more than 3.8°, and that consequently the Gulf Stream does not essentially lose in temperature to that depth. ^ On Irmingcr’s chart of the currents and ice drifts around Iceland, there is, in Brede Bugt, (Broad Bay,) in latitude 65° 17' north, longitude 23° 25' west of Greenwich, a temperature recorded of 46° at the surface, and of 45.5° at a depth of 300 feet, showing that the Gulf Stream at this place in the vicinity of the Polar Circle has lost in that depth only .5 of a degree of temperature. " “ Scoresby remarks, ‘ that the temperature of the sea near Spitzbergen is six or seven degrees warmer at the depth of from 600 feet to 1200 feet than it is at the surface.’ “ From the results obtained by the British Sounding Expedi- tion, from May 31st to September 7th, 1869, in the Horth Atlantic Ocean, between the Faroe Islands and Spain, it IGO iiiiyiearfj that the Gulf Stream has, between Ireland and Spain, a lajiih of aOQ fathoms or 5400 feet, and equally as mn<‘]i near th:' Ivockall rock, west of the Hebrides. Between lioclcall :'!)d the Faroe Islands, near the parallel of latitude 60‘^ north, k reaches ! 6 lhc bottorn of the sea, w])ich has a-depth there of 7i'7 fathoms, or 4G02 feet, and at that depth the Gulf Stpvam le.-s still a temperature of 41.5°. It has also been found that uu AntorcUc current of cold water, directly over the buttom of the son. (dear up to the Irish and Scottish coasts,’ exists, meeting tl yre an Arctic stream. In the notes of Professor Thomson,- the stx'atum at Bockall, from 900 to 1400 fathoms bAow the surface, is designated as cold indraught, Arctic and Arrtarctic, “ (Temperature"*39.2° to 37.4°,) and the stratum between 900 and 2435 fathoms, between Ireland and Spain, as indrauglit ” of cold water, probably mainly Antarctic, (temperature 39.2°’ to 36.5°.) ■ ' “ It is demonstrated by figures and facts, that the hot sonrcc and . cove of the Gnlf Stream extends -from the straits of Florida along the Horth Ameidcan coast at all times, day and night, in winter as in summer, even ]n January, with , a temperature of 77° and more, np to the 37° ^of north latitude, while at the same time gnd in the same latitude in Tunis, in Africa, the temperature of the air is hut 53.4°. The Gulf Stream transports and develops still in this latitude higher teniperature than either water or air possesses in the, Atlantic ocean, even under the equator, on which neither in duly nor in January the temperature is Cver as high as that of the .Gulf Stream in latitude 37° noi’th. . ‘‘ TJndor the 37° and 38° of northern latitude, the hot core of the Gulf Stream turns away from the American coast towards the east beyond the meridian of Newfoundland and its hank to 40°. of longitude west of Greenwich, where it still possesses a temjmrature in July of about 75°, and in January of about 06°. From there it proceeds to the northeast, diffuses nearly across the entire Atlantic, and snrronnds the whole of Europe to the Arctic region and the White Sea of Arckangol, with a ’lu'oad and pennaneut warm water course, without which England and Germany would he a second Labrador, and Scandinavia and Russia a second Greenland, buried beneath glaciers; whereas, in Fruholm, (71° 6' north,) the sun does not rise at all above the horizon during the entire month of January, in a latitude in which, in Asia and Ameiica, the mercuiw remains frozen for months — there the Gulf Stream preserves for the sea a temperature of 37.8°. Wliile the sun in tbc short days of winter sends forth his rajs of lijjht and wanntli hut for a few hours, and the influence of the latter is quickly lost again in the long nights, the Gulf Stream does not cease, day or night, to he the source of warmth. “ The Gulf Stream carries more heat to the north than is carried hy all the warm air currents from the entire periphery of the equator towards the ISTorth Pole and towards the SoutK Pole. The southwest winds receive their liigh temperature from the Gulf Stream, and only through the ocean — not hy the winds — can warmth he carried into ikitudes as high as those of the European coasts are. ‘"From the soundings obtained so far, the Gulf Stream must he, up to the Arctic ocean, a deep and voluminous water course. If it should not he so, the polar ice would reach also the European coasts. In the Antarctic ocean the polar ice drifts all around the glohe as far at least as latitude 57 ° 5 ' south, in many places to 50° and 40°, (latitudes corresponding respectively to those of the British Channel and the Mediter- ranean Sea,) on some even to 35°, (corresponding to the latitude of Morocco,) hut not the smallest particle of northern polar ice has ever reached even the northernmost cape of Europe. The Gulf Stream in its course is more powerful and steady than all the winds ; only the the polar ice and polar currents hi spring and summer exercise a great influence over it. The polar stream presses at three places against it: first, from the northwest, east of Newfoundland, then from the northeast of Iceland ; at both these places the polar stream is buried and proceeds beneath the Gulf Stream, after having pushed it off laterally to . the southeast. But for the third time, at Bear Island, the polar stream comes directly against the Gulf Stream from the northeast, splits it into two or three branches,^ and in places even presses it beneath its own waters at least in July. Under the lee of Spitzbergcn, this latter branch rises again and proceeds on the surface according to Parry’s observations to latitude 82|° north. The main branch east of Bear Island, has been traced by Dr. Bessels to latitude 76° 8' north, where in August, 1869, it had still a temperature of 41.2°. “ The polar streams, in conformity with the general laws of nature, are less powerful in winter than in the summer. The polar ice does not drift as far southward ; it makes fast more 162 or less lo fhe Arctic coasts and islands ; in spring and sum- raer, on the contrary, it drifts along similar to the glacier tongues, in Alpine mountains, or the ice in our rivers. The Gulf Stream is in winter more powerful than in summer, while the polar stream's, so to say, set at rest in some measure, withdraw their ice and concentrate it around the land. The relations of the temperature of the Gulf Stream within them- selves, are about the same in January as in July, the fluctu- ation between its maximum and minimum temperature, (July and January, or August and February,) would be on the average only about 9°(of Fahrenheit, ( 4“ of Reaumur.) “ What immense contrast to this extraordinary temperature is offered by the temperature of the air on the mainland! From the sea and air isothermal .line of 36,5® Fahrenheit, (2° of Reaumur,) at Philadelphia, to. Northumberland Sound, With — 40°, the distance is 2280 miles nearly due north, There is, therefore, in about each thirty miles a fall in temper- ature of one degree, as you go north. From the same p^v.at at Philadelphia to the Gulf Stream, east of Fruholm, on the same isothermal line of 36.5° Fahrenheit, (or 2° of Reaumur.) there are in the direction of the Gulf Stream, in an air lino, about 5400 miles, in which distance there is no fall at all in the temperature of the Gulf.Strcam. There, one degree of fall in each thirty miles; here, the same temperature aloiig 5100 miles in a northeast direction. Such is the influence and po-wer of the Gulf Stream. In the latitude of Berlin, which has a mean temperature of the air in January of 28°, the Gulf Stream .has 50°; at the Faroe Islands it has still 42.1° ; but in-Jakutsk, in the latitude of the Faroes, the air is 40° below zero, a difference of 82.1°.” Scorcsby remarks : “ In some situations near Spitzbergen, the warm water not only occupies the lower and mid regions of the sea, but also appears at the surface ; in some instances, 0 Y'cii arnong ice. the temperature of the sea at tlie suificc lias been as high as 86°, or 38°, when that of the air has been several degrees below freezing. This circumstance, however, lias chiefly occurred near the meridians of 6° to 12° east of Greenwich, and ive find from observations that the sea freezes! less in these longitudes than in any other part of the Spitz- bergen sea.” “ The hot source and core of the Gulf Stream extends from the straits of Florida, along the North American coast at all times, day and night, in winter . and summer, even in January, vritli a temperature of 77®, and more, up to the 37® of norfh- ■ era latitude, while, at the same time, and in the same latitude, in Africa, (Tunis,) the temperature of the air is but 63.4°. The Gulf Stream transports and develops still, in this lati- tude, a higher temperature than water and air possess in the Atlantic ocean, even under the equator, on which neitlier in Julv nor in January, the temperature is ever as high as that of the Gulf Stream, in latitude 37° north.”='= 'Why is this? We have shown that heat could not be. forceifdown by the sun along tlie line of the Gulf Stream, by any power of which we have a notion. If this heat could be derived from the sun, it is clear that the temperature of the ocean under the equator should be at least a.s great, if not much greater, than it is in the straits of Florida, or up to the 37° of north latitude; but we know, experimentally, that this is not the case, but that the heat is actually less either on land or ocean under the equator, than -it is in that portion of the Gulf Stream from the straits of Florida to the 87° of north latitude. Therefore solar I’adiation of heat is out of the ques- tion. ISTor could the great heat at the immense depths of the Gulf Stream, penetrate thereto, even if it were possible for heat to descend to our planet from the sun, for the tendency of heat is everywhere to ascend into the. atmosphere, and it could not remain permanently at those depths in opposition ■ to that tendency. We must therefore seek the cause of tins marvellous heat in the waters of the Gulf Stream, somewhere else than in the sun. We are told by our geologists that very great heat e.xists in the. interior ©f our earth — and the existence of volcanoes in many portions of the globe which are now active, as well as those which have been quiet for a period of time unknown to man, all attest the truth of their assertion. These volcanoes, past and present, have subterranean and submarine communi- cations with each other, which permeate large portions of the interior of the earth and serve to transmit any excessive ac- cumulation of heat from its immediate source to even the most distant parts of the earth’s interior, for radiation to the surface of the earth. These communications are simply flues for distributing the interior heat of the earth to its various parts. The greatest heat is and always has been under the equator, and these flues are for the most part submarine. If you will * From Dr. A. Peterman’s Essays on tlie Extension of tbe Gulf Stream. 1 16 i take an atlas of physical ^ography and cast your eyes upon the map showing the distribution of volcanoes and the regions subject to earthquakes, you will discover that the southern part of Mexico and the isthmus, connecting the two Americas arc studded with volcanoes, while the Caribbean sea is filled with them. These volcanoes are doubtless connected by flues which are united into many proximate flues in the straits of Florida, through which the surplus heat of the interior of the earth under the American continent and a part of the Atlantic ocean ami the Gulf of Mexico is transmitted to the Arctic regions, warm- ing the -waters of the Gulf Stream through its wdiole length, ^ and thus moderating the climates of the western parts of’ Europe. Another system of volcanoes will he observed almost on the same meridian, extending from Tristan d’Acunhain the southerm Atlantic ocean though Trinidad, St. Helena, Ascen- sion, Cape Verd Islands, Canary Islands, Azores, Iceland and Jan Mayen, to the Arctic regions. These volcanoes attest a central heat, forciiig a passage by the repellent a-ffinity of positive electricity with which it is associated in the direction of the polar axis of the earth, to outlets at either pole.' When obstructions are met with in the passage of this heat and electricity towards the polos in the interior of the earth volcanoes are formed, the superincumbent crust of the earth is upheaved and a vertical flue or chimney instead of the origi- nal horizontal or inclined flue is developed, and an eruption of matter is thrown out to form an island, -which in a series of ages may become a continent. These two systems of submarine' flues carrying the heat of the central portion of the interior of the eai’th under the Atlantic- ocean, a part of the American continent, the Carrib- hean sea, Gulf of Mexico and the Antilles, meet under the' Atlantic ocean to the southeast of tlie island of Iceland, each furnishing its supply of heat to maintain the temperature of the Gulf Stream, as well in its greatest depths as_ on its • extended surface. As heat ascends from its source into the atmosphere, it passes upwards from the bottom of the Gulf Stream through it to its surface, a.ssociated with Us positive electricity, where it encounters the negative electricity of the atmosphere, and by conjunction with it, increases the heat of the air above the water, which air, thus warmed, attracted by the colder air negatively electrified of the land that is nearest to it, flows in a steady wind towards it, ameliorating its climate and promoting the health and happiness of its inhabitants. 165 ■ All 'srarm currents of water, wherever they may be situated ' have a similar origin in the heat developed in the interior of the earth.^ The islands of the Pacific ocean may be all regarded as volcanic. The western coasts of America from Cape Horn to their noithern limits, furnish a corresponding proportion of volcanic action, and the warm Japanese current through Behring’s straits and along the coast of Asia, evinces a similar origin in submarine flues conveying heated air under the ocean to the Arctic regions on that side of the globe. ' “ The British expeditions for deep sea soundings ascertained the temperature of the water of the Gulf Stream, at a depth of 6000 feet, (being more than one mile,) to be 38.1°, and at 14,610 feet, (being nearly three miles,) to be still 36.5°. Com- pared with this, the deep sea temperature of the Gulf of Arabia, and eveu of the water under the Equator, will he found veiy low, sinking to 34° j in general, the deep sea temperature of the tropical oceans is lower than that of the Horth American basin. ■ J'lii the northern Atlantic ocean, between 50° and 60° of latitude, there are certain hands of water of a high tempera- ture interposed between bauds of water of a lower temperture. “ T/iese lands of a higher temperature art to be founds more or less, where a warm current and a cold current converge, as, for instance, east of Iceland.^ The two principal bands alluded to by Admi- ral Irmiuger, in his memoir, in about 60° of north latitude between the Shetland islands and Cape Farewell, are, doubt- less, the two convex vertices- of the. Gulf Stream in that region. The fact that the entire sea between Scotland and Iceland consists of a great number of such warm and cold hands of water, adjoining each other, is best proved by the cruise of Lord Dufterin, who, sailing from Stornoway, in the Hebrides to Reikiavik, between the 13th and 20th of June, 1856, ob’ served the temperature of the surface of the sea every, two hours— -in all, ninety times— and found, it to change hot less than forty-four times, or, in the average, once in fourteen nautical miles, the change fluctuating between 52,9° and 43° ; for the most part, however, between 50° and 47.8°; while on starting from Stornoway, the temperature was observed to be 48°, and on arriving at Iceland again 48°. “ There are hands, where the water is of a higher temperature close to one where it is of a lower temperature, and such I an ’s ai’c found on cacli passage across the Atlantic, l>ctwocn Faii-liill and Greenland. TlLc'’d'drereuce between tho highest- and tlio lowest tenipej atiii’cs of the sea observed on tliis line of the Atlantic ocean is 10.8°, up to 30° or 40" west of Green- wich ; to the west of this meridian, the temperature fell more rapid! j, the naoro so the nearer to Greenland. The tempera- ture of the warmest bands is defined frequently pi’ctty sharply against the waters which run through them. This high tcmpci’titure of the sea at its surface, cxtcmls 30 degrees of longitude, or at least 900 nautical miles Avest of Fairhill. “Findlay mentions that the temperature at the depth of 1200 feet Avas found to be only o5°, Avhilo on^tho surface of the Gulf Stream it reached 77.4°. In the Florida straits, Avhere the velocity of the Gulf Stream is greatest, the tem- perature at 4800 feet Avas found to bo only 33.1°. “ The AA-ai-m water of the Gulf Stream is not found at consider- able depths, much of the heat of the lower strata escaping to the surface. It is, besides,, a fact, that this Avarm water is but little apt to mix Avith the adjoining sea-water. “Above the broad Atlantic ocean, in high latitudes, in the colder seasons there is a relatively high temperature, which by the prcAmiling Avcstci’n gnd southAvestern Avinds is carried to the coasts of Europe.” Let us now consider, some of the recognized laAvs of heat and electricity. It is knoAvn, that Avhore tAvo adjacent .difi'erent temperatures exist there electricity is cvoh'od. iSloAv thcAAmters of the Gulf Stream, the Japanese current, and of other hot streams existing in the oceans and along coasts, deriving tbeir heat in the first place from the submarine lines connecting subterranean and submarine volcanoes Avith the Arctic and Antarctic regions, admit of the passage of tins beat through their globules to their upper surfaces, iu conformity to the attraction of heat from 1110 surface of the earth to the upper- atmosphere. This ascent of heat from the bottom of these' hot streams through their AA’aters to tlm atmosphere, iu conuoetioa with the indra'ught of cold Arctic and Antarctic Avaters flowing over the bottom of the oceans, is the cause of the low tempera- turc always found at such depths in those waters-s-while in- termediately from the bottom of the -ocean to the surface in such hot currents of water, the temperature varies tillit comes nto contact Avith that of the atmosphere, and that of the ocean water encompassing these hot currents of water through iheir whole extent. The contact of these different temperatures 167 ,-volvos electricity, which is positive whore the hi,j?h tempera- ture of the water pervades its greater volumes, ^id negative clectricitj’' where the cold Arctic and Antarctic waters exceed in volume, below the surface, the waters of the hot stream. The conjunction of these opposite electricities evolves heat, which being absorbed by the water where they meet serves to supply a continuous source of heat to the farthest extremities of such hot currents of^water to the Polar regions — and this is why tiiis- great heat is maintained from its original source in the Florida straits to the high latitude where it is observed. The cause of the hot waters of the Grulf Stream not mixing readily with the colder waters of the IS'orthern Atlantic ocean, will be in the junction of these opposite electricities, pro- ducing heat where these hot and cold watei’s meet. Ill ascending from the earth in a balloon, aeronauts have .discovered the same law to prevail among gaseous fluids as among liquid fluids on the earth, and that strata of heated air, even at groat elevations, are as it were sandwiched between . others of far lower temperature ; the contiguity of these strata Oi warm and cold air develops heat and electricity as well as rnagnetisra in the atmosphere, as is done also in the waters of the ocean by corresponding columns of warm and cold water in juxtaposition. These attributes of fluids are, therefore, among the great sources of the evolution of these impondera- ble powers. The cold Arctic and Antarctic currents of water, in motion to the Equator from the poles while currents of warm water Irom the tropics to the poles are. moving- beside them in a directly opposite direction, are conclusive evidences that they are impelled hj' magnetic^ attractions and repulsions in the crust of the earth, and so it is also with the aerial currents of tne atmosphere. Those of a great elevation, having a very low temperature, are attracted towards the Equator and down- vrards to the earth by its magnetism, wdiile the warm equato- rial currents, repelled from the earth by the same magnet- ism which has attracted the cold upper current downward towards it, ascend to the upper regions of the atmosphere attracted by the opposite magnetism existing there, and in both cases in opposition to the supposed law of gravitation, for tire air descending to the earth from the elevated regions of the atmosphere is much thinner and more attenuated than the air beneath, and the ascending warm air is much denser th.an the air of the regions that it seeks. The diagonal and spiral 168 - raotions of either the descending or the ascending currents of the atmosphere are produced by the ’magnetism of those portions of the atmosphere, through which they are respectively passing. When our attention is directed to the fact of the Labrador and Polar, or Arctic currents running towards the Ecpiator, while by their sides the Gulf Stream is running towards the Arctic regions in an opposite direction; and when it is dis- covered 15}' the deep sea soundings', that there are currents of water of varying temperatures at great depths which also run side hy side in opposite directions, at whatever depths, we are forced to the conclusion thg,t no eoncei^mhle system of gravita- tion can he devised to explain the anomaly. But if we apply the law of development of heat and magnetism, hy the con- junction of opposite electricities, which arc ahvays associated with differences of contiguous tem}.)erature3, the solution of the phenomena referred to becomes comparatively easy. The electro-miagnctic condition of the warm water of the Gulf Stream is repelled from the Equator, and attracted hy the opposite electro-magnetic condition of the waters and atmos- phere about the North Pole, while the cold waters of the Labrador and Arctic currents are repelled hy the similar electro-magnetism of the waters at their starting point, and are attracted towards the Equator by the opposite electro-mag- netism of the wmrm waters there. Similar causes produce similar effects in the southern hemisphere, and similar electro- magnetic forces dominate in the atmosphere all over the planet. Hence we find there, horizontal winds blowing in opposite directions, one above the other, and it is hy.this wise arrangement of oppositely electrified currents of air that the rainfall is scattered and distributed' over vast areas of the earth’s surface, modifying the temperatures and furnishing to the parched and arid soil those supplies of water for irriga- tion, so indispensable to the support of animal and vegetable life upon it. In the year 1828, 1 was detailed with two other officers of the army^ by the Secretary of "War, to make a survey of the mountainous region in the states of North and South Carolina, Georgia, and Tennessee, lying between the head of navigation on the Savannah river, at the eastern foot of the Blue Bidge mountains, and the head of navigation on the Tennessee river, on the w:esteru side of the same mountains. The object I y, 4 169 of the survey was to ascertain the practicability of construct- ing a navigable canal on the mountains, to bring the produce of northern Alabama and eastern Tennessee to Charleston, in South Carolina, and Savannah, in Georgia, instead of send- ing it to Mobile and New Orleans, and thus it was hoped by the administration of the Government to reconcile the people of South Carolina and Georgia especially, to the policy of having thp internal improvements of the country to be made by the Federal Government instead of by the State Govern- ments. On reaching our destination, I was directed to run a line of levels fronr the head waters of line Savannah river over the mountains to those of the Tennessee river, a distance, if T remember rightly, of some ninety miles. I had under my command eleven men — mountaineers — stout, strong, active, and hardy fellows. The other officers Avere employed in prospecting for other routes across the mountains,, at consid- erable distances from that I was pursuing. The country was then very thinly settled, and a portion of my route bordered on the lands occupied by the Creek or Cherokee Indians, then living in the state of Georgia. Of coursej we had to carry all our supplies with us, the country furnishing little or nothing. We were occupied on this duty some five months, from July till December. Frost appeared in the latter part of Septem- ber, on the parallel of latitude of Charleston, in South Caro- lina, and thin ice was formed on the streams almost nightly after October 15th. In the latter part of October my party was benighted in the valley of the Little Tennessee river, far away from any human habitation, on a narrow alluvial bottom, overhung by a precipitous and lofty mountain. The man detailed to bring to Us from tlie mountain ridge our supplies for the day and night, had missed his w^ay, and had descended to, the river, at a place that Ave had left several miles behind us. He had not observed our trail, and supposing that we had not passed the spot which he had reached, he kindled a fire, and remained there all night awaiting our arrival. After sending men in every direction in search of him, who returned without success, I began to make arrangements for the night. The air was cold and humid, ice being formed of the thick- ness of a quarter of an inch on the still waters of a portion of tlie river, a heavy growth of timber in the valley of the river where I had halted rendered the ground, as well as the air, very damp. The men, like myself, were all dressed in light 170 ’timer clotliing', and fire, therefore, became a prime necessity, Viiit tlie question was, how to obtain it. At that period, iu'ufer matches, if they had been invented, could not be procured where we were. My arms and ammunition, with the -rest of our supplies, were with, my wagon, rmd where it was we had not been able to discover. It occurred to me to procure fire by friction, for at that day it was thought that heat was evolved by friction. So I divided rny ten men into five reliefs of two men each, and directing some of them to gather the driest pieces of wood ' they could find, I notched, the pieces so as to make the greatest rubbing surfaces possible in them, and then I set two nien at a time'' to rub the pieces of wood together.' Having some pieces of dry paper in my pockets, I hoped to be able to kindle a fire with them, when sufficient heat should be developed by the friction of the pieces of wood. The men relie'ved each other every five minutes, after having rubbed the pieces of wood together, vigourously and rapidly; the wood became blackened, and much smoke was given out, but no fire could be produced. The^vood itself was not sufficiently dry, and none more suitable could be procured. _ The evening air was cold and damp and carried off as fast as- it was evolved the positive ' electricity which flowed from the friction pro- duced on the wood by the active rubbing of the men. One of the elements therefore to develop the heat, viz : the negative electricity of the atmosphere that we needed, was wanting. After having kept these five reliefs of the men continually busy in rubbing these pieces of wood for two- consecutive hours, I gave up^the effort in despair, and we submitted ourselves to the circumstances of our situation, and passed a dismal night of great suffering. Had the wood and the night air been dry, we should have kindled , a fire in fifteen minutes with such an amount of frictional electricity as was developed by the rubbing of the wood by the men. The experiment satisfied me that heat is only developed by the proper electrical condi- tions and not by friction of itself. As it was, all the friction we could produce did not prevent us from passing two days and nights in these mountains without food or fire, the rvater on the river, in its tranquil parts, having heen frozen a'f night of the thickness of a quarter of a dollar or an English shilling. Every housewife in the country knows that if she suffers the sunlight to fall upon the burning fuel on her hearth, the 171 combustion of tlie fuel uull be clea.'lene- mirrors tvith which Archimedes destroyed the Roman fleet at bvracuso. Tins fact, related by many historians, believed, without question, during fifteen or sixteen centuries, was, iii the seventeenth century, not only disputed, but was treated as a silly fable by many of the savans of that period. Even tae illustrious Des Cartes openly denied its possibility and we must acknowledge that with the then received opinions on iJioptrics Des Cartes was excusable for not believing the mirrors of Archimedes ever to have existed. This incredulity, on the part of many persons claimin'^- to be scientists, excited the interest of M. de. Buflbn, the cele- brated naturaast, at the time the Intendant of the Jardin des 1 iantes, at Paris. He determined to test the question practi- cally, and for this purpose constructed a system of reflect! n a- plane mirrors, by wEich he attained complete euccessi He be^an^ by measuring the loss of illuminating power in the reflection of the sun’s rays from metallic mirrors of the finest polish, w’hen compared \vith the loss so sustained by reflec- tion trom plane glass mirrors covered on their backs with tin' found that the glass mirrors lost less light bv reflection than the metallic mirrors did, hut that it required two plane glass mirrors of the same dimensions to produce,; 176 at a givoa distance, an, illumination equal to that from the samelinobstructed beam of sunlight passing into an obscure roor.i through an aperture in the window shutter, and conse- quently, that the number of his_ glass mirrors should be largely increase^) to produce any sensible effect on combustible sub- stances. After studying his subject iu its.various relations to the laws of light and heat, as thou understood by scientific men, M; de Buffon constructed Ids mirror of 168 pieces^ of plane glass, covered on the back with tin foil, each piece-being ■six inches wide by eight inches long, separated, from each other by four Hues, and mounted on a stand, which was sus- ceptible of being moved in every direction;, each of these glasses had a separate setting, so that it could be separately •moved in every direction, independent of the movemouts of the other glasses. It required about half an hour to adjust the reflected images of thesuu froru these mirrors into a com- mon focus. When the glasses were properly arranged, and the focus adjusted, a board of beech wood covered with pitch, was set on fire by 40 of these glasses at the distance ot 66 teet, with 98 glasses, a board covered with pitch and sulphur was set on fire at the distance of 120 feet. A slight combustion was produced on a hoard covered with wool cut very fine, by employing 112 glasses, at the distance of 138 feet, with a very pale sun. At 150 feet of distance, a board covered with pitch was made to smoke with 154 glasses, and it was thought that it would have been burnt if the sun had not become overcast with clouds. With a still feebler sun, chips of pine wood covered with pitch have been set on fire in one minute and a half, at the same distance, with a like number of glasses. With- an unclouded sun, a pine board, covered with pitch, at the same distance, has been quickly set on fire ^'"dh 128 glasses, and the fire has caught the whole surface of the focus, V hich was 16 inches in diameter, at that distance. Finally, the focus having been shortened to the distance of 20 feet, with 12 glasses' the substances easily combustible were set on fire. With 45 glasses a tin canister, weighing ^six pounds, has been quickly melted with 117 glasses. Thin scraps of silver have been melted, and a sheet of iron has been made red hot ; and there was reason to believe that if all the glasses of the mirror had been used, metals could have been as easily melted at 50 feet distance as at 20 feet. These experiments have been .made with a sun of a spring time, and without much power, having been enfeebled by atmospheric vapours, If then, with these disadvantages, wood 177 could be burnt at 150 feet distant, we may wfell tliink, that: with a summer’s sun, it could be readily burnt at 200 feet distance, and with three similar miVrors it could be set on fire at 400 feet distance. M. de BufFon thought that with mirrors similar to his own, combustibles- could not be inflamed beyoiid a distance of 900 feet. Let us attempt an explanation of these phenomena. The enormous veioeity of rays of light in coming to our planet, establishes the'flict that they cannot touch each other in their passage, since if they jostled each other their velocity would be greatly diminished. Repelled from each other, therefore, by their own negative electricity, as well as by that they have received from the cold ether through which they have passed, they are attracted to the glass of tlie mirrors and their metal- lic backing, by-the vitreous or positive electricity of those sub- stances. "On striking the glass, these rays pi’oduce friction, which evolves positive electricity, the junction of these oppo- site electricities evolves heat and magnetism, the rays of heat thuS' developed follow the same laws as do those of light, and iogether, both are reflected from the mirrors and are directed to the ecmmon focus, where their co’uceutration sets oh fire combns'dJhe substances, and melts and vaporizes those of a more obdarate asid intractable character. The refraction and. rcflectioic as v','cll as the polarization of light, are due to the repellent aiflaity of electricity. When we are told that on many parts of the earth’s surface mountains have been upheaved till their peaks and ridges, at distances varying from 16,000 to 28,000 feet above the level of the sea, appear to be covered with snow, which from year to 3 'ear, and from century to century, continues to cover them, no matter in what latitudes they may exist, nor in wliat sea- son of the year they may be examined, we naturally ask our- selves, wiry is this? How does it happen, that these snow- capped peaks and ridges, at such great elevations above the sea, far above the region of the atmosphere in which clouds aud vapours habitually love to roam as it were at will, bask- ing in a resplendent and brilliant sunlight, receiving all tiro supposed emanations of heat from tiro sun, that philosophers of every age Jiave innocently conjectured that that luminary, like a Imman spendthrift, was lavishing upon infinite space, in all directions, that a small portion of it might reach our pljauet, should preserve their mantles of perpetual snow, in all sea^rus, .iu all climatic changes that are -occurring every moment thousands of fpet beneath them, and thus continue defying, as it would seem, the mutability of all other earthly things ? Some of our philosophers of the highest distinction, have gone into the most elaborate calculations to show what enormous columns of ice, of the greatest density, could be melted by the heat of the sun, in its constant emanation, in the smallest spaces of time, in the face of the fact that the enow clad mountains, that happen to be the nearest to the 6un, have been from time immemorial, unaffected in thd slightest manner, by any heat derived from that great lumi- nary. Let us attempt an explanation of tiiis wonder. The colour of snow is white. It has a low temperature. Its elec- trical condition is negative, as is the white colour of sunlight, as arc the rays of sunlight which reach us through the nega- tively electrified ether of space, also intensely cold, and the intensely cold upper strata of our atmosphere. As a conse- quence, white sunlight, negatively electrified, falling upon the white snow capped mountains, also negatively electrified, as are also the strata of our atmosphere into which these moun- tains lift their heads, these similar electricities repel each other. The white sunlight is reflected into space from the snow covered mountains, which remain undisturbed, and no trace of the action of heat, as derived from the sun, is any- where visible upon them. If the sun is a great magnet, it must have its magnetic poles, with their reciprocal attractions and repulsions. The plane of the sun’s equator is said to be neither perpendicular to nor coincident with that of the ecliptic. Its magnetic poles may therefore be differently situated in it to the positions occupied in the earth by its magnetic poles. From the supposed enor- mous volume and intensity of magnetism in and about the sun, we may infer that the velocity of the planets and of cometary matter in their respective progress in their orbits, would bo checked when in their several perigees or nearest points to the sun, from its great magnetic attraction, and that as they severally I'eccclod therefrom, those velocities would be in- creased from the loss of the sun’s attraction by increase of distance from it, and the nearer approach to their apogees, or greatest distance from the sun, where the sun’s attraction would be the least, and the opposite magnetic attraction of the ether of space would be the greatest. If it were not for the interior forces of the planets, &c., causing their rotations, on their axes, we might suppose that their movements around the sun might be stopped entirely, when they had severally reached their perigees by the magnetism of the sun. 179 Wlieiitvro magnets of different magnetic volumes and in- tensities are brought near each other with similar poh'S towards each other, the greater magnet will repel the lesser if their opposite poles approach each other, the feebler will be attracted by the stronger. Now the sun having much greater magnetic power than the earth, when the latter is at its peri- gee its velocity must be retarded by the greater attractive magnetism of the sun, which would hold it fixed when in peri- 'gee, but for the rotation of the earth on its axis, driving it’ forward, and that, retardation or holding it back after it had passed its perigee would continue until the earth had receded so far from its perigee as to have reached the attraction of the opposite magnetism beyond its apogee. . The sun exhibits every characteristic and evidence of a bodv enveloped in two atmospheres, so to state, the one in contact with it being the region of white light, called the 'photosphere, and outside of that, a region in which coloured light is some- times manifested, especially along' the edges of the solar disc, and which last region is called the chromosphere. The. spots on the sun are supposed to be holes of various forms and dimensions in the region of white light, through which the dark body of the sun itself has been seen. These spots or holes are liable to variations, and are analogous to the spots of sunlight on the surface of the earth, which are sometimes seen to be surrounded by the shadows cast upon the earth by the clouds above it. Nasmyth, in the year 1866, made the aiscovery that the luminous portion of the sun’s disc is not composed of light of equal or homogeneous intensity, but consists of a minutely divided series of luminous streaks, which he described as like willow leaves, around which the light is less intense, or rather the photosphere is more trans- parent. These willow leaves appeared to cross each other in all varieties of directions, and their average magnitude w’as about one thousand miles long, by a hundred miles broad ; other observers have preferred to describe these appearances as “granulations,” “rice grains,” and “shingle beach,” and as having elliptical forms, and of much smaller proportions. The moon, we know to be a reflector, of light without the emission of any accompanying heat. The picture of the face of the moon exhibited to us, represents great irregularities in its surface, depressions, as if they were craters of extinct vol- canoes, and elevations of great altitude, conveying the idea of volcanic mountains; but the general colour is that of a litrht • > i ' 180 grey, not unlike to sheets of zinc, or tin foil,' the latter of which we use as hacks or reflecting surfaces in our glass mirrors. If we thus get our nocturnal light from the. moon, unac- companied hy heat, why should we insist upon violating the well established laws of heat in its radiations, and declare the sun to be an incandescent body, continually in active com- bustion, requiring inconceivable masses of fuel of sOme kind’ to maintain it, and surrounded on all sides by an immensity of ethereal space of so low a temperature that any radiation of heat from the sun must necessarily be absorbed and neu- tralized as soon as it should leave the body of the sun ? We therefore, for the reasons stated in this book, reject entirely the theory of the incandescence of the sun, and of its lumi- nous metallic vapours of great intensity of heat. We have shown in the body of this work, that the- colored lights constituting the primary rays of light, which are emitted from the various orbs of the firmament, negatively electrified, and arc propelled by the cold negatively electrified ether through which they are continually passing to the sun, and through its transparent or translucent chromosphere to the photosphere of the sun, are there commingled to prodfice its white light, which then is repelled or reflected from the grey “ willow leaves,” “granulations,” “ rice grains,” •or whatever they may be, into ethereal space by the same negative electricity, which has been, associated with them throughout, . a portion of which comes to us as the white light of the sun. This shows the synthesis or formation of the white light of the sun, and that it is merely an associa'tion of the primary rays of light thrown together by electrical and magnetic attra'Ctions and repulsions in the photosphere of the sun, and so easily separable that the slightest change in the angle qf incidence of the white light of the sun, as it falls upon vapours, clouds, or gases will excite their repellent affinities, and resolve them into the varied and brilliant tints of primary and com- posite colours, which everywhere in the temperate regions, serve to excite our astonishment, wonder, and delight. These changes need no accompaniment of heat, and as they are without it, we return to the declaration of Moses, that “ God made two great lights, a greater light to rule the day, and a . lesser light to rule the night and the stars. 181 “ And L.e set them in the firmament of heaven to shine upon the earth, and to rule the day and the night, and to divide the light and the darkness ; and God sa-w- that it was good.-’ Among the fallacies of science, as taught in our schools, to some of which I have alluded in this book, there is not one more surprising than the statement made by our astronomers,, that the earth, the planets, and the sun itself continually 'revolve on their respective axes, and in their orbits from west to east. We are also told that these orbits are elliptical curves which return into themselves. . Ifow we will illustrate this movement by supposing that a man has started from San Francisco, on the Pacific Ocean, to travel on the same parallel of latitude from west to east around the world. After he has travelled one hundred and eighty degrees on this parallel of latitude, he finds that he has reached the east cardinal point from San Francisco, and if he should continue his journey, he must travel westward, which course will bring him in time back again to San Francisco. How is it possible, therefore, in a curve which returns to itself to travel always in the same direction ?. There can be no fixed cardinal points in any solar or stellar system which is always in motion. In regard to the diminutive planet which we inhabit, the curvature or annulus of magnetic poles, north and south, is. sufficiently stable and fixed to furnish cardinal points of the compass, to regulate our journeyings upon it; but with planets, stars, and suns, it is different. They have no fixed points in the celes- tial sphere, of which we have or can have any knowledge, to which ti!e direction of their movements can.'be referrech it is simply an absurdity to attempt to assimilate planetary and stellar motions to those of mankind on our earth. The planes of the orbits of the planets are neither coincident with, parallel, nor perpendicular to each other, but they are supposed to intersect each other in such a manner that the sun shall always be in a focus, common to all of these ellipti- cal orbits; consequently any perpendicular line or plane to any one of those orbits, cannot be perpendicular to any other of them; and hence, there can be no cardinal points common to them all, and their motions cannot be from west to east. My task is finished. When, in the beginning of this cen- tury, It was announced that the primary rays of light had dif- ferent attributes, and among them, that the blue ray stimulated vegetation in a remarkable degree, many persons on the con- 182 tlncnt of Europe, as well as in the British Isles, instituted experiments, with a view to utilize these rays. Their experi- rnenls were failures, as- they were made with homogeneous tinted glass, each of the primary rays having in this w;ay been somewhere tested, but without' satisfactory results. A know-, ledge of these failures induced me to examine the subject of ve^table growth in its natural conditions. I soon discovered that where vegetation was most luxuriant, and- exuberant, there the brilliant sunlight was always associated with the blue light of the firmament. That during the torpor of winter, the rays of sunlight fell upon the earth, owing to the declination of the sun, at such acute angles of incidjpnce,^ that many of ■ them were reflected into space without stimulating life on this planet, while, at the same ti.me, the blue .colour of the sky was intercepted. from our vision by the watery vapours and clouds that were constantly floa ,\ng. in the atmosphere. The absence, therefore, of the blue colour of the sky, and many of tlie rays of sunlight at this season, together with its low temperature, convinced me that the Creator intended it to be a season of rest for vegetable and animal life, a sort of Sabbath, in which life, though existing in plants and animals, was reposing from its activity, to be aroused into exercise on the return of the season of spring,' when from the less declination of the sun, mor^ of its light would he thrown upon the earth, associated with the blue colour of the sky, then unmasked by the dis- sipation of the clouds and watery vapours which had con- cealed it during the winter just. past. I said to myself, “ here is the secret of the failures of these European experiments with the primary rays of light. I will follow the guidance of the Creator in cultivating iny vines. . I will associate the sun- light with the blue colour of the sky, intensifying the latter. I will make a tropical clirnate and atmosphere in the temper- ate zone,” The results are... before you. The reflections I have made on this subject have induced my investigation into the Physics of Nature. I have not been satisfied with what I -have been taught iu the schools. Their explanations are not consistent with the known or presumed facts. I have ven- tured, therefore, to form nay own conclusions, irrespectivemf dogmas that have been thrust upon mankind for centuries. I do not profess to teach any one, but as a human atona among the masses of mankind, for whom all knowledge should he disseminated, I venture to impart to the public the conclu- sions to which I have arrived on these subjects, and that pub- jlc may attach to them whatever value they please. APPENDIX TO PAET IL P-] A very remarkabl.e confirmation of my theory of the forma- tion of the- equatorial diameter of the earth, as well as of those of the other planets, by magnetic attraction and repulsion from their respective poles, thus increasing those diameters in various proportions over their several polar diameters, has unexpectedly appeared in a paper read before the American Academy of Sciences, at their meeting in this city held on Thursday last, November 4th, 1875, and sent to it by Professor Joseph Le Conte, of the University of California, a synopsis of which was published in the supplement to the Public Ledger^ of this city, on Saturday, November 6th, 1875. The paper was. entitled “ On the Evidence of Horizontal Crushing iir the Formation of the Coast Range of Mountains in California,” being the result of recent observations by the author. Tiis theory is, that mountains are formed wholly by a yielding of the crust of the earth along’ certain lines to horizontal pres- sure, not by bending into a convex arch filled and sustained by a liquid beneath, but by a mashing together of the whole crust Avith the formation of close folds and a thickening or SAvelling upwavd of the squeezed mass. The author walked sIoAvly through the-cut made by the Central Pacific Railroad, from the plains adjoining the bay of San Francisco through the Coast Ridge mountains to the San Joaquin plains, a dis- tance of thirty miles. Both the sub-ranges into which the range is divided are composed wholly of crumpled strata, those of the Avestern sub-range being crumpled in the most extraordinary tnanner. The sub-rswige nearest the bay is ex- ceedingly complex. From measurements of the aiigles of dip the actual length of the folded strata is two and one-half •to three times the horizontal distance through the mountain. There must have been fifteen to eighteen miles of original sea bottom crushed into six miles, with a correspon4ing upswell- ing of the whole mass. 183 ) 184 • To anticipate inquiry and satisfy curiosity respecting the history of the author of the experiments mentioned herein, and of the hook itself, his civil and military history is as fol- lows, viz : ATJGUSTIJS JAMES PLEASOFTOEr, horn in the city of JVashington, in the District of Columbia, January 21st, A. D. 1808. He was the second son of Stephen Pleaspnton, of the state of Delaware, and Mary Hopkins, his wife, of the county of Lancaster, state of Pennsylvania. His father, Stephen Pleasonton, entered the service of the government of the United States, in the State Department, in the year 1800, and continued to serve it till his. death, which occured in the year 1854, after a service of more than fifty years. He was Eifth Auditor of the Treasury Department, Acting Commissioner of the Kevenue of the United States, and Chief of the Light House Department, for many years. He was of Forman ex- traction. Eis wife was the third . daughter of John Hopkins, a sub- stantial fanner of the county of Lancester,. in the state of Pennsylvania, who for very many years represented his county in the Senate of Pennsylvania. Her ancestry was English. Their son, Augustus, was appointed a Cadet of the United States Military Academy at West Point, from the District of Columbia, July 1st, A. D. 1822, continued as such till July 1st, 1826, when he was graduated and promoted in the army, to Brevet Second Lieutenant of the Sixth Eegment of Infantry July 1st, 1826, Second Lieutenant Third Artillery June 1st, 1826. Transferred to First Artillery October 24th, 1826. Augustus James Pleasonton, served in garrison at Fortress Monroe. Virginia;' at the Artillery School of Practice in the years lo26 and 1827, and on Topographical duty, from June 16th, 1827, till January Hth, 1828, and from June 14th, 1828 till June 30th, 1830. Resigned his commission in the army June 30th, 1830. Hrs CiviSi.. History. — Counsellor at Law at Philadelphia, Penn., since the year 1832. Brigade Major in Pennsylvania Volunteer Militia in the years 1883 and 1835, Colonel of Volunteer Artillery, of Penn., from 1835 till 1845, being severely wounded July 7th, 1844, with a musket ball in the left groin, while commanding his regiment in a desperate con- 185 liict, with a Ibrmidahle body of rioters, armed with muskets and cannon, in Southwark, Philadelphia county, Penn, As- sistant Adjutant General and Paymaster General of the state of Pennsylvania from December 11th, 1838 to October G 1th, 1839, during political disturbances at Harrisburg, Penn.’ President of the- Harrisburg, Portsmouth, Mountjoj and Lancaster Railroad Company, of Pennsylvania, in the ve-vs 1839 and 1840. ' His Military History.— Served during the Rebellion of the seceding states- froin. the year 1861 till 1866 as Brigadier General of Pennaylvanir Yolunteer Militia. Appointed May 16th, 18.61, under an act of the Legislature of the state’ ot Pennsylvania, to organize- and command -a Yolunteer Army Corps of 10,000 men of Artillery, Infantry -and Cavalry, as a Home Guard for the defence of the city of Philadelphia, Penn. IT