m- \ . CONVERSATIONS ON IN WHICH THE ELEMENTS OF THAT SCIENCE ARE FAMILIARLY EXPLAINED, AND ADAPTED TO THE COMPREHENSION OF YOUNG PUPILS. BY THE AUTHOR OF CONVERSATIONS ON CHEMISTRY, AND CONVERSATIONS ON POLITICAL ECONOMY. WITH ADDITIONAL ILLUSTRATIONS AND APPROPRIATE QUESTIONS FOR THE EXAMINATION OF SCHOLARS, BT REV. J. L. BLAKE, A. M. Principal of the Literary Seminary, Concord, New Hampshire. FlfTB AMERICAJr KDITIOJr. HARTFORD : PRIKTBD BT GEORGB «OODWIN. 1823. DISTRICT OF NEW-HAMPSHIRE :-TO WIT. District Clerk's Office, »********« T) E it remembei-ed, that on the twenty-seventh day of March, A. D, » L S * JlJ 18-23, and in the forty-seventh year of the Independence of the * • * J Umted States of America, JOHN LAURIS BLAKE, of the said District, »«««*««*«* ^3th deposited in this office the title of a book, the right whereof he claims as author in the words following, viz. " Conversations on Natural Philosophy, *' in which the elements of that science are familiarly explained, and adapted to the *' comprehension of young pupils. Illustrated with plates, ay the author of Conver- ** satious on Chemistry, and Conversations on Political Economy. With additional *' ilhisirationsand appropriate questions for the examination of scholars, by Rev. J. L. •* BLAKE, A. >L Principal of the Literary Seminai7, Concord, New Hampshire." In conformity to the act of the Congress of the United States, entitled " An act for the encouragement of learning by securing the copies of maps, charts and books to the authors and proprietors of such copies, during the times therein mentioned;" and also to an act ir-ntitkd '• an act supplementary to an act entitled an act for the encourage- ment of 1 .arning, by securing the copies of maps, charts and books to the authors and proprietorsof such copies, durinj? the times therein mentioned, and extending the ben- efits thereof to the arts of designing, engraving and etching historical and other prints." WILLIAM CLAGGETT, Clerk of the District of New- Hampshire. A true copy of record, Attest, WILLIAM CkAGGETT, Clerk. PREFACE. ■'••©^5© *<*■" It is with increased diffidence that the author offers this little work to the public. The encouraging recep- tion which the Conversations on Chemistry, and Pohtical Economy have met with, has induced her to venture on publishing a short course on Natural Philosophy ; but not without the greatest apprehen- sions for its success. Her ignorance of mathematics, and the imperfect knov/ledge of natural philosophy which that disadvantage necessarily implies, renders her fully sensible of her incompetency to treat the subject in any other way than in the form of a familiar explanation of the first elements, for the use of very young pupils. It is the hope of having done this in a manner that may engage their attention, which encour- ages her to offer them these additional lessons. They are intended, in a course of elementary science, to precede the Conversations on Chemistry ; and' were actually written previous to either of her former publications. [by the AMERICAN EDITOR.} The Conversations on Natural Philosophy, by the author of Conversations on Chemistry, are probably better adapted to the minds of females and to persons generally who are only to acquire the great principles of natural science independent of abstruse demonstra- tions, than any other treatise pubhshed on tlie subject. A persuasion of this, induced the author of the following Questions for the examination of scholars in that work, to introduce it into the Seminary of which he has the superintendence. He soon found, however, that his pupils were frequently embarrassed in not knowing, to what particular parts they were chiefly to direct the iv PREFACE. attention, committing to memory what was not neces- sary and omitting what was, causing thereby a great loss of time as well as of improvement. This led to the present system of questions, by the use of which it was quickly ascertained, that his pupils could complete their lessons in about half the time they before needed, and far better than they could before possibly get them. And this determined the author to publish and append them to the work ; and in coming to the determination, it occurred to him, that some additional illustrations might advantageousl}^ be introduced, which, together with the questions, would form a valuable improvement. J. L. BLAKE. Concord, N. H. 1823. INDEX. A. Am, 15, 19, 32, 56, 145, 173, 192. Air-Pump, 36, 147. Angle, 49. — , acute, 50. , obtuse, 50. of incidence, 51, 170, 184. of reflection, 51, 163, 169, 184. of vision, 178, 180. Aphelion, 82. Arctic circle, 99, 1 07 Atmosphere, 111, 138, 145, 155, 173. , reflection of, 158. , color of, 203. — — — , refraction of, 190, 193. Attraction, 14, 19, 28, 190. ■ , of coiiesion, 19, 39, 126, 145. — , of gravitation, 23, 36, 77, 87, 103, 122, 145. Avenue, 180, Auditory Nerve, 164. Axis, 84. of motion, 54, 60. of the earth, 99, 106. of mirrors, 186. - of a lens, 195. B. Balloon, 35. Barometer, 149. Bass, 164. Bladder, 147. Bodies, 14. ' , elastic, 45, 55. , luminous, 166. — , sonorous, 160, 164. , fall of, 28, 31, 35, 42. , opaque, 166, 190. -, transparent, 167, 190. Camera obscura, 173, 183, 212. Capillary tubes, 22. Centre, 54. of Gravity, 54, 57, 59, 61, 122. »— of motion, 54, 60, 123. of magnitude, 54,58. Centrifugal force, 55, 79, 102, 122. Centripetal force, 55, 79.- Ceres, 91. Circle, 48, 101, 103, Circular motion, 53, 79. Clouds, 137. Colors, 28, 195. Comets, 92. Compression, 47. Concord, 165. Constellation, 92. Convergent rays, 185, 187. Crystals, 16. Cylinder, 58. Bulk, 20. 22 Day, 84, 112. Degrees, 49, 101, 106, 181. of latitude, 101, 119. of longitude, 101, 119. Density, 20. Diagonal, 53. Diameter, 101. Diurnal, 85. Discords, 164. Divergent rays, 185. Divisibility, 14, 16, E. Earth, 23,77,90, 90,98. Echo, 163. Eclipse, 117, 120, 168. Ecliptic, 93, 100. Elastic bodies, 45, 46. fluids, 19, 33, 127, 145, ;!j4 INDEX. Ellipsis, 81. Essential properties, 14, Exhalations, 17. Extension, 14, 15. Equator, 99. Equinox, 107, 108. , precession of, 114. Eye, 173. Fall of bodies, 28, SI, 35, 42. Figure, 14, 16. Fluids, 126. , elastic, 127, 145. , equilibrium of, 128, 150. , pressure of, 129, 140, 150. Flying, 45. Focus, 186. ' of convex mirrors, 187. — of concave, 188. • ■ of a lens, 194. Force, 38. , centrifugal, 55, 79, 102, 122. , centripetal, 55, 79. — ^ of projection, o6, 78. of gravity, 23, 77, 87. Ill, 145. Fountains, 143. Friction, 74, 144. Frigid zone, 100, 107. Fulcrum, 60. G. General properties of bodies, 14. Georgium-Sidus, 91. Glass, 194. , refraction of, 194. — — , burning, 198. Gold, 13:3, Gravity, 23, 28, 36, 38, 42, 56, 57. II. ilarmonv, 156. Heat, 20, 110. Hemisphere, 99, lCt7. llvdi'ometer, 136. Hydrostatics, 126. T. lini';;^eo.t tin; retina, 1743 182. Image r-:? versed, 1 76. Hi i.Iriin mi'iTor. 183. ' in convex ditto, 185, — - in concave, 185. Impenetrability, 14. Inclined plane, 60,72 Inertia, 14, 18, 39. J. Juno, 91. Jupiter, 9§, 120. Lake, 142. Latitude, 101, 119. Lens, 194. ' , convex, 194. , concave, 195. Lever, 60. -, first order, 64. ' -, second ditto, 66. , third ditto, 66. Light, 166. ' ■, pencil of, 167. , reflected, 169. , of the moon, 171. — -, refraction of, 190. , absorption of, 198. Liquids, 127. Longitude, 101, 119. Luminous bodies, 166. Lunar month, 116. - eclipse, 117. M. Machine, 60, 72, 74. Magic Lanthorn, 213. jNTars, 90. Matter, l4, 44. Mechanics, 60. Mediums, 167, 190. ]Melody, 165. Mercury planet?, 89, 121. Mercury, or quicksilver, 149. ^feridians, 100. ^Microscope, 21 1, 214. , sins^'le, :^11. » solar, 211. Minerals, 16. Minutes, 101. i^ Lou soon s, 157. Month, lunar, 116. Momcntiini, 43. 63. Moon, 80, 87, 91, It B, 121. I^'DEX. 255 Moon -light, 171 Motion, 18,58,44, 45. — — , uniform, 40. , perpetual, 40, — — , retarded, 41. , accelerated, 41 . — — , reflected, 48. — — , compound, 52. — — , circular, 53, 70. , axis of, 54, 61, — , centre of, 54, 60, 122. — — — , diurnal, 84. Musical instruments, 164. Mirrors, 183. — — — , reflection of, 183. , plane or flat, 185, , convex, 185. ■ ■ -, concave, 185, 187. —- , axis of, 186. — ~, burning, 188. N. Neap tides, 124. Nerves, 175. — — , auditory, 164, 175. Nerves, optic, 173, 175. — ', olfactory, 175. Night, 84. Nodes, 106, 107, 114. O. Octave, 165, Odour, 17. Opaque -bodies, 166, 167. Optics, 166. Orbit, 89. P. Pallas, 91. Parabola, 57. Parallel lines, 30. Pellucid bodies, 167. Pencil of rays, 167. Pendulum, 104. Perihelion, 82, Perpendicular lines, CO, 49, ICQ. Phases, 117. Piston, 152. Plane, 100. Planets, 83, 87, 111. Poles, 99. Polar star, 107, 119. Porosity, 47. Powers, meclianical, 60. Projection, 56, 78. Precession of the equinoxes, 114, Pulley, 60, 68. Pump, 36, 37, , sucking or lifting, 1 53, I -, forcing, 153, 155. Pupil of the eye, 173. R Rain, 138. Rainbow, 198. Rarity, 20. Ray of light, 201. of reflection, 169. of incidence, 170. Rays, intersecting, 173. Reaction, 44. Receiver, 36. Reflection of light, 169. • -, angle of, 51, 184. of mirrors, 183. — — - of plain mirrors, 1 85. - of convex mirrors, 185. of concave mirrors, 185. Reflected motion, 48. Refraction, 190. of the atmosphere, 192, i of glass, 194. of a lens, 194, of a prism, 195, Resistance, 60. Retina, 173. , image on, 174*. Rivers, 137. Rivulets, 139. S. Satellites, 87, 1 19, 120. Saturn, 91. Scales or balance, 61. Screw, 60, 73. Shadow, 117, 168. Siderialtime, 113. Sight, 175. Signs, Zodiac, 93, 100, 101. Smoke, 1 8, 34. Solar Microscope, 211. Solstice, 106, 107. Sound, 159. — — , acute, 1 64. ■ , musical, 164. Space, 39. Specific £^ravity, 131. ^ of air, 149 . Spectrum, 196. Speaking trumpet, 163. Sphere, 31, 58, 103. 256 INDEX. SpringSj 137. Springtides, 1-24, Square, 88, 92. Stars, 83, 93, 112, 119. Storms, 156. Substance, 14, Summer, 82, 106. Sun, 77, 87, 166, 192. Swimming, 46. Syphon, 141. T. Tangent, 55, 79. Telescope, 214. ■ , reflecting, 214. — , refracting, 214. Temperate zone, 100, lOS. Thermometer, 151. Tides, 121. — -, neap, 124. , spring, 124. ■— , aerial, 159. Time, 112,114. , siderial, 115. , equal, 115. ■ , solar, 115. Tone, 164. Torrid zone, 100, 108, 1S6. Transparent bodies, 167. Treble and bass, 164. Tropics, 99. U. Undulations, 162. Unison, 165. Y. ValTc, 152. Vapor, 21, 34, 137. Velocitv, 39, 63. Venus, 90, 121. Vesta, 91. Vibration, 161. Vision, 178. , angle of, 178. , double, 182. W. Waters, 126, 139. — — , spring, 139. -, rain, 139. -, level of, 128, 133, 137. Wedge, 60, 7?,. Weight, 20, 28,103, 131, 146, 147. Wheel and axle, 60, 71. Wind, 155. , trade, 156. , periodical, 157, Winch, 73. Winter, 82, 107. Year, 112. , siderial, 113. — , solar, 114. Z. Zodiac, 93. Zone, 100. , torrid, 100, 108, 156, 193. , temperate, 100, 108. , frigid, 100, 107. CONTENTS. CONVERSATION I. On General Properties of Bodies, Introdwction ; General Properties of Bodies ; Impenetrability ; Extension ; Figure ; Divisibility ; Inertia ; Attraction ; Attraction of Cohesion; Density; Rarity; Heat; Attraction of Gravitation. Page 13 CONVERSATION II. On the Attraction of Gravity. Attraction of Gravitation, continued ; Of Weight ; Of the fall of Bodies ; Of the resistance of the Air ; Of the Ascent of Light Bodies. Page 27 CONVERSATION HI. On the Laws of Motion. Of Motion; Of the Inertia of Bodies; Of Force to Produce Motion; Direction of Motion ; Velocity, absolute and relative ; Uniform Motion ; Retarded Motion ; Accelerated Motion; Velocity of Fall- ing Bodies ; Momentum ; Action and Re-action equal ; Elasticity of Bodies; Porosity of Bodies; Reflected Motion; Angles of Inci- dence ai}d Pwcflection. Page 3$ CONVERSATION IV. On Compound Motion. Compound Motion the result of two opposite forces ; Of Circular Mo- tion, the »-esuit of two forces, one of which confines the body to a fixed point ; Centre of motion, the point at rest while the other parts of the body move round it; Centre of Magnitude, the middle of a body ; Centripetal Force, that which confines a body to a fixed central point ; Centrifugal Force, that which impels a body to fly from tlie centre ; Fall of Bodies in a Parabola ; Centre of Gravity, the Centre of W^eight, or point about which the parts balance each other. Page 52 \J CONTENTS. CONVERSATION V. On the Mechanical Powers, Of the Power of Machines ; Of the Lever in general; Of the Lever of the first kind, having the Fulcrum between the Power and the weight ; Of the Lever of the second kind, having the weight between the power and the Fulcrum; Of the Lever of the third kind, having the power between the Fulcrum and the Weight; Of the Pulley ; Of the Wheel and Axle ; Of the inclined Plane ; Of the Wedge , Of the Screw. Page 60 CONVERSATION VI. ASTRONOMY. Causes of the Earth^s Annual Motion. ©f the Planets, and their motion ; Of the Diurnal motion of the Earth and Planets. Page 77 CONVERSATION VII. On the Planets, Of the Satellites or Moons; Gravity diminishes as the Square of the Distance ; Of the Solar System ; Of Comets; Constellations, signs of the Zodiac ; Of Copernicus, Newton, Szc. Page 87 CONVERSATION VIII. On the Earth. Of the Terrestrial Globe ; Of the Figure of the Earth ; Of the Pendulum ; Of the Variation of the Seasons, and of the Length of Days and Nights ; Of the Causes of the Heat of Summer ; Of Solar, Siderial, and Equal or Mean Time. Page 9S CONVERSATION IX. On the Moon. Of the Moon's Motion ; Phases of the Moon ; Eclipses of the Moon ; Eclipsesof Jupiter's Moons ; Of the Latitude and Longitude ; Of the. transits of the inferior Planets ; Of the Tides. Page 116 CONTENTS* Vll CONVERSATION X. HYDROSTATICS. On the Mechanical Properties of Fluids, Definition of a fluid ; Distinction between Fluids and Liquids ; of Non- Elastic Fluids, scarcely susceptible of Compression ; Of the Cohesion of Fluids ; Of their Gravitation ; Of their Equilibrium ; Of their Pressure ; Of Specific Gravity ; Of the Specific Gravity of Bodies heavier than Water ; Of those of the same weight as water ; Of those lighter than Water ; Of the Specific Gravity of Fluids. Page 126 CONVERSATION XL Of Springs, Fountains, ^c. Of the Ascent of Vapor and the Formation of Clouds ; Of the Formation and Fall of Rain, kc. ; Of the Formation of Springs ; Of Rivers as.d Lakes ; Of Fountains. Page 137 CONVERSATION XII. PNEUMATICS. On the Mechanical Properties of Air. Of the Spring or Elasticity of the Air ; Of the Weight of the Air ; Experiments with the Air Pump ; Of the Barometer ; Mode of Weighing Air; Specific Gravity of Air ; Of Pumps ; Description of the Sucking Pump; Description of the Forcing Pump. Page 14S CONVERSATION XIIL On Wind and Sound. Of Wind in General ; Of the Trade Wind; Of the Periodical Trade Winds; Of the Aerial Tides; Of Sound in General; Of Sonorous Bodies ; Of Musical Sounds ; Of Concord or Harmony, and Melody. Page 155 CONVERSATION XIV. On Optics. Of Luminous, Transparent, and Opaque Bodies; Of the Radiation of Light; Of Shadows ; Of the Reflection of Light ; Opaque Bodies seen only by Reflected Light ; Vision Explained ; Camera Obscura ; Image of Objects on the Retina. Page 166 viii CONTENTS. CONVERSATION XV. On the Angle of Vision^ and Reflection of Mirrors. Angle of Vision ; Reflection of Plain Mirrors ; Reflection of Convex Mirrors ; Reflection of Concave Mirrors, Page 178^ CONVERSATION XVI. On Refraction and Colors. Transmission of Light by Transparent Bodies ; Refraction ; Refraction of the Atmosphere; Refraction of a Lens; Refraction of the Prism; Of the Colors of Rays of Light ; Of the Colors of Bodies. Page 190 CONVERSATION XVIL OPTICS. On the Stimcture of the Eye^ and Optical Instruments. Description of the Eye ; Of the Image on the Retina ; Refraction of the Humors of the Eye; Of the Use of Spectacles ; Of the Single Micro- scope ; Of the Double tVTicroscope ; Of the Solar Microscope ; Magic Lanthorn ; Refracting Telebcope; Reflecting Telescope. Page 205 CON VEHSATION 1. ON GENERAL PROPERTIES OF BODIES. Introduction ; General Properties of Bodies ; Impenetr abil- ity ; Extension ; Figure ; Divisihilitij ; Inertia ; At- traction ; Attraction of Cohesion ; Density; liarity ; Heat ; Attraction of Gravitation. EMILY. I MUST request your assistance^ my dear Mrs. B. in a charge which I have lately undertaken ; it is that of instructing my youngest sister, a task, which I find proves more difficult^ than I had at first imagined. 1 can teach her the common routine of children's lessons tolerably well ; but she is such an inquis- itive little creature, that she is not satisfied without an expla- nation of every difficulty that occurs to her, and frequently asks me questions which I am at a loss to answer. This morning, for instance, when I had explained to her that the %vorld w^as round like a ball, instead of being fiat as she had supposed, and that it w^as surrounded by the air, she asked me what supported it. I told her that it required no support ; she then enquired why it did not fall as every thing else did ? This I confess perplexed me ; for I had myself been satisfied w^ith learning that the world floated in the air, without consid- ering how unnatural it was that so heavy a body, bearing the weight of all otli^r things, should be able to support itself. Mrs. B. 1 make no doubt, my dear, but that I shall be able to explain this difficulty to you ; but 1 believe that it would be almost impossible to render it intelligible to the comprehension of so young a child as your sister Sophia. You, who are now in your thirteenth year, may, I think, witli great propriety, learn not only the cause of this partictdar 2 ? 14 GENERAL PROPEKTIES OP BODIES. fact, but acquire a general knowledge of the laws by which the natural world is governed. Emily, Of all things it is what I should most like to learn ; but I was afraid it was too difficult a study even at my age. Mrs, B, Not when familiarly explained ; if you have patience to attend, I will most willingly give you all the infor- mation in my power. You may perhaps find the subject rather dry at first ; but if I succeed in explaining the laws of nature, so as to make you understand them, I am sure that you will derive not only instruction, but great amusement from that study. Emily, I make no doubt of it, Mrs. B. ; and pray begin by explaining why the earth requires no support ; for that is the point which just now most strongly excites my curiosity. I^irs, B, My dear Emily, if I am to attempt to give you a general idea of the laws of nature, which is no less than to introduce you to a knowledge of the science of natural philos- ophy, it will be necessary for us to proceed with some degree of regularity . I do not wish to confine you to the systematic order of a scientific treatise ; but if we were merely to exam- ine every vague question thai may chance to occur, our pro- gress would be but very slow. Let us, therefore, begin by taking a short survey of the general properties of bodies, some of which must necessarily be explained before I can attempt to make you understand why the earth requires no support. When I speak of bodies, I mean substances, of whatever nature^ whether solid or fluid ; and matte?' is the general term used to denote the substance, w hatever its nature be, of which the difierent bodies are composed. Thus, wood is the matter of which this table is made ; water is the matter with whicli this glass is filled, &c. Emily, I am very glad you have explained the meaning of the word matter, as it has corrected an erroneous concep- tion I had formed of it : I thought that it w^as applicable to solid bodies only. Mrs, B, There are certain properties which appear to be common to all bodies, and are hence called the essential properties of bodies ; these are. Impenetrability, Extension, Figure, Divisibility, Inertia, and Attraction, These are called the general properties of bodies, as we do not suppose any body to exist without them. By impenetrability y is meant the property which bodies GENERAL PROPERTIES OF BODIES. 15 have of occupying a certain space, so that, where one body is, another cannot be, without displacing the former ; for two bodies cannot exist in the same place at the same time. A liquid may be more easily removed than a solid body ; yet it is not the less substantial since it is as impossible for a liquid and a sohd to occupy the same space at the same time, as for two solid bodies to do so. For instance, if you put a spoon into a glass full of water, the water will flow over to make room for the spoon. Emily, I understand this perfectly. Liquids are in reality as substantial or as impenetrable as solid bodies, and they appear less so, only because they are more easily displaced. Mrs, B, The air is a fluid differing in its nature from liquids, but no less impenetrable. If I endeavour, to fill this phial by plunging it into this bason of water, the air, you see, rushes out of the phial in bubbles, in order to make way for the water, for the air and the water cannot exist together in the same space, any more than two hard bodies ; and if I reverse this goblet, and plunge it perpendicularly into the water, so that the air will not be able to escape, the water will no longer be able to fill the goblet. Emily, But it rises a considerable way into the glass. Mrii. B. Because the water compresses or squeezes the air into a small space in the upper part of the glass ; but, as long as it remains there, no other body can occupy the same place. Emily, A difficulty has just occurred to me, with regard to the impenetrability of solid bodies ; if a nail is driven into a piece of wood, it penetrates it, and both the wood and the nail occupy the same space that the wood alone did before ? Mrs, B, The nail penetrates between the particles of the wood, by forcing them to make way for it ; for you know that not a single atom of wood can remain in the space which the nail occupies ; and if the wood is not increased in size by the addition of the nail, it is because wood is a porous substance, like sponge, the particles of which may be compressed or squeezed closer together ; and it is thus that they make way for the nail. We may now proceed to the next general property of bodies, extension, A body which occupies a certain space must necessarily have extension ; that is to say, lengthy breadth^ and de])tli ; these are called the dimensions of extension ; can you form an idea of any body without them ? Emily, No ; certainly I cannot ; though these dimensions lO GENERAL PROPERTIES OF BODIES. must, of course, vary extremely in different bodies. The length, breadth, and depth, of a box, or of a thimble, are very different from those of a walking-stick, or of a hair. But is not height also a dimension of extension ? Mrs, B. Height and depth are the same dimension, con- sidered in different points of view ; if you measure a body, or a space, from the top to the bottom, you call it depth ; if from 1 he bottom upwards, you call it height ; thus the depth and height of a box are, in fact, the same thing. Emih/. Very true ; a moment's consideration would have enabled me to discover that ; and breadth and width are also the same dimension. Mrs, B, Yes ; the limits of extension constitute^,e?/^*e or shape. You conceive that a body having length, breadth, and depth, cannot be without form, either symmetrical or irregular ? Emily. Undoubtedly ; and this property admits of almost an infinite variety. ii/rs. B. Nature has assigned regular forms to her pro- ductions in general. The natural form of mineral substances is that of crystals, of which there is a great variety. Many of them are very beautiful, and no less remarkable by their transparency, or colour, than by the perfect regularity of their forn^Sj-as mav be seen in the various museums and collections of natural history. The vegetable and animal creation appears less symmetrical, but is still more diversified in figure than the mineral kingdom. Manufactured substances assume the vari- ous arbitrary forms which the art of man designs for them ; and an infinite number of irregular forms are produced by fractures, and by the dismemberment of the parts of bodies. Emily. Such as a piece of broken china or glass ? Mrs. B. Or the fragments of mineral bodies which are broken in being dug out of the earth, or decayed by the effect of torrents and other causes. The picturesque efiect of rock- scenery is in a great measure owing to accidental irregidari- ties of this kind. We may now proceed to divisihility ; that is to say, a susceptibility of being divided into an indefinite number of parts. Take any small quantity of matter, a grain of sand for instance, and cut it into two parts ; these two parts might be again divided, had we instruments sufficient!}'- fine for the purpose ; and if, by means of pounding, grinding, and other similar methods, we carry this division to the greatest possible extent, and reduce the body to its finest imaginable particles^ GENERAL PROPERTIES OF BODIES. . 1/ yet not one of the particles will be destroyed, and the body will continue to exist, though in this altered state. The melting of a solid body in a liquid affords a very strik- ing example of the extreme divisibility of matter ; when you sweeten a cup of tea, for instance, with what minuteness the sugar must be divided to be diffused throughout the whole of the liquid. Emily, And if you pour a few drops of red wine into a. glass of water, they immediately tinge the whole of the water, and must therefore be diffused throughout it. Mrs. B, Exactly so ; and the perfume of this lavender water will be almost as instantaneously diffused throughout the room, if I take out the stopper. Emily, But in this case it is only the perfume of the lav- ender, and not the water itself, that is diffused in the room ? Mrs, B, The odour or smell of a body is part of the body itself, and is produced by very minute particles or exhalations which escape from odoriferous bodies. It would be impossi- ble that you should smell the lavender water, if particles of it did not come in actual contact with your nose. Emily, But when I smell a flower, I see no vapour rise from it ; and yet I can perceive the smell at a considerable distance. Mrs, B, You could, I assure you, no more smell a flower, the odoriferous particles of which did not touch your nose, than you could taste a fruit, the flavoured particles of which did not come in contact with your tongue. Emily. That is wonderful indeed ; the particles then, which exhale from the flower and from the lavender water, are, I suppose, too small to be visible ? Mrs, B, Certainly : you may form some idea of their extreme minuteness from the immense number which must have escaped in order to perfume the whole room ; and yet there is no sensible diminution of the liquid in the phial. Emily. But the quantity must really be diminished ? Mrs. B. Undoubtedly ; and were you to leave the bottle open a sufficient length of time, the whole of the water would evaporate and disappear. But though so minutely subdivided as to be imperceptible to any of our senses, each particle would continue to exist ; for it is not within the power of man to destroy a single particle of matter : nor is there any reason to suppose that in nature an atom is ever annihilated, Emily, Yet, when a body is burnt to ashes, part of it, at a* 18 GENERAL PROPERTIES OF BODIES. leastj appears to be efTectiially destroyed ? Look how small is the residue of ashes beneath the grate, from all the coals which have been consumed within it. Mrs, B. That part of the coals, which you suppose to be destroyed, evaporates in the form of smoke and vapour, whilst the remainder is reduced to ashes. A body, in burning, undergoes no doubt very remarkable changes ; it is generally subdivided ; its form and colour altered ; its extension in- creased ; but the various parts, into which it has been sepa- rated by combustion, continue in existence, and retain all the essential properties of bodies. Emily, But that part of a burnt body which evaporates in smoke has no figure ; smoke, it is true, ascends in columns into the air, but it is soon so much diffused as to lose all form ; it becomes indeed invisible. Mrs. B. Invisible, I allow ; but we must not imagine that what we no longer see no longer exists. — Were every particle of matter that becomes invisible annihilated, the world itself would in the course of time be destroyed. The particles of smoke, when diffused in the air, continue still to be particles of matter, as well as when more closely united in the form of coals : they are really as substantial in the one state as in the other, and equally so when by their extreme subdivision they become invisible. No particle of matter is ever destroyed : this is a principle you must constantly remember. Every thing in nature decays and corrupts in the lapse of time. We die, and our bodies moulder to dust ; but not a single atom of them is lost ; they serve to nourish the earth, whence, while living, they drew their support. The next essential property of matter is called inertia ; this word expresses the resistance which inactive matter makes to a change of state. Bodies appear to be equally incapable of changing their actual state, whether it be of motion or of rest. You know that it requires force to put a body which is at rest in motion ; an exertion of strength is also requisite to stop a body which is already in motion. The resistance of the body to a change of state, in either case, is called its inertia, Emily, In playing at base-ball I am obliged to use all my strength to give a rapid motion to the ball ; and when I have to catch it, I am sure I feel the resistance it makes to being stopped. But if I did not catch it, it wodd soon fall to the ground and stop of itself. GENERAL PROPERTIES OF BODIES. 19 Mrs. B, Inert matter is as incapable of stopping of itself, as it is of putting itself into motion : when the ball ceases to move, therefore, it must be stopped by some other cause or povrer ; but as it is one with which you are yet unacquainted, we cannot at present investigate its effects. The last property which appears to be common to all bodies is attraction. All bodies consist of infinitely small particles of matter, each of which possesses the powder of attracting or draw^ing towards it, and uniting whh any other particle sufti- eiently near to be within the influence of its attraction ; but in minute particles this power extends to so very small a distance around them that its effect is not sensible, unless they are (or at least appear to be) in contact ; it then makes them stick or adhere together, and is hence called the attraction of cohesion. Without this power, solid bodies would fall in pieces or rather crumble to atoms. Emily, I am so much accustomed to see bodies firm and solid, that it never occurred to me that any power was requi- site to unite the particles of which they are composed. But the attraction of cohesion does not, I suppose, exist in liquids ; for the particles of liquids do not remain together so as to form a body, unless confined in a vessel ? Mrs, B, I beg your pardon ; it is the attraction of cohe- sion which holds this drop of Avater suspended at the end of my finger, and keeps the minute watery particles of which it is composed united. But as this power is stronger in proportion as th3 particles of bodies are more closely united, the cohesive attraction of solid bodies is much greater than that of fluids. The thmner and lighter a fluid is, the less is the cohesive attraction of its particles, because they are further apart ; and in elastic fluids, such as air, there is no cohesive attraction among the particles. Emily, That is very fortunate ; for it would be impossible to breathe the air in a solid mass ; or even in a liquid state. But is the air a body of the same nature as other bodies ? Mrs, B, Undoubtedly, in all essential properties. Emily, Yet you say that it does not possess one of the general properties of bodies — cohesive attraction ? Mrs, B, The particles of air are not destitute of the power of attraction, but they are too far distant from each other to be influenced by it ; and the utmost eflbrts of human art have proved ineffectual in the attempt to compress them, so as tp bring them within the sphere of each other's attraction, and make them cohere. 20 GKNERAL PROPERTIES OF BODIES. Emily. Ifso, howisit possible to prove that they are endowed with this power ? Mrs. B. The air is formed of particles precisely of the same nature as those which enter into the composition of liquid and solid bodies, in which state we have a proof of their attraction. Emily . It is then, I suppose, owing to the different degrees of attraction of different substances, that they are hard or soft ; and that liquids are thick or thin ? Mrs. B. Yes ; but you would express your meaning better by the term dcnsify^ which denotes the degree of closeness and compactness of the particles of a body : thus you may say, both of solids, and of liquids, that the stronger the cohe- sive attraction the greater is the density of the body. In phi- losophical language, density is said to be that property of bodies by which they contain a certain quantity of matter, under a certain bulk or magnitude. Rarity is the contrary of density ; it denotes the thinness and subtlety of bodies : thus you would say that mercury or quicksilver was a very dense fluid ; ether, a very rare one, &c. Caroline. But how are we to judge of the quantity of matter contained in a certian bulk ? Mrs. B. By the weight : under the same bulk bodies are said to be dense in proportion as they are heavy. Emily. Then we may say that metals are dense bodies, wood comparatively a rare one, &c. But, Mrs. B., when the particles of a body are so near as to attract each other, the effect of this power must increase as they are brought by it closer together ; so that one would suppose that the body would gradually augment in density, till it was impossible for its particles to be more closely united. Now, we know that this is not the case ; for soft bodies, such as cork, sponge, or butter, never become, in consequence of the increasing attrac- tion of their particles, as hard as iron ? Mrs. B. In such bodies as cork and sponge, the particles which come in contact are so few as to produce but a slight degree of cohesion : they are porous bodies, which, owing to the peculiar arrangement of their particles, abound with inters- tices which separate the particles ; and these vacancies are filled with air, the spring or elasticity of which prevents the closer union of the parts. But there is another fluid much more subtle than air, which pervades all bodies, this is heat. Heat insinuates itself more or less between the particles of all bodies, and forces them asunder ; you may therefore consider i OEXERAL PrvOPERTIES OF BODIES. 21 iit'ai and the attraction of cohesion^ as constantly acting in opposition to each other. Emily. The one endeavounng to rend a body to pieces, the other to keep its parts firmly united. Mrs. B. And it is this struggle between the contending tbrces of heat and attraction, which prevents the extreme degree of density which would result from the sole influence of the attraction of cohesion. Emihj. The more a body is heated then, the more its particles will be separated. Mrs. B. Certainly ; we find that bodies swell or dilate hy heat : this effect, is very sensible in butter, for instance, which expands by the application of heat, till at length the attraction of cohesion is so far diminished that the particles separate, and the butter becomes liquid. A similar effect is produced by heat on metals, and all bodies susceptible of being melted. Liquids, you know, are made to boil by the application of heat : the attraction of cohesion then yields entirely to the expansive powder ; the particles are totally separated and converted into steam or vapour. But the agency of heat is in no body more sensible than in air, which, dilates and contracts by its increase or diminution in a very remarkable degree.* Emily. The effects of heat appear to be one of the most interesting parts of natural philosophy. Mrs. B. That is true ; but heat is so intimately connected with chemistry, that you must allow me to defer the investi- gation of its properties till you become acquainted with that science. To return to its antagonist, the attraction of cohesion ; it is this power which restores to Vctpour its liquid form, which unites it into drops when it falls to the earth in a shower of rain, which gathers the dQ\Y into brilliant gems on the blades of grass. Emily. And I have often observed that after a shower, * The expansive power of heat proiluces some of the most iiuerestingf phenomena in nature. Tlie hoiling of liquids, is the immediate result of this power; and the operation, although simple, is peculiarly worthy of notice. As the numerous particles hecome expanded or rarified, they are continually rising to, and escaping from the surface, which occasions an agitation of the liquid, proportioned, in its violence, to the degree of heat operating on it. — And on exposing our hands or other limbs to the fire, the internal fluid becomes expanded, "which causes them to ap])ear swollen ; whereas, when exposed to the cold, the abstraction of the heat causes them to be compressed. '22 GENERAL PROPERTIES OF BODIES. 1 he water collects into large drops on the leaves of plants ; but I cannot say that I perfectly understand how the attrac- tion of cohesion produces this effect. Mrs, B, Rain does not fall from the clouds in the form of drops J but in that of mist or vapour, which is composed of very small watery particles ; these in their descent, mutually attract each other, and those that are sufficiently near in con- sequence unite and form a drop, and thus the mist is trans- formed into a shower. The dew also was originally in a state of vapour, but is, by the mutual attraction of the particles, formed into small globules on the blades of grass : in a similar manner the ram upon the leaf collects into large drops, v/hlch when they become too heavy for the leaf to support, fall to the ground. Emily. All this is wonderfully curious ! I am almost bewildered with surprise and admiration at the number of new ideas I have already acquired. Mrs, jB. Every step that you advance in the pursuit of natural science, will fill your mind with admiration and grat- itude towards its Divine Author. In the study of natural philosophy, we must consider ourselves as reading the book of nature, in which the bountiful goodness and wisdom of God is revealed to all mankind ; no study can then tend more to purify the heart, and raise it to a religious contemplation of the Divine perfections. There is another curious effect of the attraction of cohesion which I must point out to you. It enables liquids to rise above their level in capillary tubes ; these are tubes, the bores of which are so extremely small that liquids ascend within them, from the cohesive attraction between the particles of the liquid and the interior surface of the tube. Do you perceive the water rising above its level in this small glass tube, which I have immersed in a goblet full of water ? Emihj. Oh yes ; I see it slowly creeping up the tube, but now it is stationary ; will it rise no higher ? Mrs. I>. No ; because the cohesive attraction between the water and the internal surface of the tube is now balanced by the weight of the water within it : if the bore of the tube were narrower the water would rise higher ; and if you im- merse several tubes of bores of different sizes, you will see it rise to different heights in each of them. In making this experiment, you should colour the water w ith a little red wine, in order to render the effect more obvious. All porous substances, such as sponge, bread, linen, &c GENERAL PROPERTIES OF BODIES. 2S may be considered as collections of capillary tubes : if you dip one end of a lump of sugar into water the water will rise in it ; and wet it considerably above the surface of that into which you dip it. " EmiJt/. In making tea I have often observed that effectj without being able to account for it. Mrs, B. Now that you are acquainted with the attraction of cohesion, I must endeavor to explain to you that of Grav- itation, which is a modification of the same power ; the first is perceptible only in very minute particles, and at very small distances ; the other acts on the largest bodies, and extends to immense distances. Emily. You astonish me : surely you do not mean to say that large bodies attract each other. Mrs, B. Indeed I do ; let us take, for example, one of the largest bodies in nature, and observe whether it does not attract other bodies. What is it that occasions the fall of this book, when I no longer support it ? Emily, Can it be the attraction of the earth ? I thought that all bodies had a natural tendency to fall. Mrs, B, They have a natural tendency to fall, it is true ; but that tendency is produced entirely by the attraction of the earth ; the earth being so much larger than any body on its surface, forces every body, wliich is not supported, to fall upon it. Emily. If the tendency which bodies have to fall results from the earth's attractive power, the earth itself can have no such tendency, since it cannot attract itself, and therefore it requires no support to prevent it from frilling. Yet the idea that bodies do not fall of their own accord, but that they are drawn towards the earth by its attraction, is so new and strange to me, that I know not how to reconcile myself to it. Mrs, B, When you are accustomed to consider the fall of bodies as depending on this cause, it will appear to you as natural, and surely much more satisfactory, than if the cause of their tendency to fall were totally unknown. Thus you understand, that all matter is attractive, from the smallest particle to the largest mass ; and that bodies attract each other with a force proportional to the quantity of matter they contain. Emily, I do not perceive any difference between the attraction of cohesion and that of gravitation : is it not because every particle of matter is endowed with an attractive power, 24 f.i\St.AAL rKOPElLiii:.;^ Oi i;oDiJb.>. that large bodies^ consisting of a great number oi" paniciesj are so strongly attractive ? Mrs. B. True. There is, however, this difference be- tween the attraction of particles and that of masses, that the former is stronger than the latter, in proportion to the quan- tity of matter. Of this you have an instance in the attraction of capillary tubes, in which liquids ascend by the attraction of cohesion, in opposition to that of gravity. It is on this ac- count that it is necessary that the bore of the tube should be eitremely small ; for if the column of water within the tube is not very minute, the attraction would not be able either to raise or support its weight, in opposition to that of gravity. You may observe, also, that all solid bodies are enabled by the force of the cohesive attraction of their particles to resist that of gravity, which would otherwise disunite them, and bring them to a level with the ground, as it does in the case of liquids, the cohesive attraction of w^iich is not sufficient to enable it to resist the powTr of gravity.* Emily, And some solid bodies appear to be of this n^l- ture, as sand and powder for instance : there is no attraction of cohesion between their particles ? * The pov/er of gravitation is greatest at the surface of the earth, -v^'hence it decreases both upwards and downwards ; but not in the same propor- tion. The force of gravity upxvards is as the square of the distance from the centre. That is, gravity at the surface of the earth, which is about 4300 miles from the centre, is four times more powerful than it -would be at double the distance, or 8000 miles from tlie centre. Gravity and ■weight may be taken, in particular circumstances as synonymous terms. We say, a piece of lead weighs a pound, or sixteen ounces ; but if by any TAieans it could be carried 4000 miles above the surface of the earth, it vvould weigh only one fourth of a pound, or four ounces ; and if it could be transported to 8000 miles above the earth, which is three times the distance from the centre that the surface is, it would w^eigh only one ninth of a pound, or something less than two ounces. And it is demonstrated, that the force of gravity downwards decreases, as the distance from the surface increases, so that at one half the distance from the centre to the surface, the same weight, already described would -weigh only one hail of a pound, and so on. — Thus, a x>iece of metal weigh- uig, on the surface of the earth, one pound, will At The centre weigh - - - - 1000 miles from the centre 1-4 pound. 2000 1-2 5000 3-4 4000 1 8000 1-4 12,000 1-9 And at the distance of the moon from the earth, Avhich is 240,000 miles, it would weigh oidy the 3,600th part of a pound, because the distance is 60 times further from the centre of the earth than the surface-. GE^[ERAL PKOPERTIES OF BODIES. ' 25 Mrs, B. Every grain of powder or sand is composed of a great number of other more minute particles, firmly united by the attraction of cohesion ; but amongst the separate grains tliere is no sensible attraction, because they are not in suffi- ciently close contact. Emily, Yet they actually touch each other ? Mrs, B. The surface of bodies is in general so rough and uneven, that when in actual contact, they touch each other only by a few points. Thus, if I lay upon the table this book, the binding of which appears perfectly smooth, yet so few of the particles of its under surface come in contact with the table, that no sensible degree of cohesive attraction takes place ; for you see, that it does not stick, or cohere to the table, and I find no difficuhy in lifting it off. It is only when surfaces perfectly flat and well polished are placed in conta<:t, that tlie particles approach in sufficient number, and closely enough, to produce a sensible degree of cohesive attraction. Here are two hemispheres of polished metal, I press their flat surfaces together, having previously interposed a few drops of oil, to fill up every little porous vacancy. Now try to separate them. Emily, It requires an effort beyond my strength, though there are handles for the purpose of pulling them asunder. Is the firm adhesion of the two hemispheres, merely owing to the attraction of cohesion ? Mrs, B, There is no force more powerful, since it is by this that the particles of the hardest bodies are held together, it would require a weight of several pounds, to separate these hemispheres. Emily, In making a kaleidoscope, I recollect that the two plates of glass, which were to serve as mirrors, stuck so fast together, that I imagined some of the gum I had been using had by chance been interposed betv/een them ; but now I make no doubt but that it was their own natural cohesive attraction which produced this effect. Mrs B, Very probably it was so ; for plate-glass has an extremely smooth, flat surface, admitting of the contact of a great number of particles, between two plates, laid one over the other. Emily, But, Mrs. B., the cohesive attraction of some bodies is much greater than that of others ; thus glue, gum, and paste, cohere with singular tenacity. 3 Ju GENERAL PROPERTIES OF BODIES. Mrs, B. That is owing to the peculiar chemical properties of those bodies, independently of their cohesive attraction. There are some other kinds of modifications of attraction peculiar to certain bodies ; namely, that of magnetism, and of electricity ; but we shall confine our attention merely to the attraction of cohesion and of gravity ; the examination of the latter we shall resume at our next meeting. CONVERSAnON II. ON THE ATTRACTION OF GRAVITY. Attraction of Gramtation, continued ; of Weight ; Of the fall of Bodies ; Of the Resistance of the Air ; Of the Ascent of Light Bodies, EMILY. I HAVE related to my sister Caroline all that you have taught me of natural philosophy, and she has been so much delighted by it, that she hopes you will have the goodness to admit her to your lessons. Mrs. B, Very willingly ; but I did not think you had any taste for studies of this nature, Caroline ? Caroline, I confess, Mrs. B., that hitherto I had formed no very agreeable idea, either of philosophy, or philosophers ; but what Emily has told me, has excited my curiosity so much, that I shall be highly pleased if you will allow me to become one of your pupils. Mrs. B. I fear that I shall not find you so tractable a scholar as Emily ; I know that you are much biassed in favour of your own opinions. Caroline. Then you will have the greater merit in re- forming them, Mrs. B. ; and after all the wonders that Emily has related to me, I think I stand but little chance against you and your attractions. Mrs. B. You will, I doubt not, advance a number of objections ; but these I shall willingly admit, as they will be a means of elucidating the subject. Emily, do you recollect the names of the general properties of bodies ? Emily. Impenetrability, extension, figure, divisibility, inertia, and attraction. ^b OS THE ATTRACTION OF GRAVITY. Mrs. B, Very well. You must remember that these arf properties common to all bodies, and of which they cannot be deprived ; all other properties of bodies are called acci- ilental, because they depend on the relation or connection of one body to another. Caroluic, Yet surely, Mrs. B., there are other properties which are essential to bodies, besides those you have enumer- ated. Colour and weight, for instance, are common to ail bodies, and do not arise from their connexion with each other, but exist in the bodies themselves ; these, therefore, cannot be accidental qualities. Mrs, B. I beg your pardon ; these properties do not exist in bodies independently of their connection with other bodies. Caroline, What ! have bodies no weight ? Does not this table weigh heavier than this book ; and, if one thing weighs iieavier than another, must there not be such a thing as weight ? Mrs, B, No doubt : but this property does not appear to be essential to bodies ; it depends upon their connection with each other. AVeight is an effect of the power of attraction, without which the table and the book would have no weight whatever. Emily. I think I understand you : is it not the attraction of gravity, which makes bodies heavy ? Mrs, B. You are right. I told you that the attraction of gravity v/ as proportioned to the quantity of matter which bodies contained : now the earth consisting of a much greater quantity of matter than any body upon its surface, the force of its attraction must necessarily be greatest, and must draw every thing tovrards it ; in consequence of which, bodies that are unsupported fall to the ground, w^hilst those that arc sup- [)orted press upon the object which prevents their fall, v/ith a weight equal to the force with which they gravitate towards die earth. Caroline, The same cause then which occasions the fall of bodies, produces also their weight. It was very dull in me not to understand this before, as it is the natural and necessary consequence of attraction ; but the idea that bodies were not really heavy of themselves, appeared to me quite incompre- hensible. But, Mrs. B., if attraction is a property essential to matter, weight must be so likewise ; for how can one exist without the other ? Mrs, B, Suppose there were but one body existing in universal space, what would its weight be ? ON THE ATTRACTION OF GRAVITY* 29 Caroline. That would depend upon its size ; or, more accurately speaking, upon the quantity of matter it contained. Emily, No, no ; the body would have no weight whatever were its size ; because nothing would attract it. Am I not right, Mrs. B. ? Mrs. B. You are : you must allow, therefore, that it would be possible for attraction to exist without weight ; for each of the particles of which the body was composed, would possess the power of attraction ; but they could exert it only amongst themselves ; the whole mass, having nothing to attract, or to be attracted by, would have no weight. Caroline. I am now well satisfied that weight is not essential to the existence of bodies ; but what have you to object to colours, Mrs. B., you will not, I think, deny that they really exist in the bodies themselves. Mrs. B. When we come to treat of the subject of colours, I trust that I shall be able to convince you, that colours are likewise accidental qualities, quite distinct from the bodies to which they appear to belong. Caroline. Oh do pray explain it to us now, I am so very curious to know how that is possible. Mrs. B. Unless we proceed with some degree of order and method, you will in the end find yourself but little the wiser for all you learn. Let us therefore go on regularly, and make ourselves well acquainted with the general properties of bodies, before we proceed further. Emily. To return, then, to attraction, (which appears to me by far the most interesting of them, since it belongs equal- ly to all kinds of matter,) it must be mutual between two bodies ; and if so, when a stone falls to the earth, the earth should rise part of the way to meet the stone ? Mrs. B. Certainly ; but you must recollect that the force of attraction is proportioned to the quantity of matter which bodies contain, and if you consider the difference there is in that respect, between a stone and the earth, you will not be surprised that you do not perceive the earth rise to meet the stone ; for though it is true that a mutual attraction takes place between the earth and the stone, that of the latter is so very small in comparison to that of the former, as to render its effect insensible., Emily. But since attraction is proportioned to the quantity of matter which bodies contain, why do not the hills attract the houses aad churches towards them ? 30 ON THE ATTRACTION OP GRAVITY. Caroline, Heavens, Emily, what an idea ! Hov/ can the houses and churches be moved, when they are so firmly fixed in tlie ground ? Mrs. B. Emily's question is not absurd, and your answer, Caroline, is perfectly just ; but can you tell us why the houses und churches are so firmly fixed in the ground ? Caroline, I am afraid I have answered risfht by mere chance ; for I begin to suspect that bricklayers and carpenters itould give but little stability to their buildings, without the aid of attraction. Mrs, B, It is certainly the cohesive attraction between the bricks and the mortar, which enables them to build walls, and these are so strongly attracted by the earthy as to resist every other impulse ; otherwise they would necessarily move towards the hills and the mountains ; but the lesser force must yield to the greater. There are, however, som_e circumstances in which the attraction of a large body has sensibly counteracted that of the earth. If, whilst standing on the declivity of a mountain, you hold a plumb-line in your hand, the weight will not fall perpendicular to the earth, but incline a httle towards the mountain ; and this is owing to the lateral, or sideways attraction of the mountain, interfering with the perpendicular attraction, of the earth. Emily, But the size of a mountain is very trifling compared ro the whole earth ? Mrs, B, Attraction, you must recollect, diminishes w^itli distance ; and in the example of the plumb-line, the weight suspended is considerably nearer to the mountain than to the centre of the earth. Caroline, Pray, Mrs. B.,^ do the two scales of a balance hang parallel to each other ? Mrs, B, You mean, I suppose, in other words, to inquire Avhether two lines which are perpendicular to the earth, are parallel to each other ? I believe I guess the reason of your question ; but I wish you w ould endeavour to answ^er it without my assistance. Caroline, I was thinking that such lines must both tend by gravity to the same point, the centre of the earth ; now lines tending to the same point cannot be parallel, as parallel lines are always at an equal distance from each other, and would never meet. Mrs, B, Very well explained ; you see now the use of your knowledge of parallel lines : had you been ignorant of theio; TLATE I ON THE ATtRACTION OF GP.AVITr. Si properties, you couid not have drawn such a conclusion. This may enable you to form an idea of the great advantage to be derived even from a slight knowledge of geometry, in the study of natural philosophy ; and if, after I have made you acquain- ted with the first elements, you should be tempted to pursue the study, I would advise you to prepare yourselves by acqui- ring some knovvdedge of geometry. This science v/ould teach you that lines which fall perpendicular to the surface of a sphere cannot be parallel, because they would all meet, if prolonged to the centre of the sphere ; while lines that fail perpendicular to a plane or flat surface, are always parallel, because if prolonged, they would never meet. Emily, And yet a pair of scales, hanging perpendicular to the earth, appear parallel ? Mrs. B, Because the sphere is so large, and the scales consequently converge so little, that their inclination is not perceptible to our senses ; if we could construct a pair of scales whose beam would extend several degrees, their con- vergence would be very obvious ; but as this cannot be accom- plished, let us draw a small figure of the earth, and then we may make a pair of scales of the proportion we please, (fig. 1. plate I.) Caroline, This figure renders it very clear : then two bodies cannot fall to the earth in parallel lines ? Mrs. B. Never. Caroline, The reason that a heavy body falls quicker than a hght one, is, I suppose, because the earth attracts it more strongly ? Mrs. B, The earth, it is true, attracts a heavy body more than a light one ; but that would not make the one fall quicker than the other. Caroline, Yet, since it is attraction that occasions the fall of bodies, surely the more a body is attracted, the more rapid- ly it will fall. Besides, experience proves it to be so. Do we not every day see heavy bodies fall quickly, and light bodies slowly ? Emily. It strikes me, as it does Caroline, that as attraction is proportioned to the quantity of matter, the earth must necessarily attract a body which contains a great quantity more strongly, and therefore bring it to the ground sooner than one consisting of a smaller quantity. Mrs, B. You must consider, that if heavy bodies are attracted more strongly than Hght ones, they require more 32 ON THE ATTRACTION OF GRAVITY, attraction to malie thcin fall. Remember that bodies have no natural tendency to faH, any more than to rise, or to move laterally, and that they will not fall unless impelled by some force ; now this force must be proportioned to the quantity of matter it has to move : a body consisting of 1000 particles of matter, for instance, requires ten times as much attraction to bring it to the ground in the same space of time as a body consisting of only 100 particles. Caroline. I do not understand that ; for it seems to me, that the heavier a body is, the more easily and readily it falls. Emily, I think I nov/ comprehend it ; let me try if I can explain it to Caroline. Suppose that I draw^ towards me tv/o weighty bodies, the one of lOOlbs., the other of lOOOlbs.^ must I not exert ten times as much strength to draw the larger one to me, in the same space of time as is required for the smaller one ? And if the earth draws a body of lOOOlbs. weight to it in the same space of time that it draws a body of lOOlbs. does li not follow that it attracts the body of lOOOlbs. weight with ten times the force that it does that of lOOlbs. ? CaroUrie, I comprehend your reasoning perfectly ; but if it were so, the body of lOOOlbs. weight, and that of lOOlbs. Vv'ouldfall with the same rapidity ; and the consequence would be, that all bodies, whether light or heavy, being at an equal distance from the ground, would fall to it in the same space of time : now it is very evident that this conclusion is absurd ; experience cver}^ instant contradicts it ; observe how much sooner this book reaches the floor than this sheet of paper, when I let them drop together. Emily. That is an objection I cannot answer. I must refer it to you, Mrs. B. Mrs, B. I trust that v/e shall not find it insurmountable, \t is true that, according to the laws of attraction, all bodies- at an equal distance from the earth, should fall to it in the same space of time ; and this would actually take place if no ob- stacle intervened to impede their fall. But bodies fall through the air, and it is the resistance of the air which makes bodies of different density fall with different degrees of velocity. They must all force their way through the air, but dense heavy- bodies overcome this obstacle more easily than rarer and lighter ones> The resistance which the air opposes to the fall of bodies is proportioned to their surface, not to their weight ; the air b^ing inert^ cannot exert a greater foice to support the weight ON THE ATTE ACTION OF GRAVITY. SS of a cannon-ballj than it does to support the weight of a ball (of the same size) made of leather ; but the cannon-ball will overcome this resistance more easily^ and fall to the ground, consequently, quicker than the leather ball. Caroline. This is very clear, and solves the difficulty perfectly. The air offers the same resistance to a bit of lead and a bit of feather of the same size ; yet the one seems to meet with no obstruction in its fall, whilst the other is evidently resisted and supported for some time by the air. Emily, The larger the surface of a body, then, the more air it covers, and the greater is the resistance it meets with from it. Mrs. B. Certainly : observe the manner in which this sheet of paper falls ; it floats awhile in the air, and then gently descends to the ground. I will roll the same piece of paper up into a ball : it offers now but a small surface to the air, and encounters therefore but little resistance : see how much more rapidly it falls. The heaviest bodies may be made to float awhile in the air, by making the extent of their surface counterbalance their weight. Here is some gold, which is the most dense body we are acquainted with, but it has been beaten into a very thin leaf, and offers so great an extent of surface in proportion to its weight, that its fall, you see, is still more retarded by the resistance of the air than that of the sheet of paper. Caroline. That is very curious ; and it is, I suppose, upon the same principle that iron boats may be made to float on water ? But, Mrs. B., if the air is a real body, is it not also subjec- ted to the laws of gravity ? Mrs. B. Undoubtedly: Caroline. Then v/hy does it not, like all other bodies, fall to the ground ? Mi^s. B. On account of its spring or elasticity. The air is an elastic fluid ; a species of bodies, the peculiar property of which is to resume, after compression, their original dimen- sions ; and you must consider the air of which the atmosphere is composed as existing in a state of compression, for its par- ticles being drawn towards the earth by gravity, are brought closer together than they would otherwise be, but the spring or elasticity of the air by which it endeavours to resist com- pression gives it a constant tendency to expand itself, so as ro resimi^^ the dimensions it would naturally have, if not 34 ON THE ATTRACTION OF GRAVITY. under the influence of gravity. The air may therefore be said constantly to struggle with the power of gravity without being abie to overcome it. Gravity thus confines the air to the regions of our globe, w^hilst its elasticity prevents it from, falling like other bodies to the ground. Emily, The air then is I suppose, thicker, or I should rather say more dense, near the surface of the earth, than in the higher regions of the atmosphere ; for that jiart of the air which is nearer the surface of the earth must be most strongly attracted. Mrs, B, The diminution of the force of gravity, at so small a distance as that to which the atmosphere extends (compared with the size of the earth) is so inconsiderable as to be scarcely sensible ; but the pressure of the upper parts of the atmosphere on those beneath, renders the air near the surface of the earth much more dense than the upper regions. The pressm'e of the atmosphere has been compared to that of a pile of fleeces of wool, in which the lower fleeces are pressed together by the weight of those above ; these lie light and loose, in proportion as they approach the uppermost fleece, which receives no external pressure, and is confined merely by the force of its ow n gravity. Caroline, It has just occurred to me that there are some bodies w^hich do not gravita,te tov/a^'ds the earth. Smoke and. steam, for instance, rise instead of falling. Mrs, B, It is still gravity which produces their ascent ; at least, were that power destroyed, these bodies would not rise. Caroline, I shall be out of conceit with gravity, if it is so inconsistent in its operations. Mrs. B. There is no difficulty in reconciling this apparent inconsistency of eflect. The air near the earth is heavier than smoke, steam or other vapours ; it consequently not only suppoits these light bodies, but forces them to rise, till they reach a part of the atmosphere, the weight of w^hich is not greater than their own, and then they remain stationary. Look at this basin of water : why does the piece of paper which I throw into it float on the surface ? Emihj, Because, being lighter than the water, it is sup- ported by it. Mrs, B. And now that I pour more water into the basin, why does the paper rise ? Emihj, The water being heavier tlian the paper, gets beaeatli it, and obliges it to rise. 0>» THE ATTRACTION OF GRAVITY. Sb Mrs. B. In a similar manner are smoke and vapour forced upwards by the air ; but these bodies do not, hke the paper, ascend to the surface of the fluid, because, as we observed before, the air being thinner and lighter as it is more distant from the earth, vapours rise only till they attain a region of air of their own density. Smoke, indeed, ascends but a very little way ; it consists of minute particles of fuel carried up by a current of heated air from the fire below : heat, you recollect, expands all bodies ; it consequently rarefies air, and renders it lighter than the colder air of the atmosphere ; the heated air from the fire carries up with it vapour and small particles of the combustible materials which are burning in the fire. When ih.s current of hot air is cooled by mixing with that of the atmosphere, the minute particles of coal or other combustible fall, and it is this which produces the small black flakes which render the air and every thing in contact with it, in London, so dirty. Caroline. You must, however, allow me to make one more objection to the universal gravity of bodies ; which is the ascent of air balloons, the materials of which are un- doubtedly heavier than air ; how, therefore, can they be supported by it ? Mrs.B. I admit that the materials of which balloons are made are heavier than the air ; but the air with which they are filled is an elastic fluid, of a different nature from the atmospheric air, and considerably lighter ; so that on the whole, the balloon is lighter than the air which it displaces, and consequently will rise, on the same principle as smoke and vapour. Now, Emily, let me hear if you can explain how the gravity of bodies is modified by the effect of the air ? Emily. The air forces bodies which are lighter than itself to ascend ; those that are of an equal weight will remain stationary in it ; and those that are heavier will descend through it : but the air will have some effect on these last ; for if they are not much heavier, they will with difficulty overcome the resistance they meet with in passing through it, they will be borne up by it, and their fall will be more or less retarded. Mrs. B. Very well. Observe how slowly this light feather falls to the ground, while a heavier body, like this marble, overcomes the resistance which the air makes to its descent much more easily, and its fall is proportionally more rapid. I now throw a pebble into this tub of water ; it does S6 ON THE ATTRACTION OF GRAVITV. not reach the bottom near so soon as if there were no water in the tub, because it meets with resistance from the water. Suppose that we could empty the tub, not only of water, but of air also, the pebble would then fall quicker still, as it would in that case meet with no resistance at all to counteract its gravity. Thus you see that it is not the different degrees of gravity, but the resistance of the air, which prevents bodies of different weight from falling with equal velocities ; if the air did not bear up the feather, it would reach the ground as soon as the marble. Ccu'oline, I make no doubt that it is so ; and yet I do not feel quite satisfied. I wish there was any place void of air, in which the experiment could be made. Mrs, B. If that proof will satisfy your doubts, I can give it you. Here is a machine called an air pump^{^g, 2. pi. I.) by means of which the air may be expelled from any close vessel which is placed over this opening, through which the air is pumped out. Glasses of various shapes, usually called receivers, are employed for this purpose. We shall now exhaust the air from this tall receiver which is placed over the opening, and we shall find that bodies of whatever weight or size within it, will fall from the top to the bottom in the same space of time. Caroline. Oh, I shall be delighted with this experiment ; what a curious machine ! how can you put the two bodies of different weight within the glass, without admitting the air. Mrs, B, A guinea and a feather are already placed there for the purpose of the experiment : here is, you see, a contri- vance to fasten them in the upper part of the glass ; as soon as the air is pumped out, I shall turn this little screw, by which means the brass plates which support them will be inclined, and the two bodies will fall. — Now I believe I have pretty well exhausted the air. Caroline, Pray let me turn the screw. I declare, they both reached the bottom at the same instant ! Did you see, Emily, the feather appeared. as heavy as the guinea ? Emily, Exactly ; and fell just as quickly. How won- derful this is ! what a number of entertaining experiments might be made with this machine ! Mrs, B, No doubt there are a great variety ; but we shall reserve them to elucidate the subjects to which they relate : if I had not explained to you why the guinea and the feather ON THE ATTRACTION OF GRAVITY. 37 ieil with equal velocity, you would not have been so well pleased with the experiment. Emily, I should have been as much surprised, but not so much interested ; besides, experiments help to imprint on the memory the facts they are intended to illustrate ; it will be better therefore for us to restrain our curiosity, and wait for other experiments in their proper places. Caroline, Pray by what means is the air exhausted in this receiver. Mrs. B, You must learn something of mechanics in order to understand the construction of a pump. At our next meet- ing, therefore, I shall endeavour to make you acquainted with the laws of motion, as an introduction to that subject. CONVERSATION III. ON THE LAWS OF MOTION. On Motion ; Of the Inertia of Bodies ; Of Force to Produce Motion ; Direction of Motion ; Velocity, Absolute and Relative ; Uniform Motion ; Retarded Motion ; Accele- rated Motion ; Velocity of Falling Bodies ; Momentum ; Action and Re-action Equal ; Elasticity of Bodies ; Porosity of Bodies ; Refected Motion y- Angles of Inci- dence and Reflection, MRS. B. The science of mechanics is founded on the laws of motion ; it will, therefore, be necessary to make you acquainted with these laws before we examine the mechanical powers. Tell me, Caroline, what do you understand by the word motion ? Qftroline. 1 think I understand it perfectly, though I am at a loss to describe it. Motion is the act of moving about, going from one place to another, it is the contrary of remain- ing at rest. Mrs, B. Very well. Motion then consists in a change of place ; a body is in motion whenever it is changing its situa- tion with regard to a fixed point. Now since we have observed that one of the general pro- perties of bodies is Inertia, that is, an entire passiveness either with regard to motion or rest, it follows that a body cannot move without being put into motion ; the power which puts a body into motion is called force ; thus the stroke of the hammer is the force which drives the nail ; the pulling of the horse that which draws the carriage, &c. Force then is the cause which produces motion. Emily, And may we not say that gravity is the force which occasions the fall of bodies ? ON THE LAWS OP MOTION. S\) Mrs. B. Undoubtedly. I had given you the most familiar illustrations in order to render the explanation clear ; but since you seek for more scientific examples, you may say that cohesion is the force which binds the particles of bodies to- gether, and heat that which drives them asunder. The motion of a body acted upon by a single force is always in a straight line, in the direction in which it received the impulse. Caroline. That is very natural ; for as the body is inert, and can move only because it is impelled, it will move only in the direction in wiiich it is impelled. The degree of quick- ness wath which it moves, must, I suppose, also depend upon the degree of force with which it is impelled. Mrs. B. Yes ; the rate at which a body moves, or the shortness of the time which it takes to move from one place to another, is called its velocity ; and it is one of the laws of motion that the velocity of the moving body is proportional to the force by which it is put in motion. We must distin- guish between absolute and relative velocity. The velocity of a body is called absolute^ if we consider the motion of the body in space, without any reference to that of other bodies. When for instance a horse goes fifty miles in ten hours, his velocity is five miles an hour. The velocity of a body is termed relative^ when compared with that of another body which is itself in motion. For instance, if one man w^alks at the rate of a nnle an hour, and another at the rate of two miles an hour, the relative velocity of the latter is double that of the former, but the absolute velocity of the one is one mile, and that of the other two miles an hour. Emihj. Let me see if I understand it. The relative ve- locity of a body is the degree of rapidity of its motion compared \Y\t\i that of another body ; thus if one ship sail three times as far as another ship in the same space of time, the velocity of the former is equal to three times that of the latter. Mrs. B. The general rule may be expressed thus : the velocity of a body is measured by the space over w hich it moves, divided by the time which it employs in that motion : thus if you travel one hundred miles in twenty hours, what is your velocity in each hour ? Emlbf. I must divide the space, which is one hundred miles, by the time, which is twenty hours, and the answer w ill be five miles an hour. Then, Mrs. B., mav we not reverse 40 ON THE LAWS OF MOTION. this mle and say, that the time is equal to the space divided by the velocity ; since the space one hundred miles, divided by the velocity five miles, gives twenty hours for the time ? Mrs. B, Certainly ; and we may say also that space is equal to the velocity multiplied by the time. Can you tell me, Caroline, how many miles you will have travelled, if your velocity is three miles an hour and 3 ou travel six hours ? Caroline, Eighteen miles ; for the product of 3 multiplied by 6, is 18. Mrs. B. I suppose that you understand what is meant by the terms uniform^ accelerated and retarded motion. Emili/. I conceive uniform motion to be that of a body whose motion is regular, and at an equal rate throughout ; for instance, a horse that goes an equal number of miles every hour. But the hand of a w^atch is a much better example, as its motion is so regular as to indicate the time. M7^s. B. You have a right idea of uniform motion ; but it would be more correctly expressed by saying, that the motion of a body is uniform when it passes over equal spaces in equal times. Uniform motion is produced by a force having acted on a body once, and having ceased to act ; as for instance^ the stroke of a bat on a cricket ball. Caroline. But the motion of a cricket ball is not uniform ; its velocity gradually diminishes till it falls to the ground. Mrs. B. Recollect that the cricket ball is inert, and has no more power to stop than to put itself in motion ; if it falls, therefore, it must be stopped by some force superior to that hy wlTich it was projected, and v/hich destroys its motion. Caroline. And it is no doubt the force of gravity which 3ui:teracts and destroys that of projection ; but if there were ) such power as gravity, would the cricket ball never stop ? Mrs. B. If neither gi-avity nor any .other force, such a:> ilie resistance of the air, opposed its motion, the cricket ball, or even a stone thrown by the hand, would proceed onwards in a right line, and with an uniform velocity for ever. Caroline. You astonish me ! I thought that it was impos- sible to produce perpetual motion ? Mrs. B. Perpetual motion cannot be produced by art, because gravity ultimately destroys all motion that human powers can produce. Emily. But independently of tlie force of gravity, I can- not conceive that the little motion I am capable of giving to a stone would put it in motion for ev^r. ON THE LAWS OF MOTIOIS. 41 Mrs, B, The quantity of motion you communicate to the stone would not influence its duration ; if you threw it with httle force it would move slowly, for its velocity, you must remember, will be proportional to the force with which it is projected ; but if there is nothing to obstruct its passage, it will continue to move with the same velocity, and in the same direction as when you first projected it. Caroline. This appears to me quite incomprehensible ; we do not meet with a single instance of it in nature. Mrs, B, I beg your pardon. When you come to study the motion of the celestial bodies, you will find that nature abounds with examples of perpetual motion ; and that it conduces as much to the harmony of the system of the universe, as the prevalence of it would to the destruction of all comfort on our globe. The wisdom of Providence has therefore ordained insurmountable obstacles to perpetual motion here below, and though these obstacles often compel us to contend with great difficulties, yet there results from it that order, regularity and repose, so essential to the preservation of all the various beings of which this world is composed. Now can you tell me what is retarded motion ? Caroline, Retarded motion is that of a body which moves every moment slower and slower : thus when I am tired with walking fast, I slacken my pace ; or when a stone is thrown upwards, its velocity is gradually diminished by the power of gravity. Mrs, B, Retarded motion is produced by some force act- ing upon the body in a direction opposite to that which first put it in motion : you who are an animated being, endowed with power and will, may slacken your pace, or stop to rest when you are tired ; but inert matter is incapable of any feel- ing of fatigue, can never slacken its pace, and never stop, unless retarded or arrested in its course by some opposing force ; and as it is the laws of inert bodies which mechanics treats of, I prefer your illustration of the stone retarded in its ascent. Now, Emily, it is your turn ; what is accelerated motion ? Emili/, Accelerated motion, I suppose, takes place when the velocity of a body is increased ; if you had not objected to our giving such active bodies as ourselves as examples, I should say that my motion is accelerated if I change my pace from walking to running. I cannot think of any instance of 4* 42 ON THE LAWS OF MOTION. accelerated motion in inanimate bodies ; all motion of inert matter seems to be retarded by gravity. Mrs, B. Not in all cases ; for the power of gravitation sometimes produces accelerated motion ; for instance, a stone falling from a height moves with a regularly accelerated motion. Emihj. True ; because the nearer it approaches the earth, the more it is attracted by it. Mrs, B, You have mistaken the cause of its acceleration of motion ; for though it is true that the force of gravity increases as a body approaches the earth, the difference is so trifling at any small distance from its surface as not to be perceptible. Accelerated motion is produced when the force which put a body in motion continues to act upon it during its motion, so that its motion is continually increased. When a stone falls from a lieight, the impulse which it receives from gravity during the first instant of its fall, would be sufficient to bring it to the ground with a uniform velocity : for, as we have ob- served, a body having been once acted upon by a force, will continue to move w^itli a uniform velocity ; but the stone is not acted upon by gravity merely at the first instant of its fall, this power continues to impel it during the whole of its descent, and it is this continued impulse which accelerates its motion. Emily, I do not quite understand that. Mrs, B. Let us suppose that the instant after you have let fall a stone from a high tower, the force of gravity were anni- liilated, the body would nevertheless continue to move down- wards, for it v/ould have received a first impulse from gravity, and a body once put in motion will not stop unless it meets with some obstacle to impede its course ; in this case its velocity would be uniform, for though there w^ould be no obstacle to obstruct its descent, there would be no force to accelerate it. Emily, That is very clear. Mrs, B, Then you have only to add the power of gravity constantly acting on the stone during its descent, and it will not be difficult to understand that its motion will become accelerated, since the gravity which acts on the stone during the first instant of its descent, will continue in force every instant till it reaches the ground. Let us suppose that the impulse given by gravity to the stone during the first instant of its descent be equal to one^ the next instant we shall find ON THE LAWS OF MOTION. 46 that an additional impulse gives the stone an additional velo- city equal to one, so that the accumulated velocity is now equal to two ; the following instant another im.pulse increases the velocity to three, and so on till the stone reaches the ground. Caroline. Now I understand it ; the effects of preceding impulses must be added to the subsequent velocities. Blrs, B, Yes ; it has been ascertained both by experiment and calculations, which it would be too difficult for us to enter into, that heavj/ bodies descending from a height by the force of gravity, fall sixteen feet the first second of time, three times that distance in the next, five times in the third second, seven times in the fourth, and so on, regularly increasing their velo- cities according to the number of seconds during which tlie body has been falling. Emily. If you throw a stone perpendicularly upwards, is it not the same length of time ascending that it is descending. Mrs. B. Exactly ; in ascending, the velocity is diminished by the force of gravity ; in descending, it is accelerated by it. Caroline. I should then have imagined that it would have fallen quicker than it rose ? Mrs. B. You must recollect that the force with v>"hich it is projected must be taken into the account ; and that this force is overcome and destroyed by gravity before the body falls. Caroline. But the force of projection given to a stone in throwing it -upwards, cannot alwajs be equal to the force of gravity in bringing it down again, for the force of gravity is always the same, whilst the degree of impulse given to the stone is optional ; I may throw it up gently or v/itli violence. Mrs. B. If you throw it gently, it will not rise high ; per- haps only sixteen feet, in which case it will fall in one second of tiine. Now it is proved by experiment, tha,t an impulse requisite to project a body sixteen feet upwards, will make it ascend that height in one second ; here then the times of the ascent and descent are equal. But supposing it be required to throw a stone twice that height, the force must •be propor- tionally greater. You see then, that the impulse of projection in throwing a body upwards, is always equal to the action of the force ot gravity during its descent ; and that it is the greater or less distance to which the body rises, that makes these two forces balance each other. I must now explain to you what is meant by the momeninm 44 ON THE LAWS OF MOTION. of bodies. It is the force, or power, with which a body in motion, strikes against another body. The momentum of a bod}^ is composed of its quantity of matter^ muhiphed by its quantity of motion ; in other words, its weight and its velocity. Caroline, The quicker a body moves, the greater, no doubt, must be the force with which it would strike aeainst another body. Emily. Therefore a small body may have a greater mo- mentum than a large one, provided its velocity be sufficiently greater ; for instance, the momentum ol' an arrow shot from a bow, must be greater than a stone throvv^n by the hand. Caroline, We know also by experience, that the heavier a body is, the greater is its force ; it is not therefore difficult to understand, that the whole power or momentum of a body must be composed of these two properties : but I do not under- stand, why they should be muUipUed^ the one by the other ; I should have supposed fTiat the quantity of matter should have been added to the quantity of motion ? Mrs, B, It is found by experiment, tliat if the weight of a body is represented by the number 3, and its velocity also by 3, its momentum will be represented by 9 ; not 6, as would be the case, were these figures added, instead of being multi- plied together. I recommend it to you to be careful to remem- ber the definition of the momentum of bodies, as it is one of the most important points in mechanics ; you will find, that it is from opposing motion to matter, that machines derive their powers.* The re-action of bodies, is the next law of motion which I must explain to you. When a body in motion strikes against another body, it meets with resistance from it ; the resistance of the bod}^ at rest, will be equal to the blow struck by the body in motion ; or to express myself in philosophical language,. action and re-action will be equal, and in opposite directions. Caroline, Do you mean to say, that the action of the body which strikes, is returned with equal force by the body which receives the blow, * Tn comparing together the momenta of different bodies, we must be attentive to measure their Meighis and velocities, by the same denomina- tion of weights and of spaces, otherwise the results woald not agree. Thus if we estimate tlie weight of OJie body in on? ces, we must estimate the weight of the rest also in ounces, and not in pounds ; and in compu- ti'igthe velocities, in Tike manner, we should adhere to the same standai*(l of measure, both of space and of time; as for instance, the number of feet in one second, or of miles in one hour. ON THE LAWS OF MOTION. 45 Mrs, B. Exactly. Caroline. But if a man strikes another on the face with his fistj he surely does not receive as much pain by the re- action as he inflicts by the blow ? Mrs. B. iVo ; but this is simply owing to the knuckles having much less feeling than the face. Here are two ivory balls suspended by direads, (plate 1. fig. 3.) draw one of them, A, a little on one side, — now let it go ; — it strikes, you see, against the other ball B, and drives it off, to a distance equal to that through which the first ball fell ; but the motion of A is stopped, because when it struck B, it received in return a blov/ equal to that it gave, and its motion w^as consequently destroyed. Emily. I should have supposed that the motion of the ball A was destroyed, because it had communicated all its motion to B. Mrs. B. It is perfectly true, that when one body strikes against another, the quantity of motion communicated to the second body, is lost by the first ; but this loss proceeds from the action of the body which is struck. Here are six ivory balls hanging in a row, (fig. 4.) draw the first out of the perpendicular, and let it fall against the second. None of the balls appear to move, you see, except the last, which flies off as far as the first ball fell ; can you explain this ? Caroline. I believe so. When the first ball struck the second, it received a blow in return, w^hich destroyed its mo- tion ; the second ball, though it did not appear to move, must have struck against the third ; the re-action of which set it at rest ; the action of the third ball must have been destroyed by the re-action of the fourth, and so on till motion was commxunicated to the last ball, which, not being re-acted upon, ifies off. M/'5. B. Very v/ell explained. Objerve, that it is only when bodies are clastic, as these ivory balls are, that the stroke returned is equal to the stroke given. I w^ill show you !«the difference Vv'ith these tv/o balls of clay, (fig. 5.) which are not elastic ; when you raise one of these, D, out of the per- pendicular, and let it fall against the other, E, the re-action of the Ia,tter, on account of its not being elastic, is not sufficient to destroy the motion of the former ; only part of the motion of D will be communicated to E, and the tw^o balls will move 16 ON THE LAWS OF MOTION. on together to d and e, which is not to so great a distance as that tlirough whicli D fell. Observe how useful re-action is in nature. Birds in flying strike the air with their wings, and it is the re-action of the air which enables them to rise, or advance forwards ; re-action being always in a contrary direction to action. Caroline, I thought that birds might be lighter than the air, when their wings were expanded, and by that means enabled to fly. .' rs,B. \Vhen their wings are spread, they are better supported by the air, as they cover a greater extent of sur- face ; but the}' are still much too heavy to remain in that situ- ation, without continually flapping their wings, as you may have noticed, w hen biids hover over their nests : the force with which their wings strike against the air must equal the weight of their bodies, in order that the re-action of the air may be able to support that weight ; the bird will then re- main stationary. If the stroke of the wings, is greater than is required merely to support the bird, the re-action of the air will make it rise ; if it be less, it will gently descend ; and you may have observed the lark, sometimes remaining with its wings extended, but motionless : in this state it drops rapidly into its nest. Caroline, What a beautiful effect this is of the law of re-ac- tion ! But if flying is merely a mechanical operation, Mrs. B.^ why should we not construct wings, adapted to the size of our bodies, fasten them to our shoulders, move them with our arms, and soar into the air. Mrs, B, Such an experiment has been repeatedly at- tempted, but never with success ; and it is now considered ?.s totally impracticable. The muscular power of birds is greater in proportion to their weight than that of man ; were we therefore furnished with wings sufficiently large to enable us to fly, we should not have strength to put them in motion. In swimming, a similar action is produced on the water, as that on the air in flying ; and also in rov/ing ; you strike the water with the oars, in a direction opposite to that in tvhich the boat is required to move, and it is the re-action of the water on the oars which drives the boat along. Emily, You said, that it was in ehistlc bodies only, that re-action was equal to action ; pray what l^odles are elastic besides the air. ON THE LAWS OF MOTION. 47 Mrs, B. In speaking of the air, I think we defined elasti- city to be a property, by means of which bodies that are compressed returned to their former state. If I bend this , cane, as soon as I leave it at liberty it recovers its former ■ position; if I press my finger upon your arm, as soon as I remove it, the flesh, by virtue of its elasticity, rises and des- troys the impression I made. Of all bodies, the air is the most eminent for this property, and it has thence obtained the name of elastic fluid. Hard bodies are in the next degree elastic ; if two ivory, or metallic balls are struck together, the parts at which they touch will be flattened : but their elasticity will make them instantaneously resume their former shape. Caroline, But when two ivory balls strike against each other, as they constantly do on a biUiard table, no mark or impression is made by the stroke. Mrs. B. I beg your pardon ; but you cannot perceive any mark, because their elasticity instantly destroys all trace of It. Soft bodies, which easily retain impression, such as clay, wax, tallow, butter, &c. have very little elasticity ; but of all descriptions of bodies liquids are the least elastic. Emily, If sealing-wax were elastic, instead of retaining the impression of a seal, it would resume a smooth surface as soon as the weight of the seal was removed. But pray what is it that produces the elasticity of bodies ? Mrs, B. There is great diversity of opinion upon that point, and I cannot pretend to decide which approaches nearest to the truth. Elasticity implies susceptibility of com- pression, and the susceptibility of compression, depends upon the porosity of bodies, for were there no pores or spares between the particles of matter of which a body is composed, it could not be compressed. Caroline, That is to say, that if the particles of bodies were as close together as possible, they cuuld not be squeezed closer. j^ Emily, Bodies then, whose particles are most distant from each other, must be most susceptible of compression, and consequently most elastic ; and this you say is the case with air, which is perhaps the least dense of all bodies ? Mrs. B, You will not in general find this rule hold good, for liquids have scarcely any elasticity, whilst hard bodies are eminent for this property, though the latter are certainly of much greater density than the former ; elasticity implies, 48 uiN THE LA^^s of motion. therefore, not only a susceptibility of compression, but depends upon the power of resumincr its former state after compression. Caroline, But surely there can be no pores in ivory and metals, Mrs. B. ; how then can they be susceptible of compression ? Mrs, B, The pores of such bodies are invisible to the naked eye, but you must not thence conclude that they have none ; it is, on the contrary, well ascertained that gold, one of the most dense of all bodies, is extremely porous, and that these pores are sufficiently large to admit water when strongly compressed to pass through them. This was shown by a celebrated experiment made many years ago at Florence. Emily, If water can pass through gold, there must cer- tainly be pores or interstices which afford it a passage ; and if gold is so porous, what must other bodies be, which are so much less dense than gold ! Mrs, B. The chief difference in this respect is, I believe, that the pores in some bodies are larger than in others ; in cork, sponge, and bread, they form considerable cavities ; in wood and stone, when not polished, they are generally- perceptible to the naked eye ; whilst in ivorj-, metals, and all varnished and polished bodies, they cannot be discerned. To give you an idea of the extreme porosity of bodies, sir Isaac Newton conjectured that if the earth were so compressed as to be absolutely without pores, its dimensions might possibly not be more than a cubic inch. Caroline, What an idea ! Were we not indebted to sir Isaac Newton for the theory of attraction, I should be tempted to laugh at him for such a supposition. What insignitic^nt little creatures we should be ! Mrs, B, If our consequence arose from the size of our bodies we should indeed be but pigmies, but remember that the mind of Newton was not circumscribed by the dimensions of its envelope. Emily, It is, however, fortunate that heat keeps the pores of matter open and distended, and prevents the attraction of^ cohesion from squeezing us into a nut-shell. Mrs. B. Let us now return to the subject of re-action, on which we have some further observations to make. It is re-action, being contrary to action, which produces reflected Qnotion, If you throw a ball against the wall, it rebounds ; this return of the ball is owing to the re-action of the wall against which it struck, and is called reflected motion. I'i^f. 1. PLATE 71. ON THE LAWS OF MOTION. 49 Emily. And I now understand why balls filled with air rebound better than those stuffed with bran and wool, air being most susceptible of compression and most elastic, the re-action is more complete. Caroline, I have observed that when I throw a ball straight against the wall, it returns straight to my hand ; but if I throw it obliquely upwards, it rebounds still higher, and I catch it when it falls. Mrs, B, You should not say straight, but perpendicularly against the wall ; for straight, is a general term for lines in all directions which are neither curved nor bent, and is there- fore equally applicable to oblique or perpendicular lines. Caroline, I thought that perpendicularly meant either directly upwards or downwards. Mrs, B, In those directions lines are perpendicular to the earth. A perpendicular line has always a reference to some- thing towards which it is perpendicular ; that is to say, that it inclines neither to the one side nor the other, but makes an equal angle on every side. Do you understand what an angle is ? Caroline. Yes, I believe so : it is two lines meeting in a point. Mrs, B, Well then, let the line A B (plate II, fig. 1.) 1'epresent the floor of the room, and the line C D that in which you throw a ball against it ; the line C D you will observe, forms two angles with the line A B, and those two angles are equal. Emily, How can the angles be equal, while the lines which compose them are of unequal length ? Mrs, B, An angle is not measured by the length of the lines, but by their opening. Emily, Yet the longer the lines are, the greater is the opening between them. Mrs, B, Take a pair of compasses and draw a circle over these angles, making the angular point the centre. Emily, To what extent must I open the compasses ? Mrs. K You may draw the circle what size you please, provided that it cuts the lines of the angles we are to measure. All circles, of whatever dimensions, are supposed to be divided into 360 equal parts, called degrees ; the opening of an angle, being therefore a portion of a circle, must contain a certain number of degrees : the larger the angle, the greater 5 UN I UK LAWS OFMuTlO.N. the number of degrees, and the two angles are said to be equal when they contain an equal number of degrees. Emily, Now I understand it. As the dimensions of an angle depend upon the number of degrees contained between its lines, it is the opening and not the length of its lines, which determines the size of the angle. ^irs, B, Very well : now that you have a clear idea of the dimensions of angles, can you tell me how many degrees are contained in the two angles formed by one line falling perpendicular on another, as in the figure I have just drawn ? Emily, You must allow me to put one foot of the com- passes at the point of the angles, and draw a circle round them, and then I think I shall be able to answer your ques- tion : the two angles are together just equal to half a circle, they contain therefore 90 degrees each ; 90 degrees being a quarter of 360. Mrs, B, An rmgle of 90 degrees is called a right angle, and w^hen one line is perpendicular to another, it forms, you see (fig. 1.) a right angle on either side. Angles containing more than 90 degrees are called obtuse angles (fig. 2. ;) and those containing less than 90 degrees are called acute angles, (fig. 3.) Caroline, The angles of this square table are right angles, but those of the octagon table are obtuse angles ; and the an- gles of sharp-pointed instruments are acute angles. Mrs, B, Very well. To return now to your observation, that if a ball is thrown obliquely against the wall it will not rebound in the same direction ; tell me, have you ever played at billiards ? Caroline, Yes, frequently ; and I have observed that when I push the ball perpendicularly against the cushion it returns in the same direction ; but when I send it obliquely to the cushion, it rebounds obliquely, but on the opposite side ; the ball in this latter case describes an angle, the point of which is at the cushion. I have observed too, that the more obliquely the ball is struck against the cushion, the more obliquely it rebounds on the opposite side, so that a billiard player can calculate with great accuracy in what di- rection it will return. Mrs, B, Very well. This figure (fig. 4. plate II.) rep- resents a billiard table ; now if you draw a line A B from the point where the ball A strikes perpendicular to the cushion ; ox THE LAWS OP MOTION. 51 vou will find that it will divide the angle v/hich the ball de- scribes into two parts, or two angles ; the one will show the obliquity of the direction of the ball in its passage tow^ards the cushion, the other its obliquity in its passage back from the cushion. The first is called the angle of incidence^ the other the angle of reflection^ and these angles are always equal. Caroline. This then is the reason why, when I throw a ball obliquely against the wall, it rebounds in an opposite oblique direction, forming equal angles of incidence and of reflection. Mrs. B. Certainly ; and you will find that the more ob- liquely you throw the ball, the more obliquely it will rebound. We must now conclude : but I shall have some further observations to make upon the lav/s of motion, at our next meeting. CONVERSATION IV. ON COMPOUND MOTION. Compound Motion^ the Result of two Opposite Forces ; Of Circular Motion^ the Result of tivo Forces^ one of lohich confines the Body to a Fixed Point ; Centre of Motion^ the Point at Rest while the other Parts of the Body move round it ; Centre of Magnitude, the Middle of a Body ; Centripetal Force ^ that which confines a Body to a fixed Central Point ; Centrifugal Force, that which impels a Body to fly from the Centre ; Fall of Bodies in a Para- bola ; Centre of Gravity, the Centre of Weight, or point about which the Parts balance each other. MRS. B. I MUST now explain to you the nature ol' compound motion. Let us suppose a body to be struck by two equal forces in opposite directions^ how will it move ? Emily, If the directions of the forces are in exact oppo- sition to each other, I suppose the body would not move at all. M?'s, B, You are perfectly right ; but if the forces, instead of acting on the body in opposition, strike it in two directions inclined to each other, at an angle of ninety degrees, if the ball A (fig. 5, plate II.) be struck by equal forces at X and at Y, will it not move ? Emily, The force X would send it towards B, and the force Y towards C, and since these forces are equal, I do not know how the body can obey one impulse rather than the other, and yet I think the ball would move, because as the two forces do not act in direct opposition, they cannot entire- , ly destroy the effect of each other ON COMPOUND MOTION, 53 Mrs. B. Very true ; the ball will therefore follow the di- rection of neither of the forces, but will move in a line between them, and will reach D in the same space of time, that the force X v/ouldhave sent it to B, and the force Y would have sent it to C. Now if you drav/ two lines from D, to join B and C, you will form a square, and the oblique line which the body describes is called the diagonal of the square. Caroline. That is very clear, but supposing the two forces to be unequal, that the force X, for instance, be twice as great as the force Y ? Mrs. B. Then the force X would drive the ball twice as far as the force Y, consequently you must draw the line A B {fig. 6.,) twice as long as the line A C, the body will in this case move to D ; and if you draw lines from that point to B and C, you will find that the ball has moved in the diagonal of a rectangle. Emily. Allow me to put another case ? Suppose the two forces are unequal, but do not act on the ball in the direction of a right angle, but in that of an acute angle, what will result ? Mrs. B. Prolong the lines in the directions of the two forces, and \ou will soon discover which way the ball will be impelled ; it will move from A to D, in the diagonal of a^ parallelogram, (fig. 7.) Forces acting in the direction of lines forming an obtuse angle, will also produce motion in the diagonal of a parallelogram. For instance, if the body set out from B, instead of A, and was impelled by the forces X and Y, it would move in the dotted diagonal B C. We may now proceed to circular motion : this fs the result of two forces on a body, by one of which it is projected for- v/ard in a right line, whilst by the other it is confined to a fixed point. For instance, when I whirl this ball, which is fastened to my hand with a string, the ball moves in a circular direction ; because it is acted on by two forces, that which I give it which represents the force of projection, and that of the string which confines it to niy hand. If during its motion you were suddenly to cut the string, the ball would fly off* in a straight line ; being released from confinement to the fixed point, it would be acted on but by one force, and motion pro- duced by one force, you knov/, is always in a right line. Caroline. This is a little more difficult to comprehend than compound motion in straight lines. Mrs. B. You have seen a mop trundled, and have observ- 5* 54 ON eo3rpouN» motion^* ed, that the threads which compose the head of the mop fly from the centre ; but being confined to it at one end, they cannot part from it ; whilst the water they contain, being unconfined, is thrown off in straight lines. Emily. In the same way, the flyers of a windmill, when put in motion by the wind, would be driven straight forwards in a right line, were they not confined to a fixed point round which they are compelled to move. Mrs, B, Very well. And observe, that the point to which the motion of a small body, such as the ball with the stringy which may be considered as revolving in one plane, is confin- ed, becomes the centre of its motion. But when the bodies are not of a size or shape to allow of our considering every part of them as moving in the same plane, they in reality re- volve round a line, which line is called the axis of motion. In a top, for instojice, when spinning on its point, the axis is the line which passes through the middle of it, perpendicular- ly to the floor. Caroline. Tlie axle of the flyers of the windmil?, is then the axis of its motion ; but is the centre of motion always in the middle of a body ? Mrs. B. No, not always. The middle point of a body, is called its centre of magnitude, or position, that is the centre of its mass or bulk. Bodies have also another centre, called the centre of gravity, which I shall explain to you ; but at present we must confine ourselves to the axis of motion. This line you must observe remains at rest ; whilst all the other parts of the body move around it ; when you spin a top the axis is stationary vrhilst every other part is in motion round it. Caroline. But a top generally has a motion forwards, besides its spinning motion ; and then no point within it can be at rest ? Mrs. B. What I say of the axis of nwtion, relates only to circular motion ; that is to say, to motion round a line, and not to that which a body may have at the same time in any other direction. There is one circumstance in circular mo- tion, wliich you must carefully attend to ; which is, that the iiirther any part of a body is from the axis of motion, the greater is its velocity ; as you approach that line, the velocity of the parts gradually diminish till you reach the axis of motion, which is perfectly at rest. Cwroiine*, But^ if every part of the same body did not F^rehend3 the several levers you have described. Mrs, B, Yes, when in levers of tlie first kind, tlie fulcrum ^ is equally between the power and the weight, as in the bal- ance, the power must be greater than the weight, in order to move it ; for nothing can in this case be gained by velocity ; the two arms of the lever being equal, the velocity of their extremities must be so likewise. The balance is therefore of no assistance as a mechanical powder, but it is extremely useful to estimate the respective v>^eights of bodies. ON THE MECHANICAL POWERS. 65 But when (fig. 5.) the fulcrum F of a lever is not equally distant from the power and the weight, and that the power P acts at the extremity of the longest arm, it may be less than the weight W, its deficiency being compensated by its supe- rior velocity ; as we observed in the see-smv, Emily. Then when we want to lift a great weight, wt must fasten it to the shortest arm of a lever, and apply our strength to the longest arm ? Mrs, jB. If the case will admit of your putting the end of the lever under the weight, no fastening will be required ; as you will perceive by stirring the fire. Emily, Oh yes ! the poker is a lever of the first kind, the point where it rests against the bars of the grate whilst I am stirring the fire, is the fulcrum ; the short arm or resisting part of the lever is employed in lifting the weight, which is the coals, and my hand is the power applied to the longest arm, or acting part of the lever. Mrs, B, Let me hear, Caroline, whether you can equally well explain this instrument, which is composed of two levers, united in one common fulcrum. Caroline, A pair of scissors ! Mrs, B, You are surprised, but if you examine their construction, you will discover that it is the power of the lever that assists us in cutting with scissors. Caroline, Yes ; I now perceive that the point at which the two levers are screwed together, is the fulcrum ; the handles, to which the power of the fingers is applied, are the extremities of the acting part of the levers, and the cutting part of the scissors, are the resisting parts of the levers : therefore, the longer the handles and the shorter the points of the scissors, the more easily you cut with them. Emily, That I have often observed, for when I cut pasteboard or any hard substance, I always make use of that part of the scissors nearest the screw or rivet, and I now understand why it increases the power of cutting ; but I con- fess that I never should have discovered scissors to have been double levers ; and pray are not snufiers levers of a similar description ? Mrs, B, Yes, and most kinds of pincers ; the great power of which consists in the resisting part of the lever being very short in comparison of the acting part. Caroline,. And of what nature are the two other kinds of levers ? 6* 66 ON THE MECHANICAL POWERS. Mrs. B. In levers of the second kind, the weight, instead of being at one end, is situated between the power and the . fulcrum, (fig. 6.) Caroline, The weight and the fulcrum have here chang- ed places ; and what advantage is gained by this kind of lever ? Mrs, B. In moving it, the velocity of the power must necessarily be greater than that of the weight, as it is more distant from the centre of the motion. Have you ever seen your brother move a snow-ball by means of a strong stick, when it became too heavy for him to move without assistance ? Caroline, Oh yes ; and this was a lever of the second order (fig. 7-) ; the end of the stick, which he thrusts under the ball, and which rests on the ground, becomes the fulcrum ; the ball is the weight to be moved, and the power his hands applied to the other end of the lever. In this instance there is an immense difference in the length of the arms of the lever ; for the weight is almost close to the fulcrum. Mrs, B, And the advantage gained is proportional to this difference. Fishermen's boats are by levers of this description raised from the ground to be launched into the sea, by means of slippery pieces of board which are thrust under the keel. The most common example that we have of levers of the second kind is in the doors of our apartments. EniiJij, The hinges represent the fulcrum, our hands the power applied to the other end of the lever ; but where is the weight to be moved ? Mrs, B, The door is the weight, and it consequently occupies the whole of the space between the power and the fulcrum. Nutcrackers are double levers of this kind ; the hinge is the fulcrum, the nut the resistance, and the hands the power. In levers of the third kind (fig. 8,), the fulcrum is again at one of the extremities, the weight or resistance at the other, and it is now the power which is applied between the fulcrum and the resistance. Emily, The fulcrum, the weight, and the power, then, each in their turn, occupy some part of the middle of the lever between its extremities. But in this third kind of lever, the weight being farther from the centre of motion than the pow- er, the difficulty of raising it seems increased rather than diminished. Mrs, B. That is very true ; a lever of this kind is there- ox THE .MECHANICAL POWERS. 6/ fore never used, unless absolutely necessary, as is the case in lifting up a ladder perpendicularly in order to place it against the wall ; the man who raises it cannot place his hands on the upper part of the ladder, the power, therefore, is necessa- rily placed much nearer the fulcrum than the weight. Caroline. Yes, the hands are the power, the ground the fulcrum, and the upper part of the ladder the weight. Mrs. B. Nature employs this kind of lever in the struc- ture of the human frame. In lifting a weight with the hand, the lower part of the arm becomes a lever of the third kind ; the elbow^ is the fulcrum, the muscles of the fleshy part of the arm the power ; and as these are nearer to the elbow than the hand, it is necessary that their power should exceed the weight to be raised. Emily. Is it not surprising that nature should have fur- nished us with such disadvantageous levers ? Mrs. B. The disadvantage, in respect to power, is more than counterbalanced by the convenience resulting from this structure of the arm ^ and it is no doubt that which is best adapted to enable it to perform its various functions. We have dwelt so long on the lever, that we must reserve the examination of the other mechanical powers to our next interview. CONVERSATION V- CONTINUED. ON THE MECHANICAL POWERS. Of the Fitlley ; Of the Wheel and Axle ; Of the Inclined^ Plane: OftheJFedge; Of the Screw, MRS. B. The pulley is the second mechanical power we are to examine. You, both, I suppose, have seen a pulley ? Caroline. Yes, frequently : it is a circular and flat piece of wood or metal, with a string which runs in a groove round it ; by means of which, a weight may be pulled up ; thus pulleys are used for drawing up curtains. M7'S, B. Yes ; but in that instance the pulleys are fixed, and do not increase the power to raise the w^eights, as you will perceive by this figure, (pi. Y. fig. 1.) Observe that the fixed pulley is on the same principle as the lever of a pair of scales, in which the fulcrum F being in the centre of gravity, the power P and the weight W, are equally distant from it, and no advantage is gained. Emily, Certainly ; if P represents the power employed to raise the weight W, the power must be greater than the weight in order to move it. But of what use then are pulleys n mechanics ? Mrs, B, The next figure represents a pulley which is not fixed, (fig. 2.) and thus situated you will perceive that it affords us mechanical assistance. In order to raise the weight (W) one inch, P, the power, must draw the strings B and C one inch each ; the whole string is therefore shortened two inches, while the weight is raised only one. 4 ^^' PLATE V. F ■6 -6 m ©N THE MECHANICAL POWERS. 60 Emily. That I understand : if P drew the string but one inch, the weight would be raised only half an inch, because it would shorten the strings B and C half an inch each, and consequently the pulley with the weight attached to it, can be raised only half an inch. Caroline, I am ashamed of my stupidity ; but I confess that I do not understand this ; it appears to me that the weight would be raised as much as the string is shortened by the power. Mrs. B. I will endeavour to explain it more clearly. I fasten this string to a chair and draw it towards me ; I have now shortened the string, by the act of drawing it, one yard. Caroline. And the chair, as I supposed, has advanced one yard. Mrs. B. This exemplifies the nature of a single fixed pulley only. Now unfasten the string, and replace the chair where it stood before. In order to represent the moveable pulley, we must draw the chair forwards by putting the string round it ; one end of the string may be fastened to the leg of the table, and I shall draw the chair by the other end of the string. I have again shortened the string one yard ; how much has the chair advanced ? Caroline. I now understand it ; the chair represents the weight to which the moveable pulley is attached ; and it is very clear that the weight can be drawn only half the length you draw the string. I believe the circumstance that per- plexed me was, that I did not observe the difference that resuhs from the weight being attached to the pulley, instead of being fastened to the string, as is the case in the fixed pulley. Emily. But I do not 3^et understand the advantage of pulleys ; they seem to me to increase rather than diminish the difficulty of raising weights, since you must draw the string double the length that you raise the weight ; whilst with a single pulley, or without any pulley, the weight is raised as much as the string is shortened. Mrs. B. The advantage of a moveable pidley consists in dividing the difficulty ; we must draw, it is true, twice the length of the string, but then only half the strength is required tliat would be necessary to raise the weight without the assistance of a moveable pulley. Emily. So that the difficulty is overcome in the same manner as it would be, by dividing the weight into two equal parts, and raising them successively. 70 ON THE MECHANICAL POWERS. Mrs. B, Exactly. You must observe, that with a move- able pulley the velocity of the power is double that of the weight, since the power P (fig, 2.) moves two inches, whilst the weight W moves one inch ; therefore the power need not be more than half the weight to make their momentums equal. Caroline, Pulleys act then on the same principle as the lever, the deficiency of strength of the power being compen- sated by its superior velocity. Mr5. B. You will find, that all mechanical power is founded on the same principle. Emily. But may it not be objected to pulleys, that a longer time is required to raise a weight by their aid than without it ; for what you gain in powder you lose in time ? Mrs. B. That, my dear, is the fundamental law in me- chanics : it is the case with the lever as well as the pulley ; and you will find it to be so with all the other mechanical powers. Caroline. I do not see any advantage in the mechanical powers then, if what we gain by them one way is lost another. Mrs. B. Since we are not able to increase our natural strength, is not that science of wonderful utility, by means of whiv'^h we may reduce the resistance or weight of any body to the level of our strength ? This the mechanical powers enable us to accomplish, by dividing the resistance of a body into parts which we can successively overcome. It is true, as you observe, that it requires a sacrifice of time to attain this end, but you mast be sensible how very advantageously it is exchanged for power : the utmost exertion we can make adds but little to our natural strength, whilst we have a much more unlimited command of time. You can now understand, that the greater the number of pulleys connected by a string, the more easily the weight is raised, as the difficulty is divided among the number of strings, or rather of parts into which the string is divided by the pulleys. Several pulleys thus connec- ted, form what is called a system, or tackle of pulleys, (fig. 3.) You may have seen them suspended from cranes to raise goods into warehouses, and in ships to draw up the sails. Emily. But since a fixed pulley affords us no mechanical aid, why is it ever used ? Mrs. B. Though it does not increase our power, it is frequently useful for altering its direction. A single pulley enables us to draw up a curtain, by drawing down the string ON THE MECHANICAL POWERS. ?! connected with it ; and we should be much at a loss to accom- plish this simple operation without its assistance. Ca7'oline, There would certainly be some diificulty in ascending to the head of the curtain, in order to draw it up. Indeed. I now recollect having seen workmen raise small w^eights by this means, whicli seemed to answer a very useful purpose. Mrs. B. In shipping, both the advantages of an increase of power and a change of direction, by means of pulleys, are united : for the sails are raised up the masts by the sailors on deck, from the change of direction wdiich the pulley effects, and the labour is facilitated by the mechanical power of a combination of pulleys. Emily, But the pulleys on ship-board do not appear to me to be united in the manner you have shown us. Mrs. B. They are, I believe, generally connected as des- cribed in figure 4, both for nautical, and a variety of other purposes ; but in whatever manner pulleys are connected by a single string, the mechanical power is the same. The third mechanical powder is the wheel and axle. Let us suppose (plate V. fig. 5.) the weight W to be a bucket of water in a w ell, w^hich we raise by winding the rope, to which it is attached, round the axle ; if this be done without a wheel to turn the axle, no mechanical assistance is received. The axle without a wheel is as impotent as a single fixed pulley, or a lever, whose fulcrum is in the centre ; but add the wheel to the axle, and you will immediately find the bucket is raised with much less difficulty. The velocity of ^ the circumference of the wheel is as much greater than that of the axle, as it is further from the centre of motion : for the wheel describes a great circle in the same space of time that the axle describes a small one, therefore the powder is increas- ed in the same proportion as the circumference of the wheel is greater than that of the axle. If the velocity of the w heel is twelve times greater than that of the axle, a pow er nearly twelve times less than the weight of the bucket would be able to raise it. Emily. The axle acts the part of the shorter arm ol the lever, the wheel that of the longer arm. Caroline. In raising water there is commonly, I believe^ instead of a wheel attached to the axle, only a crooked handle, which answers the purpose of winding the rope round the axle, and thus raising the bucket. 72 eS THE MECHANICAL POWERS. Mrs. 7>. In this manner (fig. 6.) ; now if you observe the dotted circle which the handle describes in winding up the rope, you will perceive that the branch of the handle A, which is united to the axle, represents the spoke of a wheel, and answers the purpose of an entire wheel ; the other branch B affords no mechanical aid, merely serving as a han- dle to turn the wheel. Wheels are a very essential part to most machines : they are employed in various ways ; but, when fixed to the axle, their mechanical power is always the same ; that is, as the circumference of the wheel exceeds that of the axle, so much will the energy of its power be increased. Caroline. Then the larger the wh^el the greater must be its effect. ]\Irs. B. Certainly. If you have ever seen any consid- erable mills or manufactures, you must hive admired the immense wheel, the revolution of which puts the whole of the machinery into motion ; and though so great an effect is produced by it, a horse or two has sufficient power to turn it ; sometimes a stream of water is used for tliat purpose, but of late years, a steam-engine has been found both the most pow- erful and the most convenient mode of turning the wheel. Caroline, Do not the vanes of a windmill represent a wheel, Mrs. B. ? Mrs. B. Yes ; and in this instance we have the advan- tage of a gratuitous force, the wind, to turn the wheel. One of the great benefits resulting from the use of machinery is, that it gives us a sort of empire over the powers of nature, and enables us to make them perform the labour which would otherwise fall to the lot of man. When a current of wind, a stream of water, or the expansive force of steam, performs our task, we have only to superintend and regulate their operations. The fourth mechanical power is the inclined plane ; this is nothing more than a slope, or declivity, frequently used to facilitate the drawing up of weights. It is not difficult to understand, that a weight may much more easily be draw^n up a slope than it can be raised the same height perpendicu- larly. But in this, as well as the other mechanical powers, the facility is purchased by a loss of time (fig. 7.) ; for the weight, instead of moving directly from A to C, must move from B to C, and as the length of the plane is to its height, so much is the resistance of the weight diminished. ON THE MECHANICAL POWERS. io Emily, Yes ; for the resistance, instead of being confined to the short line A C, is spread over the long line B C. Mrs. B, The wedge, which is the next mechanical pow- er, is composed of two inclined planes (^fig. 8.) : you may have seen wood-cutters use it to cleave wood. The resistance consists in the cohesive attraction of the wood, or any other body which the wedge is employed to separate ; and the advantage gained by this power is in the proportion of half its width to its length ; for whik the wedge forces asunder the coherent particles of the wood to A and B, it penetrates downwards as far as C. Emily, The wedge, then, is rather a compound than a distinct mechanical power, since it is composed of two inclined planes. Mrs. B. It is so. All cutting instruments are constructed upon the principle of the inclined plane, or the wedge : those that have but one edge sloped, like the chisel, may be referred to the inclined plane ; whilst the axe, the hatchet, and the knife (when used to split asunder) are used as wedges. Caroline. But a knife cuts best when it is drawn across the substance it is to divide. We use it thus in cutting meat, we do not chop it to pieces. Mrs. B. The reason of this is, that the edge of a knife is really a very fine saw, and therefore acts best when used like that instrument. The screw, which is the last mechanical power, is more complicated than the others. You will see by this figure, (fig. 9.) that it is composed of two parts, the screw and the nut. The screw S is a cylinder, with a spiral protuberance coiled round it, called the thread ; the nut N is perforated to contain the screw, and the inside of the nut has a spiral groove made to fit the spiral thread of the screw. Caroline. It is just like this little box, the lid of which screws on the box as you have described : but what is this handle which projects from the nut ? Mrs, B. It is a lever, which is attached to the nut, without which the screw is never used as a mechanical power : the nut with a lever L attached to it, is commonly called a winch. The power of the screw, complicated as it appears, is refera- ble to one of the most simple of the mechanical powers ; which of them do you think it is ? Caroline. In appearance, it most resembles the wheel and axle. 7 74 ON THE MECHANICAL POWERS, Mrs. B. The lever, it is true, has the effect of a wheel, as it is the means by which you wind the nut round ; but the lever is not considered as composing a part of the screw, though it is true, that it is necessarily attached to it. But observe, that the lever, considered as a wheel, is not fastened to the axle or screw, but moves round it, and in so doing, the nut either rises or descends, according to the way in which you turn it. Emily, The spiral thread of the screw resembles, I think, an inclined plane : it is a sort of slope, by means of which the nut ascends more easily than it would do if raised perpen- dicularly ; and it serves to support it when at rest. Mrs, B. Very well : if you cut a slip of paper in the form of an inclined plane, and wind it round your pencil, which will represent the cylinder, you will find that it makes a spiral line, corresponding to the spiral protuberance of the screw, (fig. 10.) Emily, Very true; the nut then ascends an inclined plane, but ascends it in a spiral, instead of a straight line ; the closer the thread of the screw, the more easy the ascent ; it is like having shallow, instead of steep steps to ascend. Mrs. B, Yes, excepting that the nut takes no steps, it gradually winds up or down ; then observe, that the closer the threads of the screw, the greater the number of revolu- tions the winch must make ; so that we return to the old principle, — what is saved in power is lost in time. Emily. Cannot the power of the screw be increased also, by lengthening the lever attached to the nut ? Mrs. B, Certainly. The screw, with the addition of the lever, forms a very powerful machine, employed either for compression or to raise heavy weights. It is used by book-binders, to press the leaves of books together ; it is used also in cider and wine presses, in coining, and for a variety of other purposes. All machines are composed of one or more of these six mechanical powers we have examined : I have but one more remark to make to you relative to them, which is, that friction in a considerable degree diminishes their force, allowance must therefore always be made for it in the construction of machinery. Caroline. By friction, do you mean one part of the ma- chine rubbing against another part contiguous to it. Mrs. B. Yes ; friction is the resistance which bodies ON THE MECHANICAL POWERS. 75 meet with in rubbing against each other ; there is no such thing as perfect smoothness or evenness in nature : poHshed metals, though they wear that appearance, more than any other bodies, are far from really possessing it ; and their inequalities may frequently be perceived through a good magnifying glass. When, therefore, the surfaces of the two bodies come into contact, the prominent parts of the one will often fall into the hollow parts of the other, and occasion more or less resistance to motion. Caroline. But if a machine is made of polished metal, as a watch, for instance, the friction must be very trifling ? Mrs. B. In proportion as the surfaces of bodies are well polished, the friction is doubtless diminished ; but it is always considerable, and it is usually computed to destroy one- third of the power of a machine. Oil or grease is used to lessen friction ; it acts as a polish by filling up the cavities of the rubbing surfaces, and thus making them slide more easily over each other. Caroline. Is it for this reason that wheels are greased, and the locks and hinges of doors oiled ? Mrs. B. Yes ; in these instances the contact of the rub- bing surfaces is so close, and the rubbing so continual, that notwithstanding their being polished and oiled, a considera- ble degree of friction is produced. There are two kinds of friction ; the one occasioned by the sliding of the flat surface of a body, the other by the rolling of a circular body ; the friction resulting from the first is much the most considerable, for great force is required to enable the sliding body to overcome the resistance which the asperities of the surfaces in contact oppose to its motion, and it must be either lifted over, or break through them ; whilst, in the other kind of friction, the rough parts roll over each other with comparative facility ; hence it is, that wheels are often used for the sole purpose of diminishing the resist- ance of friction. Emily. This is one of the advantages of carriage-wheels ; is it not ? Mrs. B. Yes ; and the larger the circumference of the wheel the more readily it can overcome any considerable obstacles, such as stones, or inequalities in the road. When, in descending a steep hill, we fasten one of the wheels, we decrease the velocity of the carriage, by increasing the friction. 76 ON THE MECHANICAL POWERS. Caroline, That is to say, by converting the rolling fric- tion into the dragging friction. And when you had casters put to the legs of the table, in order to move it more easily, you changed the dragging into the rolling friction. Mrs, B, There is another circumstance which we have already noticed, as diminishing the motion of bodies, and which greatly affects the power of machines. This is the resistance of the medium in which a machine is worked. All fluids, whether of the nature of air, or of water, are called mediums ; and their resistance is proportioned to their den- sity ; for the more matter a body contains, the greater the resistance it will oppose to the motion of another body striking against it. Emily, It would then be much more difficult to work a machine under water than in the air ? Mrs, B, Certainly, if a machine could be worked in vacuOy and without friction, it would be perfect ; but this is unattainable ; a considerable reduction of power must there- fore be allowed for the resistance of the air. We shall here conclude our observations on the mechan- ical powers. At our next meeting I shall endeavour to give you an explanation of the motion of the heavenly bodies. CONVERSATION VI. CAUSES OF THE EARTH'S ANNUAL MOTION. Of the Planets^ and their Motion ; Of the Diurnal Motion of the Earth and Planets, CAROLINE. I AM come to you to-day quite elated with the spirit of opposition, Mrs. B. ; for I have discovered such a powerful objection to your theory of attraction, that I doubt whether even your conjuror Newton, with his magic wand of attrac- tion, will be able to dispel it. Mrs, B. Well, my dear, pray what is this weighty objec- tion ? Caroline. You say that bodies attract in proportion to the quantity of matter they contain, now we all know the sun to be much larger than the earth : why, therefore, does it not attract the earth ; you will not, I suppose, pretend to say that we are falling towards the sun ? Emily, However plausible your objection appears, Caro- line, I think you place too much reliance upon it : when any one has given such convincing proofs of sagacity and wisdom as Sir Isaac Newton, when we find that his opinions are uni- rersally received and adopted, is it to be expected that any objection we can advance should overturn them ? Caroline, Yet I confess that I am not inclined to yield implicit faith even to opinions of the great Newton : for what purpose are we endowed with reason, if we are denied the privilege of making use of it, by judging for ourselves ? MrSy B, It is reason itself which teaches us, that when we, novices in science, start objections to theories established by men of acknowledged wisdom, we should be diffident rather of our own than of their opinion. I am far from wish- 7* 78 CAUSES OF THK ing to lay the least restraint on your questions ; you cannot be belter convinced of the truth of a system, tlian by finding that it resists all your attacks, but I would advise you not to advance your objections with so much confidence, in order that the discovery of their fallacy may be attended with less mortification. In answer to that you have just proposed, I can only say, that the earth really is attracted by the sun. Caj'oline. Take care at least that we are not consumed by him, Mrs. B. Mrs. B, We are in no danger ; but our magician Newton, as you are pleased to call him, cannot extricate himself from this difficulty without the aid of some cabalistical figures, which I must draw for him. Let us suppose the earth, at its creation, to have been projected forwards into universal space : we know that if no obstacle impeded its course it would proceed in the same direction, and with a uniform velocity for ever. In fig. 1 plate 6., A represents the earth, and S the sun. We shall suppose the earth to be arrived at the point in which it is represented in the figure, having a velocity which would carry it on to B in the space of one month ; whilst the sun's attrac- tion would bring it to C in the same space of time. Observe that the two forces of projection and attraction do not act in opposition, but perpendicularly, or at a right angle to each other. Can you tell me now, how the earth will move ? Emily. I recollect your teaching us that a body acted upon by two forces perpendicular to each other would move in the diagonal of a parallelogram ; if, tlierefore, I complete the parallelogram by drawing the lines C D, B D, the earth will move in the diagonal A D. Mrs. B. A ball struck by two forces acting perpendicu- larly to each other, it is true, moves in the diagonal of a parallelogram ; but you must observe that the force of attrac- tion is continually acting upon our terrestrial ball, and produ- cing an incessant deviation from its course in a right line, which converts it into that of a curve line ; every point of w^hich may be considered as constituting the diagonal of an infinitely small parallelogram. Let us detain the earth a moment at the point D, and con- sider how it will be aflected by the combined action of the two forces in its new situation. It still retains its tendency to fly off in a straight line ; but a straight line would now carry it PIATE U ^' ^4^ ^' earth's annual motion. 79 away to F, whilst the sun would attract it in the direction D S ; how then will it proceed ? Emily. It will go on in a curve line, in a direction between that of the two forces. Mrs, B. In order to know exactly what course the earth will follow, draw another parallelogram similar to the first, in which the line D F describes the force of projection, and the line D S, that of attraction ; and you will find that the earth will proceed in the curve line D G. Caroline, You must now allow me to draw a parallelo- gram, Mrs. B. Let me consider in w^hat direction will the force of projection now impel the earth. Mrs, B. First draw a line from the earth to the sun representing the force of attraction ; then describe the force of projection at a right angle to it. Caroline, The earth will then move in the curve G I, of the parallelogram G H I K. Mrs, B, You recollect that a body acted upon by two forces, moves through a diagonal in the same time that it would have moved through one of the sides of the parallelo- gram, were it acted upon by one force only. The earth has passed through the diagonals of these three parallelograms in the space of three months, and has performed one quarter of a circle ; and on the same principle it will go on till it has completed the whole of the circle. It will then recommence a course, which it has pursued ever since it first issued from the hand of its Creator, and which there is every reason to suppose it will continue to follow, as long as it remains in existence. Emily, What a grand and beautiful effect resulting from so simple a cause ! Caroline, It affords an example, on a magnificent scale, of the circular motion which you taught us in mechanics. The attraction of the sun is the centripetal force, which con- fines the earth to a centre ; and the impulse of projection the centrifugal force, which impels the earth to quit the sun and fly off in a tangent. Mrs, B, Exactly so. A simple mode of illustrating the effect of these combined forces on the earth, is to cut a slip of card in the form of a right angle, (fig. 2. plate YI.) to describe a small circle at the angular point representing the earth, and to fasten the extremity of one of the legs of the angle to a fixed point, which we shall consider as the sun. Thus situa- 30 CAUSES OF THE tedy the angle will represent both the centrifugal and centri- petal forces ; and if you draw it round the fixed point, you will see how the direction of the centrifugal force varies, constantly forming a tangent to the circle in which the earth moves, as it is constantly at a right angle with the centripetal force. Emihj, The earth, then, gravitates towards the sun with- out the slightest danger either of approaching nearer or receding further from it. How admirable this is contrived ! If the two forces which produce this circular motion had not been so accurately adjusted, one would ultimately have pre- vailed over the other, and we should either have approached so near the sun as to have been burnt, or have receded so far from it as to have been frozen. Mrs. B, What will you say, my dear, when I tell you that these two forces are not, in fact, so proportioned as to produce circular motion in the earth ? Caroline. You must explain to us, at least, in what man- ner we avoid the threatened destruction. Mrs. B. Let us suppose that when the earth is at A, (fig. 3.) its projectile force should not have given it a velocity sufficient to counterbalance that of gravity, so as to enable these powers conjointly to carry it round the sun in a circle ; the earth, instead of describing the line A C, as in the former figure, will approach nearer the sun in the line A B. Caroline. Under these circumstances, I see not what is tc prevent our approaching nearer and nearer the sun till we fall into it : for its attraction increases as we advance towards it, and produces an accelerated velocity in the earth which increases the danger. Mrs. B. And there is yet another danger, of which you are not aware. Observe, that as the earth approaches the sun, the direction of its projectile force is no longer perpendicular to that of attraction, but inclines more nearly to it. When the earth reaches that part of its orbit at B, the force of pro- jection would carry it to D, which brings it nearer the sun instead of bearing it away from it. Emily. If, then, we are driven by one power and drawn by the other to this centre of destruction, how is it possible for us to escape ? Mrs. B. A little patience, and you will find that we are not without resource. The earth continues approaching tlie sun with a uniformly increasing accelerated motion, till it earth's annual 3I0TI0N. 81 ueaches the point E ; in what direction will the projectile ibrce now impel it ? Emily, In the direction E F. Here then the two forces act perpendicularly to each other, and the earth is situated just as it was in the preceding figure ; therefore, from this point, it should revolve round the sun in a circle. Mrs, B. No, all the circumstances do not agree. In mo- tion round a centre, 3^ou recollect that the centrifugal force increases with the velocity of the body, or, in other words, the quicker it moves the stronger is its tendency to fly oil in a right line. When the earth, therefore, arrives at E, its accelerated motion will have so far increased its velocity, and consequently its centrifugal force, that the latter will prevail over the force of attraction, and drag the earth away from the sun till it reaches G. Caroline, It is thus, then, that vre escape from the dan- gerous vicinity of the sun ; and in proportion as we recede from it, the force of its attraction, and, consequently, the velo- city of the earth's motion are diminished. Mrs, B, Yes. From G the direction of projection is towards H, that of attraction towards S, and the earth pro- ceeds between them with a uniformly retarded motion, till it has completed its revolution. Thus you see, that the earth travels round the sun, not in a circle, but an ellipsis, of which the sun occupies one of the foci ; and that in its course the earth alternately approaches, and recedes from it, without any danger of being either swallowed up, or being entirely carried away from it. Caroline, And I observe, that what I apprehended to be a dangerous irregularity, is the means by which the most per- fect order and harmony are produced ! Emily, The earth travels, then, at a very unequal rate, its velocity being accelerated as it approaches the sun, and retarded as it recedes from it. Mrs, B, It is mathematically demonstrable, that, in mov- ing round a point towards which it is attracted, a body passes over equal areas in equal times. The whole of the space contained Vv'ithin the earth's orbit, is, in fig. 4., divided into a number of areas, or spaces, 1, 2, 3, 4, &c. all of which are of equal dimensions, though of very different forms ; some of them, you see, are long and narrow, others broad and short : but they each of them contain an equal quantity of space. An imaginary line drawn from the centre of the earth to that ^2 CAUSES OF THE of the sun, and keeping pace with the earth in its revolution, passes over equal areas in equal times ; that is to say, if it is a month going from A to B, it will be a month going from B to C, and another from C to E, and so on. Caroline. What long journeys the earth has to perform in the course of a month, in one part of her orbit, and how short they are in the other part ! Mrs, B. The inequality is not so considerable as appears in this figure ; for the earth's orbit is not so eccentric as it is there described ; and, in reality, differs but litde from a cir- cle ; that part of the earth's orbit nearest the sun is called its perihelion, that part most distant from the sun its aphelion ; and the earth is above three millions of miles nearer the sun at its perihelion than at its aphelion. Emily. I think I can trace a consequence from these dif- ferent situations of the earth ; is it not the cause of summer and winter ? Mrs. B. On the contrary ; during the height of summer, the earth is in that part of its orbit which is most distant from the sun, and it is during the severity of winter, that it ap- proaches nearest to it. Emily. That is very extraordinary ; and how then do you account for the heat being greatest, when we are most distant from the sun ? Mrs. B. The difference of the earth's distance from the sun in summer and winter, when compared with its total distance from the sun, is but ipconsiderable. The earth, it is true, is above three millions of miles nearer the sun in winter than in summer ; but that distance, however great it at first appears, sinks into insignificance in comparison of 95 mil- lions of miles, which is our mean distance from the sun. The change of temperature, arising from this difference, would scarcely be sensible ; were it not completely overpowered by other causes which produce the variations of the seasons ; but these I shall defer explaining, till we have made some further observations on the heavenly bodies. Caroline. And should not the sun appear smaller in sum- mer, when it is so much further from us ? Mrs. B. It actually does when accurately measured ; but the apparent difference in size, is, I believe, not perceptible to the naked eye. Emily, Then, since the earth moves with greatest velo- city in that part of its orbit nearest the sun, it must have EARTH'S ANNUAL MOTION. 83 rdmpleted its journey through one half of its orbit in a shortev time than the other half ? Mrs. B. Yes, it is about seven days longer performing the summer-half of its orbit, than the winter-half. The revolution of all the planets round the sun is the result of the same causes, and is performed in the same manner as that of the earth. Caroline. Pray what are the planets ? Mrs. B, They are those celestial bodies, which revolve iike our earth about the sun ; they are supposed to resemble the earth also in many other respects ; and we are led by analogy to suppose them to be inhabited worlds. Caroline. I have heard so ; but do you not think such an opinion too great a stretch of the imagination ? Mrs. B. Some of the planets are proved to be larger than the earth ; it is only their immense distance from us, which renders their apparent dimensions so small. Now, if we consider them as enormous globes, instead of small twinkhng spots, we shall be led to suppose, that the Almighty would not have created them merely for the purpose of giving us a little light in the night, as it was formerly imagined, and we should find it more consistent with our ideas of the Divine wisdom and beneficence to suppose that these celestial bodies, should be created for the habitation of beings, who are, like us, blessed by his providence. Both in a moral as well as a physical point of view, it appears to me more rational to con- sider the planets as worlds revolving round the sun ; and the fixed stars as other suns, each of them attended by their respective system of planets, to which they impart their influence. We have brought our telescopes to such a degree of perfection, that from the appearances which the moon exhibits when seen through them, we have very good reason to conclude, that it is a habitable globe, for though it is true, that we cannot discern its towns and people, we can plainly perceive its mountains and valleys ; and some astronomers have gone so far as to imagine they discovered volcanos. Emily. If the fixed stars are suns, with planets revolving round them, why should we not see those planets as well as their suns ? Mrs. B. In the first place, we conclude that the planets of other systems, (like those of our own,) are much smaller than the suns which give them light ; therefore at so great a distance as to make the suns appear like fixed stars, the 84 CAUSES OF TH£ planets would be quite invisible. Secondiyj the light of the planets being only reflected light, is much more feeble than that of the fixed stars. There is exactly the same difference as between the light of the sun and that of the moon ; the first being a fixed star, the second a planet. Emily, But if the planets are worlds like our earth, they are dark bodies ; and instead of shining by night, we should see them only by day-light. And why do we not see the fixed stars also by day-light ? Mrs, B, Both for the same reason ; their light is so faint, compared to that of our sun reflected by the atmosphere, that it is entirely efiaced by it : the light emitted by the fixed stars may probably be as strong as that of our sun, at an equal distance ; but being so much more remote, it is diflfused over a greater space, and is consequently proportionally weakened. Caroline, True ; I can see much better by the light of a candle that is near me, than by that of one at a great distance. But I do not understand what makes the planets shine ? Mrs, B* What is it that makes the steel buttons on your brother's coat shine ? Caroline, The sun. But if it was the sun which made the planets shine, we should see them in the day-time when the sun shone upon them ; or if the faintness of their light prevented our seeing them in the day, we should not see tliem at all, for the sun cannot shine upon them in the night. Mrs, B, There you are in error. But in order to explain this to you, I must first make you acquainted with the various motions of the planets. You know, that according to the laws of attraction, the planets belonging to our system all gravitate towards the sun ; and that this force combined with that of projection, will occasion their revolution round the sun, in orbits more or less elliptical, according to the proportion which these two forces bear to each other. But the planets have also another motion ; they revolve upon their axes. The axis of a planet is an imaginary line which passes through its centre, and on which it turns ; and it is this motion which produces day and night. With that side of the planet facing the sun it is day ; and with the opposite side, which remains in darkness it is night. Our earth, which we consider as a planet, is 24 hours in performing one revolution on its axis ; in that period of time, therefore, we have a day and a night ; hence this revolution is called earth's annual motion. 85 the earth^s diurnai or daily motion ; and it is this revolution of the earth from west to east which produces an apparent motion of the sun^ moon, and stars in a contrary direction. Let us now suppose ourselves to be beings independent of any planet, travelling in the skies, and looking upon the earth in the same point of view as upon the other planets. Caroline. It is not flattering to us, its inhabitants, to see it make so insignificant an appearance. Mrs. B. To those who are accustomed to contemplate it in this light, it never appears more glorious. We are taught by science to distrust appearances : and instead of considering the planets as little stars, we look upon them either as brilliant suns or habitable worlds, and we consider the whole together as forming one vast and magnificent sys- tem, worthy of the Divine hand by which it was created. Emily. I can scarcely conceive the idea of this immensity of creation ; it seems too sublime for our imagination : — and to think that the goodness of Providence extends over mil- lions of worlds throughout a boundless universe — Ah ! Mrs. B., it is we only who become trifling and insignificant beings in so magnificent a creation ! Mrs. B. This idea should teach us humility, but without producing despondency. The same Almighty hand which guides these countless worlds in their undeviating course, conducts with equal perfection the blood as it circulates through the veins of a fly, and opens the eye of the insect to behold His wonders. Notwithstanding this immense scale of creation, therefore, w^e need not fear to be disregarded or forgotten. But to return to our station in the skies. We were, if you recollect, viewing the earth at a great distance, in appearance a little star, one side illuminated by the sun, the other in obscurity. But would you believe it, Caroline, many of the inhabitants of this little star imagine that when that part which they inhabit is turned from the sun, darkness prevails throughout the universe merely because it is night with them ; whilst, in reality, the sun never ceases to shine upon every planet. When, therefore, these little ignorant beings look around them during their night, and behold all the stars shin- ing, they cannot imagine why the planets, which are dark bodies, should shine, concluding, that since the sun does not illumine themselves, the whole universe must be in darkness. Caroline. I confess that I was one of these ignorant peo- 86 CAUSES OF THE EARTh's ANNUAL MOTION. pie ; but I am now very sensible of the absurdity of such an idea. To the inhabitants of the other planets, then, we must appear as a little star ? Mrs. B, YeSj to those which revolve round our sun ; for since those which may belong to other systems (and whose existence is only hypothetical,) are invisible to us, it is probable, that we also are invisible to them. Emily, But they may see our sun as we do theirs, in ap- pearance a fixed star ? Mrs, B, No doubt, if the beings who inhabit those planets are endowed with senses similar to ours. By the same rule, we must appear as a moon, to the inhabitants of our moon ; but on a larger scale, as the surface of the earth is about thirteen times as large as that of the moon. Emily, The moon, Mrs. B., appears to move in a differ- ent direction, and in a different manner from the stars ? Mrs, B, I shall defer the explanation of the motion of the moon, till our next interview, as it would prolong our present lesson too much. CONVERSATION VII ON THE PLANETS. fjf the Satellites or Moom ; Gravitij diminishes as the Square of the distance ; Of the Solar System; Of Com- ets ; Constellations. Signs of the Zodiac; Of Coperni- rus^ Newfon* &'c. MRS.B. The planets are distinguished into primary and secondary. Those which revolve immediately about the sun are called primary. Many of these are attended in their course by smaller planets, which revolve round them : these are called secondary planets, satellites, or moons. Such is our moon which accompanies the ^arth, and is carried with it round the sun. Emily, How then can you reconcile the motion of the secondar}' planets to the laws of gravitation ; for the sun is much larger than any of the primary planets ; and is not the power of gravity proportional to the quantity of matter ? Caroline, Perhaps the sun, though much larger, may be less dense than the planets. Fire you know is very ligbt, and it may contain but little matter, though of great mag-.ii- tude. Mrs. B. We do not know of what kind of matter the sun is made ; but we may be certain, that since it is the general centre of attraction of our system of planets, it must be the body which contains the greatest quantity of matter in tiat system. You must recollect, that the force of attraction is not only proportional to the quantity of matter, but to the degree of 88 ON THE PLANETS. proximity of the attractive body : this power is weakened, by being diffused, and diminishes as the squares of the distances increase. The square is the product of a number muhiplied by itseh^; so that a planet situated at twice the distance at which we are from the sun would gravitate four times less than we do ; for the product of two multiplied by itself is four. Caroline, Then the more distant planets move slower in their orbits; for their projectile force must be proportioned to that of attraction ? But I do not see how this accounts for the motion of the secondar}^ round the primary planets j in preference to the sun ? Emily. Is it not because the vicinity of the primary planets renders their attraction stronger than that of the sun ? Mrs, B, Exactly so. But since the attraction between bodies is mutual, the primary planets are also attracted by the satellites, which revolve round them. The moon attracts the earth, as well as the earth the moon ; but as the latter is the smaller body, her attraction is proportionally less ; therefore neither the earth revolves round the moon, nor the moon round the earth ; but they both revolve round a point, which is their common centre of gravity, and which is as much nearer the earth than the moon, as the gravity of the former exceeds that of the latter. Emily, Yes, I recollect your saying, that if two bodies were fastened together by a wire or bar, their common centre of gravity would be in the middle of the bar, pro^'ided the bodies were of equal weight ; and if they differed in weight, it would be nearer the larger body. If then the earth and moon had no projectile force which prevented their mutual attrac- tion from bringing them together, they would meet at their common centre of gravity. Caroline, The earth then has a great variety of motions, it revolves round the sun, upon its axis, and round the point towards which the moon attracts it. Mrs. B, Just so ; and this is the case with evory planet which is attended by satellites. The complicated effect of this variety of motions, produces certain irregularities, which, however, it is not necessary to notice at present. The planets act on the sun in the same manner as they are themselves acted on by their satellites ; for attraction, you must remember, is always mutual ; but the gravity of the planets (even when taken collectively) is so trifling compared PLA1\E kh F.o. L ILrschel ri^. 2. »j Hfnv^ Ve7iits Earth ^"""&' ^o o O IlerscJiel Ox\ THE PLANETS, ' 89 with that of the sun, that they do not cause the latter to move so much as one half of his diameter. The planets do not, therefore, revolve round the centre of the sun, but round a point at a small distance from its centre, about which the sun also revolves. Emily, I thought the sun had no motion ? Mrs. B, You were mistaken ; for besides that which I have just mentioned, which is indeed very inconsiderable, he revolves on his axis ; this motion is ascertained by observing certain spots w^hich disappear, and re-appear regularly at stated times. Caroline, A planet has frequently been pointed out to me in the heavens ; but I could not perceive that its motion differed from that of the fixed stars, which only appear to move. Mrs, B, The great distance of the planets renders their motion apparently so slow, that the eye is not sensible of their progress in their orbit, unless we watch them for some considerable length of time : in different seasons they appear in different parts of the heavens. The most accurate idea I can give you of the situation and motion of the planets, will be by the examination of this diagram, (plate VII. fig. 1.) representing the solar system, in which you will find every planet with its orbit delineated. Emily, But the orbits here are all circular, and you said^- that they were elliptical. The planets appear too, to be moving round the centre of the sun ; whilst you told us that they moved round a point at a little distance from thence. Mrs, B, The orbits of the planets are so nearly circular, and the common centre of gravity of the solar system so near the centre of the sun, that these deviations are scarcely worth observing. The dimensions of the planets, in their true pro- portions, you will find delineated in fig. 2. Mercury is the planet nearest the sun ; his orbit is conse- quently contained within ours ; but his vicinity to the sun, occasions his being nearly lost in the brilliancy of his rays ; and when we see the sun, he is so dazzling, that very accurate observations cannot be made upon Mercury. He performs his revolution round the sun in about 87 days, which is conse- quently the length of his year. The time of his rotation on his axis is not known ; his distance from the sun is computed to be 37 millions of miles, and his diameter 3180 miles, 8* 90 ON THE PLANETS. The heat of this planet is so great, that water cannot exist tliere, but in a state of vapour, and metals would be liquified.^ Caroline. Oh, what a dreadful climate ! Mrs, B. Though we could not live there, it may be per- fectly adapted to other beings destined to inhabit it. Venus, the next in the order of planets, is 68 millions of miles from the sun ; she revolves about her axis in 23 hours and 21 minutes, and goes round the sun in 244 days 17 hours. The orbit of Venus is also within ours ; during one half of her course in it, we see her before sun-rise, and she is called the morning star ; in the other part of her orbit, she rises later than the sun. Caroline. In that case, we cannot see her, for she must rise in the day time ? Mrs. B. True ; but when she rises later than the sun, sjie also sets later ; so that we perceive her approaching the horizon after sun-set : she is then called Hesperus, or the evening star. Do you recollect those beautiful lines of Milton : Now came still evening on, and twilight gray Had in her sober livery all things clad ; Silence accompanied ; for beast and bird, They to their grassy couch, these to their nests "Were slunk, all but the wakeful nightingale ; She all night long her amorous descant sung ; Silence waspleas'd ; now glow'd the firmament With living sapphires. Hesperus, that led The starry host, rode brightest, till the moon Rising in clouded majesty, at length Apparent queen unveil'd her peerless light, And o'er the dark her silver mantle threw. The planet next to Venus is the Earth, of which we shall soon speak at full length. At present I shall only observe, that we are 95 millions of miles distant from the sun, that we perform our annual revolution in 365 days, 5 hours, and 49 minutes ; and are attended in our course by a single moon. Next follows Mars. He can never come between us and the sun, like Mercury and Venus ; his motion is, however, very perceptible, as he may be traced to different situations in * The intenseness of the sun's heat, which is in the same proportion as his light, is seven times as great in Mercur} as with us ; so that water there would be carried off in the shape of steam, for by experiments with the thermometer, it appears that a heat seven times greater than that d" the sun's beams in summer will serve to make water boil. ON THE PLANETS. 91 the heavens; his distance from the gun is 144 miUions of miles ; he turns round his axis in 24 hours and 39 minutes ; and he performs his annual revolution, in about 687 of our days: his diameter is 4120 miles. Then follow four very small planets, Juno, Ceres, Pallas, and Vesta, which have been recently discovered, but whose dimensions and distances from the sun have not been very accurately ascertained.* Jupiter is next in order : this is the largest of all the plan- ets. He is about 490 millions of miles from the sun, and completes his annual period in nearly 12 of our years. He turns round his axis in about ten hours. He is above 1200 times as big as our earth ; his diameter being 86^000 miles. The respective proportions of the planets cannot, therefore, you see, be conveniently delineated in a diagram. He is attended by four moons. t The next planet is Saturn, whose distance from the sun is about 900 millions of miles ; his diurnal rotation is performed in 10 hours and a quarter: — his annual revolution in nearly 30 of our years. His diameter is 79,000 miles. This planet is surrounded by a luminous ring, the nature of which, as- tronomers are much at a loss to conjecture ; he has seven moons. Lastly, we observe the Georgium Sidus, discovered by Dr. Herschel, and which is attended by six moons. J Caroline. How charming it must be in the distant planets, to see several moons shining at the same time ; I think I should like to be an inhabitant of Jupiter or Saturn. Mrs. B. Not long, I believe. Consider what extreme cold must prevail in a planet, situated as Satarn is, at nearly ten times the distance at which we are from the sun. Then his numerous moons are far from making so splendid an *These anomalous bodies, so unlike the other primary planets, Dr. Herschel has denominated Asteroids. Probably they are the fragments of some planet ; or perhaps other similar bodies abound in the solar system, though they have hitherto, from their sraallness or darkness, escaped observation. -f Jupiter is surrounded by cloudy substances, subject to frequent changes in their situation and appearance, called Belts. These Belts are sometimes of a regular form ; sometimes interrupted and broken ; and sometimes not at all to be seen. t This ring is set edgewise round it, and the distance of the rmg from the planet is equal to the breadth of the ring. The sun shines for almost fifteen of our years together on the northern side of the ring ; then goes off, and shines as long on the southern side of it, so there is but one day and one night on each side of the ring, in the time of Saturn's whole revolution about the sun, whi«h takes up almost thirty of our years. 92 ON THE PLANETS. appearance as ours ; for th^y can reflect only the light which they receive from the sun ; and both light and heat decrease in the same ratio or proportion to the distances as gravity. Can you tell me now how much more light we enjoy than Saturn. Caroline, The square of ten, is a hundred ; therefore, Saturn has a hundred times less — or to answer your question exactly, we have a hundred times more light and heat than Saturn — this certainly does not increase my wish to become one of the poor wretches who inhabit that planet.* Mrs, B. May not the inhabitants of Mercury, with equal plausibility, pity us, for the insupportable coldness of our situation ; and those of Jupiter and Saturn for our intolerable heat ? The Almighty Power w^hich created these planets, and placed them in their several orbits, has no doubt peopled them w^ith beings whose bodies are adapted to the various temperatures and elements in which they are situated. If we judge from the analogy of our own earth, or from that of the great and universal beneficence of Providence, we must con- clude this to be the case. Caroline. Are not comets also supposed to be planets ? Mrs. B. Yes, they are ; for by the re-appearance of some of them, at stated times, they are know^n to revolve round the sun, but in orbits so extremely eccentric, that they disappear for a great number of years. If they are inhabited, it must be by a species of beings very different, not only from the inhabitants of this, but from those of any of the other planets, as they must experience the greatest vicissitudes of heat and cold ; one part of their orbit. being so near the sun, that their heat, when there, is computed to be greater than that of red- hot iron ; in this part of its orbit, the comet emits a luminous vapour, called the tail, which it gradually loses as it recedes from the sun ; and the comet itself totally disappears from our sight, in the more distant parts of its orbit, which extends considerably beyond that of the furthest planet. The number of comets belonging to our system, cannot be ascertained, as some of them are whole centuries before they make their re-appearance. The numbers that are known by . their regular re-appearance is only three. Emily. Pray, Mrs. B. what are the constellations ? • The sun's light at Saturn is 1 0^0 times as great as the light of the full moon is to us. PhAT^ 1 I ON THE PLANETS. 93 Mrs, B, They are the fixed stars, which the ancients, in order to recognize them, formed into groupes, and gave the names of the figures, which you find delineated on the celestial globe. In order to show their proper situations in the heav- ens, they should be painted on the internal surface of a hollow sphere, from the centre of which you should view them ; you would then behold them, as they appear to be situated in the heavens. The twelve constellations, called the signs of the zodiac, are those w^hich are so situated, that the earth in its annual revolution passes directly between them and the sun. Their names are Aries, Taurus, Gemini, Cancer, Leo, Virgo, Libra, Scorpio, Sagittarius, Capricornus, Aquarius, Pisces ; the whole occupying a complete circle, or broad belt, in the heavens, called the zodiac, (plate VIII. fig, 1.) Hence, a right line drawn from the earth, and passing through the sun, v>^ould reach one of these constellations, and the sun is said to be in that constellation at which the line terminates : thus, when the earth is at A, the sun would appear to be in the constellation or sign Aries ; when the earth is at B, the sun would appear in Cancer ; when the earth was at C, the sun would be in Libra ; and when the earth was at D, the sun would be in Capricorn. This circle, in which the sun thus appears to move, and which passes through the middle of the zodiac, is called the ecliptic. Caroline, But many of the stars in these constellations appear beyond the zodiac. Mrs, B, We have no means of ascertaining the distance of the fixed stars. When, therefore, they are said to be in the zodiac, it is merely implied, that they are situated in that direction, and that they shine upon us through that portion of the heavens, which we call the zodiac* Emihj, But are not those large bright stars, which are called stars of the first magnitude, nearer to us, than those small ones which vv^e can scarcely discern ? Mrs, B. It may be so ; or the difference of size and brilliancy of the stars may proceed from their difference of dimensions ; this is a point which astronomers are not enabled to determine. Considering them as suns, I see no reason * An easy distinction between a planet and a f.xed star is this — the torn-iCr shines with a steady liglit, but the latter is constantly twinkling. \V hat it is which occasions tliis twinkling* oi* scintillation of a star, y^t remains undecided. 94 ON THE PLANETS. why different sunS should not vary in dimensions as well as the planets belonging to them. Emily, Whai a wonderful and beautiful system this is, and how astonishing to think that every fixed star may probably be attended by a similar train of planets ! Caroline, You will accuse me of being very incredulous, but I cannot help still entertaining some doubts, and fearing that there is more beauty than truth in this system. It cer- tainly may be so ; but there does not appear to me to be sufficient evidence to prove it. It seems so plain and obvious that the earth is motionless, and that the sun and stars revolve round it ; your solar system, you must allow, is directly in opposition to the evidence of our senses. Mrs, B. Our senses so often mislead us, that we should not place implicit reliance upon them. Caroline, On what then can we rely, for do we not receive all our ideas through the medium of our senses ? Mrs, B, It is true that they are our primary source of knowledge ; but the mind has the power of reflecting, judging, and deciding upon the ideas received by the organs of sense. This faculty, which we call reason, has frequently proved to us, that our senses are liable to err. If you have ever sailed on the water, with a very steady breeze, you must have seen the houses, trees, and every object move, while you were sailing. Caroline, I remember thinking so, when I was very young ; but I now know that their motion is only apparent. It is true that my reason, in this case, corrects the error of my sight. Mrs, B, It teaches you that the apparent motion of the objects on shore, proceeds from your being yourself moving, and that you are not sensible of your own motion, because you meet with no resistance. It is only when some obstacle impedes our motion, that we are conscious of moving ; and if you were to close your eyes when you were sailing on calm water, with a steady wind, you would not perceive that you moved, for 3^ou could not feel it, and you could see it only by observing the change of place of the objects on shore. So it is with the motion of the earth ; every thing on its surface, and the air that surrounds it, accompanies it in its revolution ; it meets w^ith no resistance : therefore, hke the crew of a vessel sailing w^ith a fair wind, in a calm sea, we are insensible of our motion. ON THE PLANETS. 95 Caroline, But the principal reason why the crew of a vessel in a calm sea do not perceive their motion, is, because they move exceedingly slowly ; while the earth, you say, revolves with great velocity. Mrs* B. It is not because they move slowly, but because they move steadily, and meet with no irregular resistances, that the crew of a vessel do not perceive their motion ; for they would be equally insensible to it, with the strongest wind, provided it were steady, that they sailed with it, and that it did not agitate the water ; but this last condition, you know, is not possible, for the wind will always produce waves whkh offer more or less resistance to the vessel, and then the motion becomes sensible, because it is unequal. Caroline. But, granting this, the crew of a vessel have a proof of their motion, though insensible, which the inhabitants of the earth cannot have, — the apparent motion of the objects on shore. Mrs. B. Have we not a similar proof of the earth's motion, in the apparent motion of the sun and stars. Imagine the earth to be sailing round its axis, and successively passing by every star, which, like the objects on land, we suppose to be moving instead of ourselves. I have heard it observed by an aerial traveller in a balloon, that the earth appears to sink beneath the balloon, instead of the balloon rising above the earth. It is a law which we discover throughout nature and worthy of its great Author, that all its purposes are accomplished by the most simple means ; and what reason have we to suppose this law infringed, in order that we may remain at rest, while the sun and stars move round us ; their regular motions, which are explained by the laws of attraction on the first supposition, would he unintelligible on the last, and the order and harmony of the universe be destroyed. Think what an immense circuit the sun and stars would make daily, were their apparent motions real. We know many of them to be bodies more considerable than our earth ; for our eyes vainly endeavour to persuade us, that they are little brilliants spark- ling in the heavens, while science teaches us that they are immense spheres, whose apparent dimensions are diminished by distance. Why then should these enormous globes daily traverse such a prodigious space, merely to prevent the necessity of our earth's revolving on its axis ? ^J ON THE PLANETS. Caroline. I think I must now be convinced. But you wiilj I hope, allow me a little time to familiarize myself to an idea so different from that which I have been accustomed to entertain. And pray, at what rate do we move ? Mrs. B. The motion produced by the revolution of the earth on its axis, is about eleven miles a minute, to an inhab- itant of London. Emily. But does not every part of the earth move with the same velocity ? Mrs. B. A moment's reflection would convince you of the contrary ; a person at the equator must move quicker dian one situated near the poles, since they both perform a revolution in 24 hours. Emily. True, the equator is farthest from the axis of motion. But in the earth's revolution round the sun^ every part must move with equal velocity ? Mrs. B. Yes, about a thousand miles a mini'te. Caroline. How astonishing ! — and that it should be pos- sible for us to be insensible of such a rapid motion. You would not tell me this sooner, Mrs. B., for fear f increasing my incredulity. Before the time of Newton, was not the earth supposed to be in the centre of the system, and the sun, moon, and stars to revolve round it ? Mrs. B. This was the system of Ptolemy in ancient times ; but as long ago as the beginning of the sixteenth cen- tury it was discarded, and the solar system, such as I have shown you, was established by the celebrated astronomer Copernicus, and is hence called the Copernican system. But the theory of gravitation, the source from which this beautiful and harmonious arrangement flows, we owe to the powerful genius of Newton, who lived at a much later period. Emily. It appears, indeed, far less difficult to trace by observation the motion of the planets, than to divine by what power they are impelled and guided. I wonder how the idea of gravitation could first have occurred to Sir Isaac Newton ? Mrs. B. It is said to have been occasioned by a circum- stance from which one should little have expected so grand a theory to have arisen. During the prevalence of the plague in the year l665, Newton retired into the country io avoid the contagion : when ON THE PLANETS. 97 ^^ikig one day in his orchard he observed an apple fail from tree, and was led to consider what could be the cause which jrought it to the ground. Caroline, If I dared to confess it, Mrs. B., I should say that such an enquiry indicated rather a deficiency than a. superiority of intellect. I do not understand how any one can wonder ai what is so natural and so common. Mr^. B. It is the mark of superior genius to find matter for wonder, observation, and research, in circumstances which, to the ordinary mind, appear trivial, because they are com- mon, and with which they are satisfied, because they are natural, without reflecting that nature is our grand field of observation, that within it is contained our whole store of knowledge ; in a word, that to study the works of nature, is to learn to appreciate and admire the wisdom of God. Thus, it was the simple circumstan€e of the fall of an apple, which led to the discovery of the laws upon which the Copernicaii system is founded ; and whatever credit this system had ob- tained before, it now rests upon a basis from which it cannot be shaken. Emily. This was a most fortunate apple, and more wor- t^.y to be commemorated than all those that have been sung by the poets. The apple of discord for which the goddesses contended ; the golden apples by which Atalanta won the race ; nay, even the apple which William Tell shot from the head of his son, cannot be compared to this ! The Strx. The sun is a spherical body, situated near tlie centre of gravity in the system of planets, of which our earth is one. Its diameter IS 877,547 English miles ; or equal to 100 diameters of the earth ; and therefore its cubic magnitude must exceed that of the earth one millioa of times. It revolves round its axis in 25 days, and 10 hours, vhich has been determined by means of several dark spots seen with telescopes on that luminary. Dr. Herschel supposes these spots in the sun to be the appearance of the opaque body of the sun througl^ the openings in his luminous atapoaphere,. CONVERSATION VIH- ON THE EARTH. Of the Terrestrial Globe ^ Of the Figure of the Earth ; Of the Pendulum ; Of the Variation of the Seasons^ and of the Length of Days and Nights ; Of the causes of the Heat of Summer ; Of Salary Siderial^ and Equal or Mean Time. MRS. B. As the earth is the planet in which we are the most partic- ularly interested, it is my intention this morning, to explain to you the effects resulting from its annual and diurnal motions ; but for this purpose it will be necessary to make j^ou acquaint- ed with the terrestrial globe : you have not either of you^ I conclude, learnt the use of the globes ?* Caroline. No ; I once indeed learnt by heart the names of the lines marked on the globe, but as I was informed they were only im,aginary divisions, they did not appear to me worthy of much attention, and were soon forgotten. Mrs* B» You suppose, then, that astronomers had been at the trouble of inventing a number of lines to little purpose. It will be impossible for me to explain to you the particular effects of the earth's motion without your having acquired a knowledge of these lines : in plate VIH. fig. 2. you will find • The earth is of a globular form. For, 1. The shadow of the earth projected on the moon in an eclipse is always circular ; which appearance could only be produced by a spherical body. 2. The convexity of the surface of the sea is evident ; the mast of an approaching ship being seea before its hull. 3. The north pole becomes more elevated by travelling northward, in proportion to the space passed over. 4. Navigators have sailed round the earth, and by steering their course continually weftward^ t^rriyed, at leogth^ at the plate from wheaoe they departed* ON THE JEARTH. 99 them all delineated ; and you must learn them perfectly if you wish to make any proficiency in astronomy. Caroline, I was taught them at so early an age that I could not understand their meaning ; and I have often heard you say that the only use of words was to convey ideas. Mrs. B, The names of these lines would have conveyed ideas of the figures they were designed to express, though the use of these figures might at that time have been too difficult for you to understand. Childhood is the season when impres- sions on the memory are most strongly and most easily made : k is the period at which a large stock of ideas should be treas- ured up J the application of which we may learn when the understanding is more developed. It is, I think, a very mis- taken notion that children should be taught such things only^ as they can perfectly understand. Had you been early made acquainted with the terms which relate to figure and motion^ how much it would have facilitated your progiess in natural philosophy. I have been obliged to confine myself to the most common and familiar expressions, in explaining the laws of nature, though 1 am convinced that appropriate and scien- tific terms would have conveyed more precise and accurate ideas ; but I was afraid of not being understood. Emily. You may depend upon our learning the names of these lines thoroughly, Mrs* B. ; but before we commit them to memory, will you have the goodness to explain them to us ? Mrs. B, Most willingly. This globe, or sphere, repre- sents the earth ; the line which passes through its centre, and on which it turns, is called its axis, and the two extremities oi the axis A and B, are the poles, distinguished by the names of the north and south pole. The circle C D, which divides the globe into two equal parts between the poles, is called the equator, or equinoctial line ; that part of the globe to the north of the equator is the northern hemisphere ; that part to the south of the equator, the southern hemisphere. The small circle E F, which suj-rounds the north pole, is called the arctic circle ; that G H, which surrounds the south pole, the antarctic circle. There are two intermediate circles be- tween the polar circles and the equator ; that to the north, I Kj called the tropic of Cancer ; that to the south, L M, called the tropic of Capricorn. Lastly, this circle, L K, which divides the globe into two equal parts, crossing the equator and extending northward as far as the tropic of Can- cer, and southward as far as the tropic of Capricorn, is called 100 ON THE EARTH. tlie ecliptic. The delineation of the ecliptic on the terrestrial globe is not without danger of conveying false ideas ; for the ecliptic (as I have before said) is an imaginary circle in the heavens passing through the middle of the zodiac, and situated in the plane of the earth's orbit. Cai'oline, I do not understand the meaning of the plane of the earth's orbit. Mrs, B. A plane, or plain, is an even level surface. Let us suppose a smooth thin solid plane cutting the sun through the centre, extending out as far as the fixed stars, and termin- ating in a circle which passes through the middle of the zodiac ; in this plane the earth would move in its revolution round the sun ; it is therefore called the plane of the earth's orbit, and the circle in which this plane cuts the signs of the zodiac is the ecliptic. Let the fig, 1» plate IX. represent such a plane, S the sun, E the earth with its orbit, and A B C D the echp- tic passing through the middle of the zodiac. Emily, li tlie ecliptic relates only to the heavens, why is it described upon the terrestrial globe ? Mrs, B, It is. convenient for the demonstration of a vari- ety of problems in the use of the globes ; and besides, the obliquity of this circle to the equator is rendered more con- spicuous by its being described on the same globe ; and the obliquity of the ecliptic shows the inclination of the earth's axis to the plane of its orbit. But to return to fig. 2. plate VIII. The spaces between the several parallel circles on the ter- restrial globe are called zones ; that which is comprehended between the tropics is distinguished by the name of the torrid zone ; the spaces which extend from the tropics to the polar circles, the north and south temperate zones ; and the spaces, contained within the polar circles, the frigid zones. The several lines which, you observe, are drawn from one pole to the other, cutting the equator at right angles, are called meridians. When EJjy one of these meridians is exactly opposite the sun it is rkid-day, or twelve o'clock in the day, with all the places situated on that meridian ; and, with the places situated on the opposite meridian, it is consequently midnight. Emihj, To places situated equally distant from these two meridians, it must then be six o'clock ? Mrs. B. Yes : if thev are to the east of the sun'$ meri- BLATJS iX. ON THE EARTH. lOi ciian it is six o'clock in the afternoon, because the sun will have previously passed over them ; if to the west, it is six o'clock in the morning, and the sun will be proceeding to-^ wards that meridian. Those circles which divide the globe into two equal parts^ such as the equator and the ecliptic, are called greater circles ; to distinguish them from those which divide it into two une- qual parts, as the tropics and polar circles, which are called lesser circles. All circles are divided into 360 equal parts, called degrees, and degrees into 60 equal parts, called minutes. The diameter of a circle is a right line drawn across it^ and passing through the centre ; for instance, the boundary of this sphere is a circle, and its axis the diameter of that circle ; the diameter is equal to a little less than one-third of the circumference. Can you tell me nearly how many degrees it contains ? Caroline, It must be something less than one-third of 360 degrees, or nearly 120 degrees. Mrs, B, Right ; now Emily you may tell me exactly how many degrees are contained in a meridian ? Emily. A meridian, reaching from one pole to the other, is half a circle, and must therefore contain 180 degrees. Mrs, B, Very well ; and what number of degrees are there from the equator to the poles ? Caroline, The equator being equally distant from either pole, that distance must be half of a meridian, or a quarter of the circumference of a circle, and contain 90 degrees. Mrs, B, Besides the usual division of circles into degrees^ the ecliptic is divided into twelve equal parts, called signs, which bear the names of the constellations through which this circle passes in the heavens. The degrees measured on the meridians from north to south, or south to north, are called degrees of latitude ; those measured from east to west on the equator, the echptic, or any of the lesser circles are called degrees of longitude ; hence these circles bear the name of longitudinal circles ; they are also called parallels of latitude. Emily, The degrees of longitude must then vary in length according to the dimensions of the circle on which they are reckoned ; those^ for instance, at the polar circles will be considerably smaller than those at the equator ? Mrs, B, Certainly ; since the degrees of circles of differ- ent dimensions do not vary in number, they must necessarily 9# I0::i ON THE EARTB. vary in length. The degrees of latitude, 3^011 may observe^ never vary m length ; for the meridians on which they axe reckoned are all of the same dimensions. Emily. And of what length is a degree of latitude ? Mrs, B, Sixty geographical miles, which is equal to 69 i English statute miles. Emily, The degrees of longitude at the equator must then be of the same dimensions ? Mrs, B, They would, were the earth a perfect sphere ; but its form is not exactly* spherical, being somewhat protu- berant about the equator, and flattened towards the poles. This form is supposed to proceed from the superior action of the centrifugal power at the equator. Caroline, I thought I had understood the centrifugal force perfectly, but I do not comprehend its effect in this instance. Mrs. B, You know that the revolution of the earth on its axis must give every particle a tendency to fly ofl* from the centre, that this tendency is stronger or weaker in proportion to the velocity with which the y article moves ; now a parti- cle situated near one of the polar circles makes one rotation in the same space of time as a particle at the equator ; the latter, therefore, having a much larger circle to describe^ travels proportionally faster, consequently the centrifugal force is much stronger at the equator than at the polar circles : it gi'adually decreases as you leave the equator and approach the poles, where, as there is no rotatory motion, it entirely ceases. Supposing, therefore, the earth to have been origin- ally in a fluid state, the particles in the torrid zone would recede much farther from the centre than those in the frigid zones ; thus the polar regions would become flattened, and those about the equator elevated. Caroline. I did not consider that the particles in the neighborhood of the equator move with greater velocity than those about the poles ; this was the reason I could not under- stand you. Mrs, B. You must be careful to remember, that those j^arts of a body which are farthest from the centre of motion must move with the greatest velocity : the axis of the earth is the centre of its diurnal motion, and the equatorial regions the parts most distant from the axis. Caroline. My head then moves faster than my feet ; and upon the summit of a mountain we are carried round quicker ^anin a vallev? Mrs* B. Certainlyj your head is more distant from the centre of motion, than your feet; the mountain-top than the valley : and the more distant any part of a body is from the centre of motion, the larger is the circle it will describe, and the greater therefore must be its velocity. Emily, I have been reflecting that if the earth is not a perfect circle..... Mrs, B. A sphere you mean, my dear ; a circle is a round line, every part of which is equally distant from the centre ; a sphere or globe is a round body^ the surface of which is every where equally distant from the centre. Emily. If, then, the earth is not a perfect sphere, but prominent at the equator, and depressed at the poles, would not a body weigh heavier at the equator than at the poles ? For the earth being thicker at the equator, the attraction of gravity perpendicularly downwards must be stronger. Mrs, B. Your reasoning has some plausibility, but I am sorry to be obliged to add that it is quite erroneous ; for the nearer any part of the surface of a body is to the centre of attraction, the more strongly it is attracted ; because the most considerable quantity of matter is about that centre. In re- gard to its effects, you might consider the power of gravity, as that of a magnet placed at the centre of attraction. Emily, But were you to penetrate deep into the earth, would gravity increase as you approached the centre ? Mrs, B, Certainly not ; I am referring only to any sit- uation on the surface of the earth. Were you to penetrate into the interior, the attraction of the parts above you would counteract that of the parts beneath you, and consequently diminish the power of gravity in proportion as you approached the centre ; and if you reached that point, being equally attracted by the parts all around you, gravity would cease, and you would be without weight. Emily, Bodies then should weigh less at the equator than at the poles, since they are more distant from the centre of gravity in the former than in the latter situation. Mrs^ B, And this is really the case ; but the difference of weight would be scarcely sensible, were it not augmented by another circumstance. Caroline, And what is this singular circumstance which seems to disturb the laws of nature ? Mrs. B, One that you are well acquainted with, as con- ^^ucing more to the preservation than the destruction of order, 104 ON THE EARTH, — ^the centrifugal force. This we have just observed to be stronger ai the equator ; and as it tends to drive bodies from the centre, it is necessarily opposed to, and must lessen the power of gravity? which attracts them towards the centre. We accordingly find that bodies weigh lightest at the equator, ivhere the centrifugal force is greaiest ; and heaviest at the poles, where this power is least.* Caroline. Has the experiment been made in these differ- ent situations ? Mrs. B, Lewis XIV., of France, sent philosophers both to the equator and to Lapland for this purpose ; the severity of the climate, and obstruction of the ice, has hitherto rendered every attempt to reach the pole abortive ; but the difference of gravity at the equator and in Lapland is very perceptible. Caroline. Yet I do not comprehend, how the difference of weight could be ascertained ; for if the body under trial decreased in weight, the weight which was opposed to it in the opposite scale must have diminished in the same propor- tion. For instance, if a pound of sugar did not weigh so heavy at the equator as at the poles, the leaden pound which served to weigh it, would not be so heavy either : therefore they would still balance each other, and the different force of gravity could not be ascertained by this means. Mrs. B. Your observation is perfectly just : the drfference of gravity of bodies situated at the poles and at the equator cannot be ascertained by weighing them ; a pendulum was therefore used for that purpose. Caroline. What, the pendulum of a clock ? how could that answer the purpose ? Mrs. B. A pendulum consists of a line, or rod, to one end of which a weight is attached, and it is suspended by ihe other to a fixed point, about which it is made to vibrate. Without being put in motion, a pendulum, like a plumb line, hangs perpendicular to the genera! surface of the earth, by which it is attracted ; but, if you raise a pendulum, gravity will bring it back to its perpendicular position. It will, how- ever, not remain stationary there, for the velocity it has received during its descent will impel it onwards, and it will rise on the opposite side to an equal height : from thence it * If the diurnal raotion of the earth round its axis was about 17 times faster than it is, th centrifugal force would, at the equator, be equal to the power of gravity, and all Hodi^s there would entirely lose weight Bat if the earth revolved still quicker thau this, they would all fly off. ON THE EARTH. 10? is brought back by gravity, and again driven by the impulse of its velocity. Caroline. If so, the motion of a pendulum would be per- petual, and I thought you said that there was no perpetual motion on the earth. Mrs, B, The motion of a pendulum is opposed by the resistance of the air in which it vibrates, and by the friction of the part by which it is suspended : were it possible to re- move these obstacles, the motion of a pendulum would be perpetual, and its vibrations perfectly regular : being of equal distances, and performed in equal times.* Emily, That is the natural result of the uniformity of the power which produces these vibrations, for the force of gravity being always the same, the velocity of the pendulum must consequently be uniform. Caroline. No, Emily, you are mistaken ; the cause is not always uniform, and therefore the effect will not be so either, I have discovered it, Mrs. B. ; since the force of gravity is less at the equator than at the poles, the vibrations of the pendulum will be slower at the equator than at the poles. Mrs, B, You are perfectly right, Caroline ; it was by this means that the difference of gravity was discovered, and the true figure of the earth ascertained. Emily, But how do they contrive to regulate their time in the equatorial and polar regions ? for, since in this part of the earth the pendulum of a clock vibrates exactly once in a second, if it vibrates faster at the poles and slower at the equator, the inhabitants must regulate their clocks in a differ- ent manner from ours. Mrs, B, The only alteration required is to lengthen the pendulum in one case, and to shorten it in the other ; for the velocity of the vibrations of a pendulum depends on its length ; and when it is said, that a pendulum vibrates quicker at the pole than at the equator, it is supposing it to be of the same length. A pendulum which vibrates a second in this latitude * The vibrations ot pendulums are subject to many irregularities, for which no effectual remedy has yet been devised. These are owing- partly to the variable density and temperature of the air, partly to the rigidity and friction of the rod by which they are suspended, and principally to the dilatation and contraction of the materials, of which they are formed. The metalline rods of pendulums are expanded by heat, and contracted by cold ; therefore clocks will go faster m winter^ and slower in summer. The common remedy for this inconvenience is the raising or lowering th© bob ©f the peadulum, by raieaDS of a screwj as occasion may re B, If the earth had no progressive motion in its orbit whilst it revolves on its axis, this would be the case ; but as it advances almost a degree westward in its orbit, in the same time that it completes a revolution eastward on its axis, it must revolve nearly one degree more in order to bring the same meridian back to the sun. Caroline, Oh, yes ! it will require as much more of a second revolution to bring the same meridian back to the sun, as is equal to the space the earth has advanced in her orbit, that is, nearly a degree ; this difference is, however, very little. Mrs, B, These small daily portions of rotation are each equal to the three hundred and sixty-fifth part of a circle, which at the end of the year amounts to one complete rotation. Emily, That is extremely curious. If the earth, then, had no other than its diurnal motion, we should have S6G days in the year. Mrs, B, We should have 366 days in the same period of time that we now have S6^ ; but if we did not revolve round the sun, we should have no natural means of computing years, You will be surprised to hear, that if time is calculated by the stars instead of the sun, the irregularity which we have just noticed does not occur, and that one complete rotation of the earth on its axis, brings the same meridian back to any fixed star. fmihj. That seems quite unaccountable : for the eai'th ON THE EARTH. IW advances in her orbit with regard to the fixed stars, the same as with regard to the sun. Mrs, B, True J but then the distance of the fixed stars is so immensej that our solar system is in comparison to it but a spot, and the whole extent of the earth's orbit but a point ; therefore, whether the earth remained stationary, or whether it revolved in its orbit during its rotation on its axis, no sensible difference would be produced with regard to the fixed stars. One complete revolution brings the same meridian back to the same fixed star ; hence the fixed stars appear to go round the earth in a shorter time than the sun by three minutes fifty-six seconds of time. Caroline, These three minutes fifty-six seconds is the time which the earth takes to perform the additional three hundred and sixty-fifth part of the circle, in order to bring the same meridian back to the sun. Mrs, B, Precisely. Hence the stars gain every day three minutes fifty-six seconds on the sun, which makes them rise that portion of time earlier every day. When time is calculated by the stars it is called sidereal time, when by the sun solar or apparent time.* Caroline, Then a sidereal day is three minutes fifty-six seconds shorter than a solar day of twenty-four hours. Mrs, B, I must also explain to you what is meant by a sidereal year. The common year, called the solar or tropical year, con- taining 365 days, five hours, forty-eight minutes, and fifty-two seconds, is measured from the time the sun sets out from one of the equinoxes, or solstices, till it returns to the same again ; but this year is completed before the earth has finished one entire revolution in its orbit. Emily, I thought that the earth performed one complete revolution in its orbit every year ; what is the reason of this variation ? Mrs, B, It is owing to the spheroidal figure of the earth. The elevation about the equator produces much the same * If one clock should be so well regulated as to shew the time to be XII at noon this day, and on the 365th day afterward ; and another clock should be so well regulated as to show the time to be XII every day or night when any given star is on the meridian ; the latter clock would gain three minutes, fifty -five seconds, and fifty-four sixtieth parts of a second upon the former in each revolution of the same star to the met'i- dian. 10* 114 ON THE EARTH. eftect as if a similar mass of matter, collected in the form of a moon, revolved round the equator. When this moon acted on the earth in conjunction with or in opposition to the sun, variations in the earth's motion would be occasioned, and these variations produce what is called the precession of the equinoxes* Emily, What does that mean ? I thought the equinoctial points, or nodes, were fixeil points in the heavens, in which die equator cuts the ecliptic. Mrs, B. These points are not quite fixed, but have an apparently retrograde motion, that is to say, instead of being every revolution in the same place, they move backwards. Thus if the vernal equinox is at A, (fig. 1. plate XI.) the autumnal one will be at B instead of C, and the following vernal equinox at D instead of at A, as would be the case if the equinoxes were stationary at opposite points of the earth's orbit. Caroline. So that when the earth moves from one equi- nox to the other, though it takes half a year to perform th^ journey, it has not travelled through half its orbit. Mrs, B, And, consequently, when it returns again to the first equinox, it has not completed the whole of its orbit. In order to ascertain when the earth has performed an entire revolution in its orbit, we must observe when the sun returns in conjunction with any fixed star ; and this is called a side- real year. Supposing a fixed star situated at E, (fig. 1. plate XI.) the sun would not appear in conjunction with it till the earth had returned to A, when it would have completed its orbit. Emily, And how much longer is the sidereal than the solar year ? Mrs, B, Only twenty minutes ; so that the variation of the equinoctial points is very inconsiderable. I have given them a greater extent in the figure in order to render them sensible. In regard to time, I must further add, that the earth's diu¥- pal motion on an inclined axis, together with its annual rev- olution in an elliptic orbit, occasions so much comphcation in its motion, as to produce many irregularities ; therefore, true equal time cannot be measured by the sun. A clock, which was always perfectly correct, would in some parts of the year be before the sun, and in other parts after it. There are but ibur periods in which the sun and a perfect clock would' I. >;f ON THE EARTH. 115 agree, which is the 15th of April, the l6th of June, the 23d of August, and the 24th of December. Emily, And is there any considerable difference between solar time and true time ? Mrs, B, The greatest difference amounts to between fifteen and sixteen minutes. Tables of equation are con- structed for the purpose of pointing out and correcting these differences between solar time and equal or mean time, which is the denomination giTen by astronomers to true time. CONVERSATION IX. ON THE MOON. Of the Moon^s Motion ; Phases of the Moon ; Eclipses of the Moon ; Eclipses of Jupiter's Moons ; Of the Lati- tude and Longitude ; Of the Transits of the Inferior Planets ; Of the Tides, MRS. B. We shall to-day confine our attention to the moon^ which offers many interesting phenomena. The moon revolves round the earth in the space of about twenty-nine days and a half, in an orbit nearly parallel to that of the earth, and accompanies us in our revolution round the sun. Emily. Her motion then must be rather of a complicated nature ; for as the earth is not stationary, but advances in her orbit whilst the moon goes round her, the moon must pro- ceed in a sort of progressive circle. Mrs, B, That is true ; and there are also other circum- stances which interfere with the simplicity and regularity of the moon's motion, but which are too intricate for you to understand at present. The moon always presents the same face to us, by which it is evident that she turns but once upon her axis, while she performs a revolution round the earth ; so that the inhabitants of the moon have but one day and one night in the course of a lunar month. Caroline. We afford them however the advantage of a magnificent moon to enlighten their long nights. Mrs. B* That advantage is but partial ; for since we al- ON THE MOON. Il7 ways see the same hemisphere of the moorij the inhabitants of that hemisphere alone can perceive us. Caroline, One half of the moon then enjoys our light every night, while the other half has constantly nights of darkness. If there are any astronomers in those regions, they would doubtless be tempted to visit the other hemisphere, in order to behold so grand a luminary as we must appear to them. But, pray, do they see the earth under all the changes which the moon exhibits to us ? M7's, B, Exactly so. These changes are called the phases of the moon, and require some explanation. In figure 2, plate XI. let us say that S represents the sun, E the earth, and A BCD the moon in different parts of her orbit. When the moon is at A, her dark side being turned towards the earth, we shall not see her as at a ; but her disappearance is of very short duration, and as she advances in her orbit we perceive her under the form of a new moon ; when she has gone through one-eighth of her orbit at B, one quarter of her en- lightened hemisphere will be turned tow^ards the earth, and she will then appear horned as at b ; when she has performed one quarter of her orbit, she shows us one half of her enlight- ened side as at c ; at c? she is said to be gibbous, and at e the whole of the enlightened side appears to us, and the moon is at full. As she proceeds in her orbit she becomes again gib- bous, and her enlightened hemisphere turns gradually away from us until she completes her orbit and disappears, and then again resumes her form of a new moon. When the moon is at full, or a new moon, she is said to be in conjunction with the sun, as they are then both in the same direction w^ith regard to the earth ; when at her quarters she is said to be in opposition to the sun. Emily* Are not the eclipses produced by the moon pass- ing between the sun and the earth ? Mrs. B. Yes ; when the moon passes between the sun and the earth, she intercepts his rays, or in other words, casts a shadow on the earth, then the sun is eclipsed, and the day- light gives place to darkness, while the moon's shadow is passing over us. When, on the contrary, the earth is between the sun and the moon, it is we who intercept the sun's rays, and cast a shadow on the moon ; the moon is then darkened, she di-s appears from our view, and is eclipsed. Emily. But as the moon goes roynd the earth every 118 ON THE MOON. month, she must be once during that time between the earth and the sun, and the earth must likewise be once between the sun and the moon, and yet we have not a solar and a lunar eclipse every month ? Mrs. B, The orbits of the earth and moon are not exactly parallel, but cross or intersect each other ; and the moon generally passes either above or below the earth when she is in conjunction with the sun, and does not therefore intercept the sun's rays, and produce an eclipse ; for this can take place only when the earth and moon are in conjunction in that part of their orbits which cross each other, (called the nodes of their orbits) because it is then only, that they are both in a right line with the sun. Emily, And a partial eclipse takes place, I suppose, when the moon in passing by the earth, is not sufficiently above or below the earth's shadow entirely to escape it ? Mrs. B. Yes, one edge of her disk then dips into the shadow, and is eclipsed ; but as the earth is larger than the moon, when the eclipse happens precisely at the nodes, they are not only total, but last for some length of time. When the sun is eclipsed, the total darkness is confined to one particular part of the earth, evidently showing that the moon is smaller than the earth, since she cannot entirely skreen it from the sun. In fig. 1. plate XII. you will find a solar eclipse described ; S is the sun, M the moon, and E the earth ; and the moon's shadow, you see, is not large enough to cover the earth. The lunar eclipses on the contrary are visible from every part of the earth, where the moon is above the horizon ; and we discover by the length of time which the moon is in passing through the earth's shadow, that it would be sufficient to eclipse her totally, were she 47 times her actual size ; it follows, therefore, that the earth is 47 times the size of the moon. In fig. 2. S represents the sun, which pours forth rays of light in straight lines in every direction. E is the earth, and M the moon. Now a ray of light coming from one extremity of the sun's disk in the direction A B, will meet another com- ing from the opposite extremity in the direction C B ; the shadow of the earth cannot therefore extend beyond B ; as the sun is larger than the earth, the shadow of the latter is conical, or the figure of a sugar loaf ; it gradually diminishes, and is much smaller than the earth where the moon passes through it, and yet we find the moon to be Bot only totally ON THE MOON. 119 eclipsedj but some length of time in darkness, and hence we are enabled to ascertain its real dimensions. Emily, When the moon eclipses the sun to us, we must be eclipsed to the moon ? Mrs, B. Certainly ; for if the moon intercepts the sun^s raysj and cast a shadow on us, we must necessarily disappear to the moon, but only partially, as in fig. 1. Caroline. There must be a great number of eclipses in the distant planets, which have so many moons ? Mrs. jB. Yes, few days pass without an eclipse taking place ; for among the number of satellites, one or other of them are continually passing either between their planet and the sun, or between the planet and each other. Astrono- mers are so well acquainted with the motion of the planets and their satellites, that they have calculated not only the eclipses of our moon, but those of Jupiter, with such perfect accuracy, that it has afforded a means of ascertaining the longitude. Caroline, But is it not very easy to find both the latitude and longitude of any place by a map or globe ? Mrs, B, If you know where you are situated, there is no difiiculty in ascertaining the latitude or longitude of the place by referring to a map ; but supposing that you had been a length of time at sea, interrupted in your course by storms, a map would afford you very little assistance in discovering where you were. - Caroline, Under such circumstances, I confess I should be equally at a loss to discover either latitude or longitude. Mrs. B, The latitude may be easily found by taking the -altitude of the pole ; that it is to say the number of degrees that it is elevated above the horizon, for the pole appears more elevated as we approach it, and less as we recede from it. Caroline, But unless you can see the pole how can you take its altitude ? Mrs. B. The north pole points constantly towards one particular part of the heavens in which a star is situated, call- ed the Polar Star : this star is visible on clear nights, from every part of the northern hemisphere, the altitude of the polar star, is therefore the same number of degrees as that of the pole ; the latitude may also be determined by observa- tions made on the sun or any of the fixed stars ; the situation therefore of a vessel at sea, with regard to north and south, 120 as THE MOON. is easily ascertained. The difficulty is respecting east and west, that is to say its longitude. As we have no eastern poles from which we can reckon our distance ; some particu- lar spot must be fixed upon for that purpose. The English reckon from the meridian of Greenwich, where the royal observatory is situated ; in French maps you will find that the longitude is reckoned from Paris. The rotation of the earth on its axis in 24 hours from west to east occasions, you know, an apparent motion of the sun and stars in the contrary direction, and the sun appears to go round the earth in the space of 24 hours, passing over fifteen degrees or a twenty-fourth part of the earth's circum- ference every hour ; therefore, when it is twelve o'clock in London, it is one o'clock in any place situated fifteen degrees to the east of London, as the sun must have passed the meri- dian of that place an hour before he reaches that of London. For the same reason it is eleven o'clock to any place situated fifteen degrees to the west of London, as the sun will not come to that meridian till an hour later. If then the captain of a vessel at sea, could know precisely what was thtB hour at London, he could, by looking at his watch, and comparing it w ith the hour of the spot in which he was, ascertain the longitude. Emily, But if he had not altered his watch, since he sail- ed from London, it would indicate the hour it was then in London. Mrs. B. True ; but in order to know the hour of the day of the spot in which he is, the captain of a vessel regulates his watch by th€ sun when it reaches the meridian. Emily, Then if he had two watches, he might keep one regulated daily, and leave the other unaltered ; the former would indicate the hour of the place in which he was situated, and the latter the hour of London ; and by comparing them together, he would be able to calculate his longitude. Mrs, B. You have discovered, Emily, a mode of finding the longitude, which I have the pleasure to tell you, is univer- sally adopted : watches of a superior construction, called chronometers, or time-keepers, are used for this purpose ; but the best watches are liable to imperfections, and should the time-keeper go too fast, or too slow, there would be no means of ascertaining the error ; implicit reliance cannot consequently be placed upon them. Recourse is therefore had to the eclipses of Jupiter's satel- ON THE MOON. 121 lites. A table is made of the precise tinie at which the several moons are eclipsed to a spectator at London ; when they appear eclipsed to a spectator in any other spot, he may, by consulting the table, know what is the hour at London ; for the eclipse is visible at the same moment from whatever place on the earth it is seen. He has then only to look at the watch which points out the hour of the place in which he is, and by observing the difference of time there, and at London, he may immediately determine his longitude. Let us suppose, that a certain moon of Jupiter is always eclipsed at six o'clock in the evening ; and that a man at sea consults his watch, and finds that it is ten o'clock, at night, where he is situated, at the moment the eclipse takes place ; what will be his longitude ? Emily, That is four hours later than in London : four times fifteen degrees makes 60 ; he would, therefore, be sixty degrees east of London, for the sun must have passed his meridian before it reaches that of London. Mrs. B. For this reason the hour is always later than in London, when the place is east longitude, and earlier when it is west longitude. Thus the longitude can be ascertained whenever the eclipses of Jupiter's moons are visible. But it is not only the secondary planets which produce eclipses, for the primary planets near the sun eclipse him to those at a greater distance when they come in conjunction in the nodes of their orbits ; but as the primary planets are much longer in performing their course round the sun, than the satellites in going round their primary planets, these eclipses very seldom occur. Mercury and Venus have how- ever passed in a right line between us and the sun, but being at so great a distance from us, their shadows did not extend so far as the earth ; no darkness was therefore produced on any part of our globe ; but the planet appeared like a small black spot, passing across the sun's disk ; this is called a transit of the planet. It was by the last transit of Venus, that astronomers were enabled to calculate with some degree of accuracy the dis- tance of the earth from the sun, and the dimensions of the latter. Emily. I have heard that the tides are affected by the moon, but I cannot conceive what influence it can have on them. 11 122 ON THE MOON. Mrs. B, They are produced by the moon's attraction , which draws up the waters in a protuberance. Caroline, Does attraction act on water more powerfully than on land ? I should have thought it would have been just the contrary, for land is certainly a more dense body than water ? Mrs, B, Tides do not arise from water being more strong- ly attracted than land, for this certainly is not the case ; but the cohesion of jfluids being much less than that of solid bodies, they more easily yield to the power of gravity, in consequence of which the waters immediately below the moon are drawn up by it in a protuberance, producing a full tide, or what is commonly called high water, at the spot where it happens. So far the theory of the tides is not difficult to understand. Caroline. On the contrary, nothing can be more simple ; the waters, in order to rise up under the moon, must draw the waters from the opposite side of the globe, and occasion ebb-tide, or low water in those parts. Mrs. B. You draw your conclusion rather too hastily, my dear ; for according to your theory, we should have full tide only once in twenty-four hours, that is, every time that we were below the moon, while we find that we have two tides in the course of twenty-four hours, and that it is high water with us and with our antipodes at the same time. Caroline. Yet it must be impossible for the moon to at- tract the sea in opposite parts of the globe, and in opposite directions at the same time. Mrs. B. This opposite tide is rather more difficult to explain, than that which is drawn up beneath the moon ; with a little attention, however, I hope I shall be able to make you understand it. You recollect that the earth and moon are mutually attrac- ted towards a point, their common centre of gravity and of motion ; can you tell me what it is that prevents their meeting and uniting at this point ? Emily. Their projectile force, which gives them a tenden- cy to fly from this centre. Mrs. B. And is hence called their centrifugal force. Now we know that the centrifugal force increases in proportion to the distance from the centre of motion. Caroline. Yes, I recollect your explaining that to us, and illustrating it by the motion of the flyers of a wmd-mill, and the spinning of a top. ON THE MOUN. 123 Emily, And it was but the other day you showed us that bodies weighed less at the equator, than in the polar regions, in consequence of the increased centrifugal force in the equa- torial parts. Mrs, B. Very well. The power of attraction, on the contrary, increases as the distance from the centre of gravity diminishes ; when, therefore, the two centres of gravity and of motion are in the same spot, as is the case with regard to the moon and the earth, the centrifugal power and those of attraction, will be in inverse proportion to each other ; that is to say, where the one is strongest, the other will be weakest. Emily, Those parts of the ocean, then, which are most strongly attracted will have least centrifugal force ; and those parts which are least attracted, will have the greatest centri- fugal force. Mrs, B, In order to render the question more simple, let us suppose the earth to be every where covered by the ocean, as represented in (fig. 3. pi. XII.) M is the moon, A B C D the earth, and X the common centre of gravity and of motion of these two planets. Now the waters on the surface of the earth, about A, being more strongly attracted than any other part, will be elevated ; the attraction of the moon at B and C being less, and at D least of all. But the centrifugal force at D, will be greatest, and the waters there, will in consequence have the greatest tendency to recede from the moon ; the waters at B and C will have less tendency to recede, and at A least of all. The waters, therefore, at D, will recede furthest, at the same time that they are least attracted, and in consequence will be elevated in a protuberance similar to that at A. Emily, The tide A, then, is produced by the moon's at- traction, and increased by the feebleness of the centrifugal power in those parts ; and the tide D is produced by the centrifugal force, and increased by the feebleness of the moon's attraction in those parts. Caroline, And when it is high water at A and D, it is low water at B and C : now I think I comprehend the nature of the tides again, though I confess it is not quite so easy as I at first thought. But, Mrs. B., why does not the sun produce tides as well as the moon ; for its attraction is greater than that of the moon ? Nrs. B, It would be at an equal distance, but our vicini- 124 ON THE ^lOOX. ty to the moon makes her influence more powerful. The sun has, however, a considerable effect on the tides, and increases or diminishes them as it acts in conjunction with, or in oppo- sition to the moon. Etnily. I do not quite understand that. Mrs. B. The moon is a month in going round the earth ; twice during that time, therefore, at full and at change, she is in the same direction as the sun, both then act in conjufiction on the earth, and produce very great tides, called spring tides, as described in fig. 4. at A and B ; but when the moon is at the intermediate parts of her orbit, the sun, instead of afford- ing assistance, weakens her power by acting in opposition to it ; and smaller tides are produced, called neap tides, as rep- resented in fig. 5. Emihj. I have often observed the difference of these tides when I have been at the sea side. But since attraction is mutual between the moon and the earth, we must produce tides in the moon ; and these must be more considerable in proportion as our planet is larger. And 3^et the moon does not appear of an oval form. Mrs. B. You must recollect, that in order to render the explanation of the tides clearer, we suppose the whole sur- face of the earth to be covered with the ocean ; but that is not really the case, either with the earth or the moon, and the land which intersects the water destroys the regularity of the effect. Caroline, True ; we may, however, be certain, that wiienever it is high water the moon is immediately over our heads. Mrs. B. Not so either ; for as a similar effect is produc- ed on that part of the globe immediately beneath the moon, and on that part most distant from it, it cannot be over the heads of the inhabitants of both those situations at the same time. Besides, as the orbit of the moon is very nearly paral- lel to that of the earth, she is never vertical but to the inhab- itants of the torrid zone ; in that climate, therefore, the tides are greatest and they diminish as you recede from it and approach the poles. Caroline. In the torrid zone, then, I hope you will grant that the moon is immediately over, or opposite the spots where it is high water ? Mrs. B. I cannot even admit that ; for the ocean natur- ally partaking of the earth's motion, in its rotation from west ON THE MOO.V. 125 fo east, the moon, in forming a tide, has to contend against the eastern motion of the waves. All matter, you know, by its inertia, makes some resistance to a change of state : the waters, therefore, do not readily yield to the attraction of the moon, and the effect of her influence is not complete till three hours after she has passed the meridian, where it is full tide. Emily, Pray what is the reason that the tide is three- quarters of an hour later every day ? Mrs. B. Because it is twenty-four hours and three-quar- ters before the same meridian on our globe returns beneath the moon. The earth revolves on its axis in about twenty- four hours ; if the moon were stationary, therefore, the same part of our globe would, every twenty-four hours, return beneath the moon ; but as during our daily revolution the moon advances in her orbit, the earth must make more than a complete rotation in order to bring the same meridian opposite the moon : we are three-quarters of an hour in overtaking her. The tides, therefore, are retarded for the same reason that the moon rises later by three-quai'ters of an hour every day. We have now, I think, concluded the observations I had to make to you on the subject of astronomy ; at our next interview, I shall attempt to explain to you the elements of hydrostatics. 11^ CONVERSATION X. ON THE MECHANICAL PROPERTIES OF FLUIDS. Definition of a Fluid ; Distinction between Fluids and Liquids ; Of Non-Elastic Fluids ; Scarcely Susceptible of Cojupression ; Of the Cohesion of Fluids ; Of their Gravitation ; Of their Equilibrium ; Of their Pressure ; Of Specific Gravity ; Of the Specific Gravity of Bodies Heavier than Water ; Of those of the Same Weight as Water ; Of those Lighter than Water ; Of the Specific Gravity of Fluids. MRS. B. We have hitherto eonfined our attention to the mechanical properties of sohd bodies, which have been illustrated, and, I hope, thoroughly impressed upon your memory, by the con- versations we have subsequently had on astronomy. It will now be necessary for me to give you some account of the mechanical properties of fluids — a science which is called hydrostatics. A fluid is a substance which yields to the slightest pressure. If you dip your hand into a basin of water, you are scarcely sensible of meeting with any resistance. Emily, The attraction of cohesion is, then, I suppose, less powerful in fluids than in solids ? Mrs, B. Yes ; fluids, generally speaking, are bodies of less density than solids. From the slight cohesion of the particles of fluids, and the facility with which they slide over each other, it is inferred, that they must be small, smooth, and globular ; smooth, because there appears to be little or no friction among them : and globular, because touching each MECHANICAL PROPERTIES OF FLUID*. 12? Other but by a point would account for the slightness of their cohesion.* Caroline. Pray what is the distinction between a fluid and a Hquid ? Mrs, B* Liquids comprehend only one class of fluids. There is another class distinguished by the name of elastic fluids, or gases, which comprehends the air of the atmosphere, and all the various kinds of air with which you will become acquainted when you study chemistry. Their mechanical properties we shall examine at our next meeting, and confine our attention this morning to those of liquids, or non-elastic fluids. Water, and liquids in general, are scarcely susceptible of being compressed, or squeezed into a smaller space than that which they naturally occupy. This is supposed to be owing to the extreme minuteness of their particles, which, rather than submit to compression, force their way through the pores of the substance which confines them. This was show^n by a celebrated experiment, made at Florence many years ago. A hollow globe of gold was filled with water, and on its being submitted to great pressure, the water was seen to exude through the pores of the gold, which it covered with a fine dew. Fluids gravitate in a more perfect manner than solid bodies ; for the strong cohesive attraction of the parti- cles of the latter in some measure counteracts the efiects of gravity. In this table, for instance, the cohesion of the particles of wood enables four slender legs to support a considerable weight. Were the cohesion destroyed, or, in other words, the wood converted into a fluid, no support could be afforded by the legs, for the particles no longer cohering together, each would press separately and independ- ently, and would be brought to a level with the surface of the earth. Emily, This want of cohesion is then the reason why fluids can never be formed into figures, or maintained in * If the particles of fluids are round, there must be vacant spaces be- tween them, in the same manner as there are vacuities between cannon balls that are piled toj^ether ; between these balls smaller shot may be placed, and between these, others still smaller, or gravel, or sand, may be diffused. In a similar manner, a certain quantity of parfcles of sugar can be taken up in water without increasing its bulk, and when the water has dissolved the sugar, salt may be dissolved in it, and yet the bulk re- main the same ; arid admitting that the particles of water are round, this 33 easily accounted for. 128 MECHANICAL PROPERTIES OF FLUIDS. heaps ; for thougli it is true the wind raises water into waves^^ they are immediately afterwards destroyed by gravity, and water always finds its level. M7S, B, Do you understand what is meant by the level, or equilibrium of fluids ? Emily. I believe I do, though I feel rather at a loss to explain it. Is not a fluid level when its surface is smooth and flat, as is the case with all fluids when in a state of rest ? Mrs. B. Smooth, if you please, but not flat ; for the definition of the equilibrium of a fluid is, that every part of the surface is equally distant from the point to which gravity tends, that is to say, from the centre of the earth ; hence the surface of all fluids must be bulging, not flat, since they will partake of the spherical form of the globe. This is very evi- dent in large bodies of water, such as the ocean, but the sphericity of small bodies of water is so trifling, that their surfaces appear flat. This level, or equilibrium of fluids, is the natural result of dieir particles gravitating independently of each other ; for when any particle of a fl jid accidentally finds itself elevated above the rest, it is attracted down to the level of the surface of the fluid, and the readiness with which fluids yield to the slightest impression, will enable the particle by its weight to penetrate the surface of the fluid and mix with it. Caroline. But I have seen a drop of oil float on the sur- face of water without mixing with it. Mrs. B. That is, because oil is a lighter liquid than wa- ter. If you were to pour water over it, the oil would rise to the surface, being forced up by the superior gravity of the water. Here is an instrument called a water-level, (fig. 1. plate XIII.) which is constructed upon the principle of the equilibrium of fluids. It consists of a short tube, A B, closed at both ends, and containing a little water ; when the tube is not perfectly horizontal the water runs to the lower end, and it is by this means that the level of any situation to which we apply the instrument, is ascertained. Solid bodies you may, therefore, consider as gravitating in masses, for the strong cohesion of their particles makes them weigh altogether, while every particle of a fluid may be con- sidered as composing a separate mass, gravitating independ- ently of each other. Hence the resistance of a fluid is con- siderably less than that of a solid body ; for the resistance of the particles acting separately, they are more easily overcome = .MECHANICAL PROPERTIES OF FLUIDS. 129 Emily. A body of water, in falling, does certainly less injury than a solid body of the same weight. Mrs, B. The particles of fluids acting thus independently, press against each other in every direction, not only down- wards but upwards, and laterally or sideways ; and in conse- quence of this equality of pressure, every particle remains at rest in the fluid. If you agitate the fluid you disturb this equahty of pressure and the fluid will not rest till its equili- brium is restored. Caroline, The pressure downwards is very natural ; it is the eflect of gravity, one particle weighing upon another pres- ses on it ; but the pressure sideways, and particularly the pressure upwards, I cannot understand. Mrs, B, If there were no lateral pressure, water would not run out of an opening on the side of a vessel. If you fill a vessel with sand, it will not run out of such an opening, because there is scarcely any lateral pressure among its particles. Emily, When water runs out of the side of a vessel, is it not owing to the w^eight of the water above the opening ? Mrs, B, If the particles of fluids were arranged in regular columns thus, (fig. 2.) there would be no lateral pressure, for when one particle is perpendicularly above the other, it can only press it downwards ; but as it must continually happen, that a particle presses between two particles beneath, (fig. 3.) these last must sufler a lateral pressure. Emily, The same as when a wedge is driven into a piece of wood, and separates the parts laterally. Mrs. B. Yes. Tlie lateral pressure proceeds, therefore, entirely from the pressure downwards, or the weight of the liquid above ; and consequently the lower the orifice is made in the vessel, the greater will be the velocity of the water rushing out of it. Here is a vessel of water (fig. 4.) with three stop cocks at different heights ; we shall open them, and you w^ill see with what different degrees of velocity the water issues from them. Do you understand this, Caroline?* Caroline, Oh yes. The water from the upper spout receiving but a slight pressure, on account of its vicinity to * An empty bottle Leing corked, and, by means of a weight, let down a certain depth into the sea, it wiil be broken, or the cork will be driven into it by the perpendicular pressure. But a bottle filled with water or any other liquid may be let down to any depth, without damage, because in this case the internal pressure is equal to the externa!. 130 MECHANICAL PROPERTIES OP FLUIDS. the surface, flows but gently ; the second cock having a greater weight above it, the water is forced out with greater velocity, whilst the lowest cock being near the bottom of the vessel, receives the pressure of almost the whole body of water, and rushes out with the greatest impetuosity. Mrs, B» Very well ; and you must observe, that as the lateral pressure is entirely owing to the pressure downwards, it is not effected by the horizontal dimensions of the vessel, which contains the water, but merely by its depth ; for as every particle acts independently of the rest, it is only the column of particles, immediately above the orifice that can weigh upon and press out the water. Emily. The breadth and width of the vessel then can be of no consequence in this respect. The lateral pressure on one side, in a cubical vessel, is, I suppose, not so great as the pressure downwards. Mrs. B. No, in a cubical vessel the pressure downwards will be double the lateral pressure on vne side ; for every particle at the bottom of the vessel is pressed upon by a col- umn of the whole depth of the fluid, whilst the lateral pressure diminishes from the bottom upwards to the surface, where the particles have no pressure. Caroline. And from whence proceeds the pressure of fluids upwards ? that seems to me the most unaccountable, as it is in direct opposition to gravity. Mrs. B. And yet it is a consequence of their pressure downwards. When, for example, you pour water into a tea- pot, the w^ater rises in the spout to a level with the water in the pot. The particles of water at the bottom of the pot are pressed upon by the particles above them ; to this pressure they will yield, if there is any mode of making way for the superior particles, and as they cannot descend, they will change their direction and rise in the spout. Suppose the tea-pot to be filled with columns of particles of water similar to that described in fig. 4. the particle 1 at the bottom will be pressed laterally by the particle 2, and by this pressure be forced into the spout, where, meeting w^ith the particle 3, it presses n upwards and this pressure will be continued, from 3 to 4, from 4 to 5, and so on till the water in the spout has risen to a level with that in the pot. Emilf/. If it were not for this pressure upwards, forcing the water to rise in the spout, the equilibrium of the fluid would be destroved. MECHANICAL PROPERTIES OF FLUIDS. 131 Caroline. True ; but then a tea-pot is wide and large^ and the weight of so great a body of water as the pot will con- tain, may easily force up and support so small a quantity as will fill the spout. But would the same effect be produced if the spout and the pot were of equal dimensions ? Mrs, B. Undoubtedly it would. You may even reverse the experiment by pouring water into the spout, and you will find that the water will rise in the pot to a level with that in the spout; for the pressure of the small quantity of water in the spout will force up and support the larger quantity in the pot. In the pressure upwards, as well as that laterally, you see that the force of pressure depends entirely on the height, and is quite independent of the horizontal dimensions of the fluid. As a tea-pot is not transparent, let us try the experiment by filling this large glass goblet by means of this narrow tube, (fig- 6.) Caroline, Lobit, Emily, as Mrs. B. fills it, how the water rises in the goblet, to maintain an equilibrium with that in the tube. Now, Mrs. B., will you let me fill the tube by pouring water into the goblet ? Mrs. B. That is impossible. However, you may try the experiment, and I doubt not but that you will be able to account for its failure. Caroline. It is very singular, that if so small a column of water as is contained in the tube can force up and support the whole contents of the goblet ; that the weight of all the water in the goblet should not be able to force up the small quantity required to fill the tube : — oh, I see now the reason, the water in the goblet cannot force that in the tube above its level, and as the end of the tube is considerably higher than the goblet, it can never be filled by pouring water into the goblet. Mrs. B. And if you continue to pour water into the gob- let when it is full, the water will run over instead of rising above the level in the tube. I shall now explain to you the meaning of the specific grav^ ity of bodies. Caroline. What ! is there another species of gravity with which we are not yet acquainted ? Mrs. B. No ; the specific gravity of a body, means sim- ply its weight compared with that of another body of the same size. When we say, that substances such as lead and stones 132 MECHANICAL PROPERTIES OF FLUIDS. are heavy, and that others, such as paper and feathers, are light, we speak comparatively ; that is to say, that the first are heavy, and the latter light, in comparison with the general- ity of substances in nature. Would you call w^ood and chalk light or heavy bodies ? Caroline, Some kinds of wood are heavy certainly, as oak and mahogany ; others are light, as deal and box. Emily, I think I should call wood in general a heavy body, for deal and box are light only in comparison to wood of a heavier description. I am at a loss to determine whether chalk should be ranked as a heavy or alight body ; I should be inclined to say the former, if it was not that it is Hghter than most other minerals. I perceive that we have but vague notions of light and heavy. I wish there was some standard of comparison, to which we could refer the weight of all other bodies. Mrs, B, The necessity of such a standard has been so much felt, that a body has been fixed upon for this purpose. What substance do you think would be best calculated to answer this end ? Caroline, It must be one generally known and easily obtained, lead or iron for instance. Mrs, B, All the metals expand by heat, and condense by cold. A piece of lead, let us say a cubic inch for instance, w^ould have less specific gravity in summer than in winter ; for it would be more dense in the latter season. Caroline, But, Mrs. B., if you compare the weight of equal quantities of different bodies, they will all be alike. You know the old saying, that a pound of feathers is as heavy as a pound of lead. Mrs, B, When therefore we compare the weight of differ- ent kinds of bodies, it w^ould be absurd to take quantities of equal weight, we must take quantities of equal bulk ; pints or quarts, not ounces or pounds. Caroline, Very true ; I perplexed myself by thinking that quantity referred to weight, rather than to measure. It is true, it would be as absurd to compare bodies of the same size in order to ascertain which was largest, as to compare bodies of the same weight in order to discover which was heaviest. Mrs. B, In estimating the specific gravity of bodies, therefore, we must compare equal bulks, and we shall find MECHANICAL PROPERTIES OP FLUIDS. 133 that their specific gravity will be proportional to their weights. The body which has been adopted as a standard of refeience is distilled water. Emily* I am surprised that a fluid should have been chos- en for this purpose, as it must necessarily be contained in some vesseij and the weight of the vessel will require to be deducted. Mrs, B, In order to learn the specific gravity of a solid body, it is not necessary to put a certain measure of it in one scale, and an equal measure of water into the other scale : but simply to weigh the body under trial in water. If you weigh a piece of gold in a glass of water, will not the gold displace just as much water, as is equal to its own bulk ? Caroline. Certainly, where one body is, another cannot be at the same time ; so that a sufficient quantity of water must be removed, in order to make way for the gold. Mrs, B. Yes, a cubic inch of water to make room for a cubic inch of gold ; remember that the bulk alone is to be considered, the weight has nothing to do with the quantity of water displaced, for an inch of gold does not occupy more space, and therefore will not displace more water than an inch of ivory, or any other substance, that will sink in water. Well, you will perhaps be surprised to hear that the gold will weigh less in water, than it did out of it. Emily. And for what reason ? Mr5. B. On account of the upward pressure of the par- ticles of water, which in some measure supports the gold, and by so doing, diminishes its weight. If the body immers- ed in water was of the same weight as that fluid, it w^ould be wholly supported by it, just as the water which it displaces was supported previous to its making way for the solid body. If the body is heavier than the water, it cannot be wholly supported by it ; but the water will offer some resistance to its descent. Caroline. And the resistance which water offers to the descent of heavy bodies immersed in it, (since it proceeds from the upward pressure of the particles of the fluid,) must in all cases, I suppose, be the same ? Mrs. B. Yes ; the resistance of the fluid is proportioned to the bulk, and not to the weight of the b dy immersed in it ; all bodies of the same size, therefore, lose the same quantity of their weight in water. Can you form any idea what this loss will be ? 12 134 MECHANICAL TROPERTIES OF FLUIDS. Emily, I should think it would be equal to the weight of the water displaced ; for, since that portion of the water was supported before the immersion of the solid body, an equal weight of the solid body will be supported. Mrs, B, You are perfectly right : a body weighed in water loses just as much of its weight, as is equal to that of the water it displaces ; so that if you were to put the water displaced into the scale to which the body is suspended, it would restore the balance. You must observe, that when you weigh a body in water, in order to ascertain its specific gravity, you must not sink the bason of the balance in the water ; but either suspend the body to a hook at the bottom of the bason, or else take off the bason, and suspend it to the arm of the balance, (fig. 7.) jNow suppose that a cubic inch of gold weighed 19 ounces out of water, and lost one ounce of its weight by being weigh- ed in water, what would be its specific gravity ? Caroline, The cubic inch of water it displaced must weigh that .one ounce ; and as a cubic inch of gold weighs 19 ounces, gold is 19 times as heavy as water. Emily, I recollect having seen a table of the comparative weights of bodies, in which gold appeared to me to be estim- ated at 19 thousand times the weight of water. Mrs, B, You misunderstood the meaning of the table. In the estimation you allude to, the weight of water was reck- oned at 1000. You must observe, that the weight of a sub- stance when not compared to that of any other, is perfectly arbitrary ; and when water is adopted as a standard, we may denominate its weight by any number we please ; but then the weight of all bodies tried by this standard must be signifi- ed by proportional numbers. Caroline, We may call the weight of water, for example, one, and then that of gold would be nineteen ; or if we choose to call the weight of water 1000, that of gold would be 19,000. In short, the specific gravity means how much more a body weighs than an equal bulk of water. Mrs, B, It is rather the weight of a body compared with that of water ; for the specific gravity of many substances is iess than that of water. Caroline, Then you cannot ascertain the specific gravity of such substances in the same manner as that of gold ; for a body that is lighter than water will float on its surface with- out displacing any water. MECHANICAL PROPERTIES OF FLUIDS. 135 Mrs. B, If a body were absolutely light, it is true that it would not displace a drop of water, but the bodies we are treating of have all some weight, however small ; and will therefore, displace some quantity of water. If the body be lighter than water, it will not sink to a level with the surface of the water, and therefore it will not displace so much water as is equal to its bulk ; but it will displace as much as is equal to its weight. A ship, you must have observed, sinks to some depth in water, and the heavier it is laden the deeper it sinks, as it always displaces a quantity of water equal to its weight. Caroline, But you said just now, that in the immersion of gold, the bulk, and not the weight of body, was to be considered. Mrs. B. That is the case with all substances which are heavier than water ; but since those which are lighter do not displace so much as their own bulk, the quantity they displace is not a test of their specific gravit}^ In order to obtain the specific gravity of a body which is lighter than water, you must attach to it a heavy one, whose specific gravity is known, and immerse them together ; the specific gravity of the lighter body may then be easily cal* culated. Emily. But are there not some bodies which have exactly the same specific gravity as v/ater ? Mrs. B. Undoubtedly ; and such bodies will remain at rest in v/hatever situation they are placed in water. Here is a piece of wood which, by being impregnated with a little sand, is rendered precisely of the weight of an equal b ilk of water ; in whatever part of this vessel of water you place it, you will find that it will remain stationary. Caroline. I shall first put it at the bottom ; from thence, of course, it cannot rise, because it is not lighter than w^ater. Now I shall place it in the middle of the vessel ; it neither rises nor sinks, because it is neither lighter nor heavier than the water. Now I will lay it on the surface of the wa- ter ; but there it sinks a little— what is the reason of that. Mrs. B. ? Mrs. B. Since it is not lighter than the water, it cannot float upon its surface ; since it is not heavier than water, it cannot sink below its surface : it will sink therefore, only till the upper surface of both bodies are on a level, so that the piece of wood is just covered with water. If you poured a 136 MECHANICAL PROPERTIES OP FLUIDS . few drops of water into the vessel, (so gently as not to increase their momentum by giving them velocity) they would mix with the water at the surface, and not sink lower. Caroline. This must, no doubt, be the reason why in drawing up a bucket of water out of a well, the bucket feels so much heavier when it rises above the surface of the water in the well ; for whilst you raise it in the water, the water within the bucket being of the same specific gravity as the water on the outside, will be wholly supported by the upward pressure of the water beneath the bucket, and consequently very little force will be required to raise it ; but as soon as the bucket rises to the surface of the well you immediately perceive the increase of weight. Emili/. And how do you ascertain the specific gravity of fluids ? Mrs. B, By means of an instrument called an hydrome- ter, which I will show you. It consists of a thin glass ball A, (fig. 8, plate XIII.) with a graduated tube B, and the specific gravity of the liquid is estimated by the depth to which the instrument sinks in it. There is a smaller ball, C, attached to the instrument below, which contains a little mercury ; but this is merely for the purpose of equipoising the instrument, that it may remain upright in the hquid un- der trial. I must now take leave of you ; bat there remain yet m any observations to be aiade on fluids ; we shall, therefore, re- sume this subject at our next interview. CONVERSATION XL OF SPRINGS, FOUNTAINS, &c. Of the Ascent of Vapor and the Formation of Clouds / Of the Formation and Fall of Rainy Sfc. ; Of the Form-* ation of Springs ; Of Pavers and Lakes ; Of Fountains^ CAROUNE. There is a question I am very desirous of asking you respecting fluids, JMrs. B., which has often perplexed me. What is the reason that the great quantity of rain which falls upon the earth and sinks into it, does not, in the course of time, injure its solidity ? The sun and the wind, I know, dry the surface, but they have no effect on the interior parts j where there must be a prodigious accumulation of moisture. Mrs, B, Do you not know that, in the course of time, all the v/ater which sinks into the ground rises out of it again ? It is the same water which successively forms seas, rivers, springs, clouds, rain, and sometimes hail, snow, and ice. If you will take the trouble of following it through these various changes, you will understand why the earth is not yet drown- ed by the quantity of water which has fallen upon it since its creation ; and you will even be convinced, that it does not contain a single drop more water now, than it did at that period. Let us consider how the clouds were originally formed. When the first rays of the sun warmed the surface of the earth, the heat, by separating the particles of v>^ater, rendered them lighter than the air. This, you know, is the case with steam or vapor. What then ensues ? Caroline. When lighter than the air it will naturally rise ; ^nd now I recollect vour telling us in a preceding les- 12* 138 OF SPRlN^Jb, FOUNTAINS . (IS^C. son, that the heat of the sun transformed the particles of water into vapor, in consequence of which it ascended into the atmosphere, where it formed clouds. Mrs. B. We have then already followed water through two of its transformations ; from water it becomes vapor, and from vapor clouds. Emihj, But since this watery vapor is lighter than the air, why does it not continue to rise ; and why does it unite again to form clouds. Mi^s. B. Because the atmosphere diminishes in density, as it is more distant from the earth. The vapor therefore which the sun causes to exhale, not only from seas, rivers, and lakes, but likewise from the moisture on the land, rises till it reaches a region of air of its own specific gravity ; and there, you know, it will remain stationary. By the frequent accession of fresh vapor it gradually accumulates, so as to form those large bodies of vapor, which we call clouds ; and these, at length, becoming too heavy for the air to support, they fall to the ground. Caroline, They do fall to the ground, certainly, when it rains ; but, according to your theory, I should have im- agined, that when the clouds became too heavy for the region of air in which they were situated to support them, they would descend till they reached a stratum of air of their own weight, and not fall to the earth ; for as clouds are formed of vapor, they cannot be so heavy as the lowest regions of the atmosphere, otherwise the vapor would not have risen. Mrs. B. If you examine the manner in which the clouds descend, it will obviate this objection. In falling, several of the watery particles come within the sphere of each other's attraction, and unite in the form of a drop of water. The vapor, thus transformed into a shower, is heavier than any part of the atmosphere, and consequently descends to the earth. Caroline. How wonderfully curious ! Mrs. B. It is impossible to consider any part of nature attentively without being struck with admiration at the wisdom it displays ; and I hope you will never contemplate these wonders without feeling your heart glow with admiration and gratitude towards their bounteous Author. Observe, that if the waters were never drawn out of the earth, all veg- etation would be destroyed by the excess of moisture ; if, on the other hand, the plants were not nourished and refreshed OP SPRINGS, FOUNTAlNSj SoC. ISP by occasional showers, the drought would be equally fatal to them. If the clouds constantly remain in a state of vapor, they might, as you remarked, descend into a heavier stratum of the atmosphere, but could never fall to the ground ; or were the power of attraction more than sufficient to convert the vapour into drops, it would transform the cloud into a mass of water, which, instead of nourishing, would destroy the produce of the earth. Water then ascends in the form of vapor, and descends in that of rain, snow, or hail, all of which ultimately become water. Some of this falls into the various bodies of water on the surface of the globe, the remainder upon the land. Of the latter, part re-ascends in the form of vapor, part is absorb- ed by the roots of vegetables, and part descends into the bowels of the earth, where it forms springs. Emili/, Is rain and spring-water then the same ? J\hs, B. Yes, originally. The only difference between rain and spring water, consists in the foreign particles which the latter meets with and dissolves in its passage through the various soils it traverses. Caroline. Yet spring water is more pleasant to the taste, appears more transparent, and, I should have supposed^ would have been more pure than rain water. Mrs. B, No ; excepting distilled water, rain water is the most pure we can obtain ; and it is its purity which ren- ders it insipid, whilst the various salts and different ingredi- ents, dissolved in spring water, give it a species of flavor, without in any degree affecting its transparency ; and the filtration it undergoes through gravel and sand in the bowels of the earth, cleanses it from all foreign matter which it has not the povv^er of dissolving. When rain falls on the surface of the earth, it continues m^aking its way downwards through the pores and crevices in the ground. When several drops meet in their subterrane- ous passage, they unite and form a little rivulet : this, in its progress, meets with other rivulets of a similar description and they pursue their course together in the bowels of the earth, till they are stopped by some substance which they cannot penetrate. Caroline, But you said that water could penetrate even the pores of gold, and they cannot meet with a substance more dense ? Mrs. B. But water penetrates the pores of gold only 140 OF SPRINGS, FOUNTAINS, &C. when under a strong compressive force, as in the Florentine experiment ; now in its passage towards the centre of the earth, it is acted upon by no other power than gravit}^, which is not sufficient to make it force its w^ay even through a stra- tum of clay. This species of earth, though not remarkably dense, being of great tenacity, will not admit the particles of water to pass. When w^ater encounters any substance of this nature therefore, its progress is stopped, and the pressure of the accumulating waters forms a bed, or reservoir. This will be more clearly explained by fig. 9. plate XIII. which represents a section, or the interior of a hill or mountain. A, is a body of water such as I have described, whicJi, when filled up as high as B, (by the continual accession of water it receives from the ducts or rivulets a, «, a, «,) finds a passage out of the cavity, and, impelled by gravity, it runs on, till it makes its w^ay out of the ground at the side of the hill, and there forms a spring, C. Caroline. Gravity impels downwards towards the centre of the earth ; and the spring in this figiu'e runs in a horizon- tal direction. Mrs, B. Not entirely. There is some declivity from the reservoir to the spot w^iere the water issues out of the ground ; and gravity you know will bring bodies down an inclined plane, as well as in a perpendicular direction. Caroline, But though the spring may descend on first issuing, it must afterwards rise to reach the surface of the earth ; and that is in direct opposition to gravity. Mrs, B, A spring can never rise above the level of the reservoir whence it issues ; it must, therefore, find a passage to some part of the surface of the earth that is lower or nearer the centre than the reservoir. It is true that, in this figure, the spring rises in its passage from B to C occasionally ; but this, I think, with a little reflection, you will be able to ac- count for. Emily, Oh yes ; it is owing to the pressure of fluids up- wards, and the water rises in the duct upon the same princi- ple as it rises in the spout of a tea-pot ; that is to say, in order to preserve an equilibrium with the water in the reservoir. Now I think I understand the nature of springs ; the water will flow through a duct, whether ascending or descending, provided it never rises higher than the reservoir. Mas. B. Water may thus be conveyed to every part of a town, and to the upper part of the houses, if it is originally ,Fu; J. TLAT£ XDT. Fiq. 2. J *;■:• B '■\^ OF SPRINGS, FOLNTAINSj&C. 141 brought from a height superior to any to which it is convey- ed. Have you never observed, when the pavement of the streets liave been mending, the pipes which serve as ducts for the conveyance of the water through the town ? Emily, Yes, frequently ; and I have remarked that when any of these pipes have been opened, the water rushes up- wards from them with great velocity, which I suppose pro- ceeds from the pressure of the water in the reservoir, which forces it out. Caroline. I recollect having once seen a very curious glass, called Tantalus's cup ; it consists of a goblet, contain- ing a small figure of a man, and whatever quantity of water you pour into the goblet, it never rises higher than the breast of the figure. Do you know how that is contrived ? Mrs, B. It is by means of a syphon, or bent tube, which is concealed in the body of the figure. It rises through one of the legs as high as the breast, and there turning descends through the other leg, and from thence through the foot of the goblet where the water runs out. (fig. 1. plate XIV.) When you pour water into the glass A, it must rise in the syphon B, in proportion as it rises in the glass ; and when the glass is filled to a level with the upper part of the syphon, the water will run out through the other leg of the figure, and will continue running out, as fast as you pour it in ; therefore the glass can never fill any higher. Emilif, I think the new well that has been made at our country-house, must be of that nature. We had a great scar- city of water, and my father has been at considerable expense to dig a well ; after penetrating to a great depth before water could be found, a spring was at length discovered, but the water rose only a few feet above the bottom of the well ; and sometimes it is quite dry. Mrs. B. This has, however, no analogy to Tantalus's cup, but is owing to the very elevated situation of your country-house. Emily, I believe I guess the reason. There cannot be a reservoir of water near the summit of a hill ; as in such a situ- ation there will not be a sufficient number of rivulets formed to supply one ; and without a reservoir, there can be no spring. In such situations, therefore, it is necessary to dig^ very deep, in order to meet with a spring ; and when we give it vent, it can rise only as high as the reservoir from 142 OF SPRINGS J FOUNTAINS, &G. whence it flows, which will be but little, as the reservoir must be situated at some considerable depth below the summit of the hill. Caroline. Your explanation appears very clear and satis- factory. But I can contradict it from experience. At the very top of a hill, near our country-house, there is a large pond, and, according to your theory, it would be impossible there should be springs in such a situation to supply it with water. Then you know that I have crossed the Alps, and I can assure you, that there is a fine lake on the summit of Mount Cenis, the highest mountain we passed over. Mrs, B. Were there a lake on the summit of Mount Blanc, which is the highest of the Alps, it would indeed be wonderful. But that on Mount Cenis, is not at ail contradic-* tory to our theory of springs ; for this mountain is surrounded by others much more elevated, and the springs which feed the lake must descend from reservoirs of water formed in those mountains. This must also be the case with the pond on the top of the hill : there is doubtless some more considerable hill in the neighborhood which supplies it with water. Emily, I comprehend perfectly, why the water in our well never rises high : but I do not understand why it should occasionally be dr3\ Mrs, B. Because the reservoir from which it flows being in an elevated situation, is but scantily supplied with water ; after a long drought, therefore, it may be drained, and the spring dry, till the reservoir be replenished by fresh rains. It is not uncornxUion to see springs flow with great violence in wet weather, and at other times be perfectly dry. Caroline, But there is a spring in our grounds which more frequently flows in dry than in wet weather : how is that to be accounted for ? Mrs, B, The spring probably comes from a reservoir at a great distance, and situated very deep in the ground : it is, therefore, some length of time before the rain reaches the reservoir, and another considerable portion must elapse, whilst the water is making its way from the reservoir to the surface of the earth ; so that the dry weather may probably have succeeded the rains before the spring begins to flow, and the reservoir may be exhausted by the time the wet weather sets in aG*ain. OF SPRINGS, FOUNTAINS, &;C, 143 Caroline. I doubt not but this is the case, as the spring is in a very low situation, therefore the reservoir may be at a great distance from it. Mrs, B* Springs which do not constantly flow, are called intermitting, and are occasioned by the reservoir being im- perfectly supplied. Independently of the situation, this is always the case when the duct or ducts which convey the water into the reservoir are smaller than those which carry it off. Caroline . If it runs out faster than it runs in, it will of course sometimes be empty. And do not rivers also derive their source from springs ? Mrs. B. Yes, they generally take their source in moun- tainous countries, where springs are most abundant. Caroline. I understood you that springs were more rare in elevated situations. Mrs. B. You do not consider that mountainous countries abound equally with high and low situations. Reservoirs of water, which are formed in the bosom of mountains, generally find a vent either on their declivity, or in the valley beneath ; while subterraneous reservoirs formed in a plain, can seldom find a passage to the surface of the earth, but remain con- cealed, unless discovered by digging a well. When a spring once issues at the surface of the earth it continues its course externally, seeking always a lower ground, for it can no longer rise. Emily. Then what is the consequence, if the spring, or I should now rather call it a rivulet, runs into a situation, which is surrounded by higher ground. Mrs. B. Its course is stopped, the water accumulates, and it forms a pool, pond, or lake, according to the dimen- sions of the body of water. The lake of Geneva, in all probability, owes its origin to the Rhone, which passes through it : if, when this river first entered the valley, which now forms the bed of the Lake, it found itself surrounded by high- er grounds, its waters would there accumulate, till they rose to a level with that part of the valley where the Rhone now continues its course beyond the Lake, and from whence it flows through valleys, occasionally forming other small lakes till it reaches the sea. Emily. And are not fountains of the nature of springs ? Mrs. B. Exactly. A fountain is conducted perpendicu- larly upwards, by the spout or adjutage A, through which it 144 OF SPRINGS, FOUNTAINS, &C. flows ; and it will rise nearly as high as the reservoir B, from whence it proceeds. (Plate XIV. figure 2.) Caroline, Why not quite as high ? Mrs. B, Because it meets with resistance from the air in its ascent ; and its motion is impeded by friction against the spoutj where it rushes out. Emily. But if the tube through which the water rises be smooth, can there be any friction ? especially with a fluid whose particles yield to the shghtest impression. Mrs. B. Friction, (as we observed in a former lesson,) may be diminished by polishing, but can never be entirely destroyed ; and though fluids are less susceptible of friction than solid bodies, they are still aflected by it. Another reason why a fountain will not rise so high as its reservoir, is, that as all the particles of water spout from the tube with an equal velocity, and as the pressure of the air upon the exterior particles must diminish their velocity, they will in some degree strike against the under parts, and force them sideways, spreading the column into a head, and rendering it both wider and shorter than it otherwise would be. At our next meeting, we shall examine the mechanical properties of the air, which being an elastic fluid, difters in many respects from liquids. CONVEHSATION XIL ON THE MECHANICAL PROPERTIES OF AIR. Of the Spring or Elasticity of the Air ; Of the weight of the Air ; Experiments icith the Air Pump ; Of the Ba- rometer ; Mode of weighing Air ; Specific Gravity of Air ; Of Pumps ; Description of the Sucking Pump ; Description of the Forcing Pump, MRS. B, At our last meeting we examined the properties of fluids in general, and more particularly of such fluids as are called liquids. There is another class of fluids, distinguished by the name of aeriform or elastic fluids, the principal of which is the air we breathe, which surrounds the earth, and is called the at- mosphere. Emily. There are then other kinds of air, besides the atmosphere ? Mrs, B, Yes ; a great variety ; but they differ only in their chemical, and not in their mechanical properties ; and as it is the latter we are to examine, we shall not at present inquire into their composition, but confine our attention to the mechanical properties of elastic fluids in general. Caroline, And from whence arises this difference ? Mrs, B, There is no attraction of cohesion between the particles of elastic fluids ; so tliat the expansive power of heat has no adversary to contend with but gravity ; any increase of temperature, therefore, expands elastic fluids prodigiously, and a diminution proportionally condenses them. 13 146 MECHANICAL PROPERTIES OF AIR. The most essential point in which air differs from other fluids, is by its spring or elasticity ; that is to say, its power of increasing or diminishing in bulk, according as it is more or less compressed : a power of which I have informed you liquids are almost wholly deprived. Emily. I think I understand the elasticity of the air very well from what you formerly said of it ; (see p. 33.) but what perplexes me is, its having gravity ; if it is heavy and we are surrounded by it, why do we not feel its weight ? Caroline. It must be impossible to be sensible of the weight of such infinitely small particles, as those of which the air is composed : particles which are too small to be seen, must be too light to be felt. Mrs. B. You are mistaken, my dear ; the air is much heavier than you imagine ; it is true, that the particles which compose it are small ; but then, reflect on their quantity : the atmosphere extends to about the distance of 45 miles from the earth ; and its gravity is such, that a man of middling stature is computed (when the air is heaviest) to sustain the weight of about 14 tons. Caroline. Is it possible ! I sliould have thought such a weight would have crushed any one to atoms. Mrs. B. That would, indeed, be the case, if it were not for the equality of the pressure on every part of the body ; but when thus diffused we can bear even a much greater weight, without any considerable inconvenience. In bathing we support the weight and pressure of the water, in addition to that of the atmosphere ; but because this pressure is equally distributed over the body, we are scarcely sensible of it ; whilst if your shoulders, your head, or any particular part of your frame were loaded with the additional weight of a hun- dred pounds you would soon sink under the fatigue. Be- sides this, our bodies contain air, the spring of which counter- balances the weight of the external air, and renders us less sensible of its pressure. Caroline. But if it were possible to relieve me from the weight of the atmosphere, should I not feel more light and agile ? Mrs. B, On the contrary, the air within you meeting with no external pressure to restrain its elasticity, would dis- tend your body, and at length bursting the parts which con- nned it, put a period to your existence. :^1ECHAN1CAL PROPERTrES OF AHl. 1^3 pump. A few strokes of the handle totally excludes the air from the body of the pump, and fills it with water, which, having passed through both the valves, runs out at the spout. Cai^oline. I understand this perfectly. When the piston is elevated, the air and the water successively rise in the pump ; for the same reason as the mercury rises in the ba- rometer. Emily, I thought that water was drawn up into a pump, by suction, in the same manner as water may be sucked through a straw. Mi^s. B. It is so, into the body of the pump ; for the power of suction is no other than that of producing a vacuum over one part of the liquid, into which vacuum the liquid is forced, by the pressure of the atmosphere on another part. The action of sucking through a straw, consists in drawing in and confining the breath, so as to produce a vacuum in the mouth ; in consequence of which, the air within the straw rushes into the mouth, and is followed by the liquid, into which the lower end of the straw is immersed. The princi- ple, you see, is the same ; and the only difference consists in the mode of producing a vacuum. In suction, the muscular powers answer the purpose of the piston and valves. Emily, Water cannot, then, be raised by a pump above 32 feet ; for the pressure of the atmosphere will not sustain a column of water above that height. Mrs, B, I beg your pardon. It is true that there must never be so great a distance as 32 feet from the level of the water in the well, to the valve in the piston, otherwise the water would not rise through that valve ; but when once the water has passed that opening, it is no longer the pressure of air on the reservoir which makes it ascend ; it is raised by lifting it up, as you would raise it in a bucket, of which the piston formed the bottom. This common pump is, therefore, called the sucking, or lifting-pump, as it is constructed on both these principles. There is another sort of pump, called the forcing-pump : it consists of a forcing power added to the sucking part of the pump. This additional power is exactly on the principle of the syringe : by raising the piston you draw the water into the pump, and by descending it you force the water out. Caroline, But the water must be forced out at the upper part of the pump ; and I cannot conceive how that can be hue by descending the piston. 154 MECHANICAL PROPERTIES OF AIR. Mrs, B. Figure 5 plate XIV. will explain the difficulty. The large pipe A B represents the sucking part of the pump, which differs from the lifting-pump, only in its piston P being unfurnished with a valve, in consequence of which the water cannot rise above it. When, therefore, the piston descends, it shuts the valve Y and forces the water (which has no other vent) into the pipe D : this is likewise furnished with a valve V, which, opening outwards, admits the water, but prevents its return. The water is thus first raised in the pump, and then forced into the pipe, by the alternate ascending and descending mo- tion of the piston, after a few strokes of the handle to fill the pipe, from whence the water issues at the spout. It is now time to conclude our lesson. When next we meet, I shall give you some account of wind, and of sound, which will terminate our observations on elastic fluids. Caroline* And I shall run into the garden, to have the pleasure of pumping, now that I understand the construction of a pump. Mrs. -B. And, to-morrow I hope you will be able to tell me; whether it is a forcing or a common lifting pump. MECHANICAL PROPERTIES OF AIR. 149 Mrs. B. Nothing more easy. I shall exhaust the air trom this little bottle by means of the air-pump : and having emptied the bottle of air, or, in other words, produced a va- cuum within it, I secure it by turning this screw adapted to its neck : we may now find the exact weight of this bottle, by putting it into one of the scales of a balance. It weighs you see just two ounces ; but when I turn the screw, so as to admit the air into the bottle, the scale which coYitains it pre- ponderates. Caroline, No doubt, the bottle filled with air^ is heavier than the bottle void of air ; and the additional weight requir- ed to bring the scales again to a balance, must be exactly that of the air which the bottle now contains. Mrs. B. That weight, you see, is almost two grains. The dimensions of this bottle are six cubic inches. Six cubic inches of air, therefore, at the temperature of this room, weighs nearly 2 grains. Caroline. Why do you observe the temperature of the room, in estimating the weight of the air. Mrs. B. Because heat rarifies air, and renders it lighter ; therefore the warmer the air is which you weigh, the lighter it will be. If you should now be desirous of knowing the specific gravity of this air, we need only fill the same bottle with water, and thus obtain the weight of an equal quantity of water — which you see is 1515 grains ; now by comparing the weight of water to that of air we find it to be in the proportion of about 800 to 1. I will show you another instance of the weight of the atmosphere, which I think will please you : you know what a barometer is ? Caroline. It is an instrument which indicates the state of the weather, by means of a tube of quicksilver ; but how, I cannot exactly say. Mrs. B. It is by showing the weight of the atmosphere. The barometer is an instrument extremely simple in its construction : in order that you may understand it, I will show you how it is made. I first fill a glass tube A B/(fig. 3. plate XIV.) about three feet in length, and open only at one end, with mercury ; then stopping the open end with m}^ finger, I immerse it in a cup C, containing a little mercury. Emily. Part of the mercury which was in the tube, I observe, runs down into the cup ; but why does not the whole 13* 1 jO MECHANICAL PROPERTIES OF AlS. of it subside in the cup, for it is contrary to the law of tht cquiUbrium of fluids, that the mercury in the tube should not descend to a level with that in the cup. Mrs. B. The mercury that has fallen from the tube into the cup, has left a vacant space in the upper part of the tube, to which the air cannot gain access ; this space is therefore a perfect vacuum ; and consequently the mercury in the tube is relieved from the pressure of the atmosphere, whilst that in the cup remains exposed to it. Caroline, Oh, now I understand it ; the pressure of the air on die mercury in the cup forces it to rise in the tube, where it sustains no pressure. Emily, Or rather supports the mercury in the tube, and prevents it from falling. Mra. B. That comes to the same thing ; for the power that can support mercury in a vacuum, would also make it ascend when it met with a vacuum. Thus you see, that the equilibrium of the mercury is des- troyed only to preserve the general equilibrium of fluids. Caroline, But this simple apparatus is, in appearance, very unlike a barometer. Mrs, B, It is all that is essential to a barometer. The tube and the cup or vase are fixed on a board, for the con- v^enicnce of suspending it ; the board is graduated for the purpose of ascertaining the height at which the mercury stands in the tube ; and the small moveable metal plate serves to show that height with greater accuracy. Emily, And at what height will the weight of the atmos- phere sustain the mercury ? Mrs, B, About 28 inches, as you will see by this baro- meter ; but it depends upon the weight of the atmosphere, '.vhich varies much according to the state of the weather. The oreater the pressure of the air on the mercury in the cup, the liigher it will ascend in the tube. Now can you tell me whether the air is heavier in wet or dry weather ? Caroline, Without a moment's reflection, the air must be iieaviest in wet weather. It is so depressing, emd makes one ieel so heavy ; while in fine weather, I feel as light as a feather, and as brisk as a bee. Mrs, B, Would it not have been better to have answered with a moment's reflection, Caroline ? It would have convin- •edyou, that the air must be heaviest in dry weather, for it is *hen. that the mercury is found to ri^e in the tube, and conse- MECHANICAL PROPERTIES OF AIR. 151 quently the mercury in the cup must be most pressed by the air : and you know^ that we estimate the dryness and fairness of the weather, by the height of the mercury in the barometer. Cm^oline. Why then does the air feel so heavy in bad weather ? Mrs, B, Because it is less salubrious when impregnated with damp. The lungs under these circumstances do not play so freely, nor does the blood circulate so well : thus obstructions are frequently occasioned in the smaller vessels, from which arise colds, asthmas, agues, fevers, &c. Emily » Since the atmosphere diminishes in density in the upper regions, is not the air more rare upon a hill than in a plain ; and does the barometer indicate this diflerence ? Mrs, B, Certainly. The hills in this country are not suffi- ciently elevated to produce any very considerable effect on the barometer ; but this instrument is so exact in its indications, that it is used for the purpose of measuring the height of moun- tains, and of estimating the elevation of balloons. Emihj, And is no inconvenience experienced from the thinness of the air in such elevated situations ? Mrs, B, Oh, yes ; frequently. It is sometimes oppres- sive, from being insufficient for respiration ; and the expan- sion which takes place in the more dense air contained within the body is often painful : it occasions distension, and some- times causes the bursting of the smaller blood-vessels in the nose and ears. Besides, in such situations, you are more exposed both to heat and cold ; for though the atmosphere is itself transparent, its lower regions abound with vapors and exhalations from the earth, which float in it, and act in some degree as a covering, which preserves us equally from the intensity of the sun's rays, and from the severity of th^ cold. Caroline, Pray, Mrs. B., is not the thermometer con- structed on the same principles as the barometer ? Mrs, B, Not at all. The rise and fall of the fluid in the thermometer is occasioned by the expansive power of heat, and the condensation produced by cold ; the air has no access to it. An explanation of it would, therefore, be irrelevant to our present subject. Emihj, I have been reflecting, that since it is the weight cf the atmosphere which supports the mercury in the tube of a barometer, it would support a column of any other fluid in the ^ame manner, 152 MECHANICAL PROPERTIES OF AIR. Mrs, B. Certainly ; but as mercury is heavier than all other fluids, it will support a higher column of any other fluid ; for two fluids are in equilibrium, when their height varies inversely as their densities. We find the weight of the atmosphere is equal to sustaining a column of water, for instance, of no less than 32 feet above its level. Caroline. The weight of the atmosphere, is then, as great as that of a body of water the depth of 32 feet ? Mrs, B, Precisely ; for a column of air of the height of the atmosphere, is equal to a column of water of 32 feet, or one of mercury of 28 inches. The common pump is constructed on this principle. By the act of pumping, the pressure of the atmosphere is taken off the water, which, in consequence, rises. The body of a pump consists of a large tube or pipe, whose lower end is immersed in the water which it is designed to raise. A kind of stopper, called a piston, is fitted to this tube, and is made to slide up and down it by means of a me- tallic rod fastened to the centre of the piston. Emily, Is it not similar to the syringe, or squirt, with which you first draw in, and then force out water ? Mrs, B, It is ; but you know that we do not wish to force the water out of the pump at the same end of the pipe at which we draw it in. The intention of a pump is to raise water from a spring or well ; the pipe is therefore placed perpendicularly over the water which enters it at the lower extremity, and it issues at a horizontal spout towards the upper part of the pump. The pump, therefore, is rather a more complicated piece of machiner}^ than the syringe. Its various parts are delineated in this figure : (fig. 4. plate XIV.) A B is the pipe or body of the pump, P the piston, V a valve, or little door in the piston, which, opening upwards, admits the water to rise through it, but prevents its returning, and Y a similar valve in the body of the pump. When the pump is in a state of inaction, the two valves are closed by their own weight ; but when, by drawing down the handle of the pump, the piston ascends, it raises a column of air which rested upon it, and produces a vacuum between the piston and the lower valve Y, the air beneath this valve, which is immediately over the surface of the water, conse- quendy expands, and forces its way through it ; the water, then, relieved fyom the pressure of the air, ascends into the MECHANICAL PROPERTIES OF AIR* 14? Caroline. This weight of the atmosphere, then, which I was so apprehensive would crush me, is, in reahty, essen- tial to my preservation. Emily. I once saw a person cupped, and was told that the swelling of the part under the cup was produced by taking away from that part the pressure of the atmosphere ; but I could not understand how this pressure produced such an effect. Mrs, B. The air pump affords us the means of making a great variety of interesting experiments on the weight and pressure of the air : some of them you have already seen. Do you not recollect, that in a vacuum produced within the air pump, substances of various weights fell to the bottom in the same time ; why does not this happen in the atmos- phere ? Caroline, I remember you told us it was owing to the resistance which light bodies meet with from the air during their fall. Mrs. B. Or, in other words, to the support which they received from the air, and which prolonged the time of their fall. Now, if the air were destitute of weight, how could it support other bodies, or retard their fall ? i shall now show you some other experiments, which illustrate, in a striking manner, both the weight and elasticity of air. I shall tie a piece of bladder over this glass receiver, which, you will observe, is open both at the top as well as below. Caroline. Why do you wet the bladder first ? Mrs. B. It expands by wetting, and contracts in drying ; it is also more soft and pliable when wet, so that I can make it fit better, and when dry it will be tighter. We must hold it to the fire in order to dry ; but not too near lest it should burst by sudden contraction. Let us now fix it on the air- pump and exhaust the air from underneath it— you will not be alarmed if you hear a noise ? Emily, It was as loud as the report of a gun, and the bladder is burst ! Pray explain how the air is concerned in this experiment. Mrs. B. It is the effect of the weight of the atmosphere on the upper surface of the bladder, when t had taken away the air from the under surface ; so that there was no longer any re-action to counterbalance the pressure of the atmos- phere on the receiver. You observed how the bladder was 148 MECHANICAL PROPERTIES OF AIR'. pressed inwards by the weight of the external air^ in propor- tion as I exhausted the receiver : and before a complete vacu- um was formed, the bladder, unable to sustain the violence of the pressure, burst with the explosion you have just heard. 1 shall now show you an experiment, which proves the expansion of the air, contained within a body when it is re- lieved from the pressure of the external air. You would not imagine that there was any air contained within this shrivel- led apple, by its appearance ; but take notice of it when placed within a receiver, from which I shall exhaust the air. Caroline, How strange, it grows quite plump, and looks like a fresh-gathered apple. Mrs, B, But as soon as I let the air again into the receiver, the apple you see returns to its shrivelled state. When I took away the pressure of the atmosphere the air within the apple expanded and swelled it out ; but the instant the atmospherical air was restored, the expansion of the internal air was checked and repressed, and the apple shrunk to hs former dimensions. You may make a similar experiment with this little blad- der, which you see is perfectly flaccid and appears to contain no air : in this state I shall tie up the neck of the bladder, so that whatever air remains within it may not escape, and then place it under the receiver. Now observe, as I exhaust the receiver, how the bladder distends ; this proceeds from the great dilatation of the small quantity of air which v/as inclosed within the bladder when I tied it up ; but as soon as I let the air into the receiver, that which the bladder contains, con- denses and shrinks into its small compass within the folds of the bladder. Emily, These experiments are extremely amusing, and they afford clear proofs both of the weight and elasticity of the air ; but I should like to know exactly how much the air weighs. Mrs, B. A column of air reaching to the top of the at- mosphere, and whose base is a square inch, weighs 15lbs. when the air is heaviest ; therefore every square inch of our bodies sustains a weight of 15lbs. : and if you wish to know the weight of the whole of the atmosphere, you must reckon how many square inches there are on the surface of the globe, and multiply them by 15. Emili/, But are there no means of ascertaining the weighi, of a small quantity of air ? CONVERSATION XIIL ON WIND AND SOUND. Of Wind in General; Of the Trade Wind', Of the Periodical Trade Winds ; Of the Aerial Tides ; Of Sounds in General ; Of Sonorous Bodies ; Of Musical Sounds ; Of Concord or Harmony^ and Melody. MRS.B. Well, Caroline, have you ascertained what kind of pump you have in your garden ? Caroline. I think it must be merely a lifting-pump, be- cause no more force is required to raise the handle than is necessary to lift its weight ; and in a forcing-pump, by raising the handle, you force the water into the smaller pipe, and the resistance the water offers must require an exertion of strength to overcome it. Mrs. B. I make no doubt you are right ; for lifting pumps, being simple in their construction, are by far the most common. I have promised to day to give you some account of the nature of wind. Wind is nothing more than the motion of a stream or current of air, generally produced by a partial change of temperature in the atmosphere ; for when any one part is more heated than the rest, that part is rarefied ; the equilibrium is destroyed, and the air in consequence rises. When this happens, there necessarily follows a motion of the surrounding air towards that part, in order to restore it ; this spot, therefore, receives winds from every quarter. Those who live to the north of it experience a north wind ; those to the south, a south wind : — do you comprehend this ? Caroline. Perfectly. But what sort of weather must I'JV ON^WINUANP SOUND. those people have, who live on the spot where these winds meet and interfere ? Mrs, B. They have turbulent and boisterous weather, whirlwinds, hurricanes, rain, lightning, thunder, &c. This stormy weather occurs most frequently in the torrid zone, where the heat is greatest : the air being more rarefied there, than in any other part of the globe, is lighter, and consequent- ly ascends ; whilst the air about the polar regions is contin- ually flowing from the poles to restore the equilibrium. Caroline. This motion of the air would produce a regular and constant north wind to the inhabitants of the northern hemisphere ; and a south wind to those of the southern hemisphere, and continual storms at the equator, where these two adverse winds would meet. Mrs, B, These winds do not meet, for they each change their direction before they reach the equator. The sun, in moving over the equatorial regions from east to west, rarefies the air as it passes, and causes the denser eastern air to flow westwards, in order to restore the equilibrium ; thus producing ti regular east wind about the equator. Caroline, The air from the west, then, constantly goes to meet the sun, and repair the disturbance which his beams have produced in the equilibrium of the atmosphere. But I wonder how you will reconcile these various winds, Mrs. B. : you first led me to suppose there was a constant struggle be- tween opposite winds at the equator producing storm and tempest ; but now I hear of one regular invariable wind, which must naturally be attended by calm weather. Emily, I think I comprehend it : do not these winds from the north and south combine with the easterly wind about the equator, and form what are called the trade-winds ? J rs. B, Just so, my dear. The composition of the two w^inds north and east, produces a constant north-east wind ; and that of the two winds south and east, produces a regular south-east wind : these winds extend to about thirty degrees on each side of the equator, the regions further distant from it experiencing only their respective north and south winds. Caroline, But, Mrs. B., if the air is constantly flowing from the poles to the torrid zone, there must be a deficiency of air in the polar regions ? Mrs, B, The light air about the equator, which expands and rises into the upper regions of the atmosphere, ultimately flows from thence back to the poles, to restore the equilibri- w>N WIND AND SOUND. 157' um : if it were not for this resource^ the polar atmospheric regions would soon be exhausted by the stream of air, which, in the lower strata of the atmosphere, they are constantly sending towards the equator. Caroline, There is then a sort of circulation of air in the atmosphere ; the air in the lower strata flowing from the poles towards the equator, and in the upper strata, flowing back from the equator towards the poles. Mrs. B, Exactly. I can show you an example of this circulation on a small scale. The air of this room being more rarefied than the external air, a wind or current of air is pour- ing in from the crevices of the windows and doors, to restore the equilibrium ; but the light air with which the room is filled must find some vent, in order to make way for the heavy air which enters. If you set the door a-jar, and hold a candle near the upper part of it, you will find that the flame will be blown outwards, showing that there is a current of air flowing out from the upper part of the room. Now place the candle on the floor close by the door, and you will per- ceive, by the inclination of the flame, that there is also a cur- rent of air setting into the room. Caroline, It is just so ; the upper current is the warm light air, which h> driven out to make wa}^ for the stream of cold dense air which enters the room lower down. Emily, I have heard, Mrs, B., that the periodical winds are not so regular on land as at sea : what is the reason of that? Mrs, B, The land reflects into the atmosphere a much greater quantity of the sun's rays than the water ; tlierefore, that part of the atmosphere which is over the land, is more heated and rarefied than that which is over the sea : this occa- sions the wind to set in upon the land, as v/e find that it regu- larly does on the coast of Guinea, and other countries in the torrid zone. Emily, I have heard much of the violent tempests occa- sioned by the breaking up of the monsoons ; are not they ^Iso regular trade-winds ? Mrs, B, They are called periodical trade-winds, as they change their course every half-year. This variation is pro- duced by the earth's annual course round the sun, when the north pole is inclined towards that luminary one half of the year, the south pole the other half. During the summer of the northern hemisphere, the countries of Arabia, Persia. 14 158 ON WIND AND SOUND. India, and China, are much heated, and reflect great quanti' ties of the sun's rays into the atmosphere, by which it becomes extremely rarefied, and the equilibrium consequently destroy- ed. In order to restore it, the air from the equatorial south- ern regions, where it is colder, (as well as from the colder northern parts,) must necessarily have a motion towards those parts. The current of air from the equatorial regions produces the trade-winds for the first six months, in all the seas between the heated continent of Asia, and the equator. The other six months, when it is summer in the southern hemisphere, the ocean and countries towards the southern tropic are most heated, and the air over those parts most rarefied : then the air about the equator alters its course, and flows exactly in an opposite direction. Caroline. This explanation of the monsoons is very curious ; but what does their breaking up mean ? Mrs, B, It is the name given by sailors to the shifting of the periodical winds ; they do not change their course sud- denly, but by degrees, as the sun moves from one hemisphere to the other : this change is usually attended by storms and hurricanes, very dangerous for shipping ; so that those seas are seldom navigated at the season of the equinox. Emily, I think I understand the winds in the torrid zone perfectly well ; but w^hat is it that occasions the great variety of winds which occur in the temperate zones ? for, according to your theory, there should be only north and south winds in those climates. Mrs. B, Since so large a portion of the atmosphere as is over the torrid zone is in continued agitation, these agitations in an elastic fluid, which yields to the slightest impression, must extend every w^ay to a great distance ; the air, therefore, in all climates, will suffer more or less perturbation, according to the situation of the country, the position of mountains, val- leys, and a variety of other causes : hence it is easy to conceive, that almost every climate must be liable to variable winds. On the sea-shore, there is almost always a gentle sea-breeze setting in on the land on a summer's evening, to restore the equilibrium which had been disturbed by reflections from the heated surface of the shore during the day ; and when night has cooled the land, and condensed the air, we generally find it, towards morning, flowing back towards the sea. Caroline. I have observed that the wind, which ever way it blows, almost always falls about sun-set. ON WIND AND SOUND. 159 Mrs. B. Because the rarefaction of air in the particu- lar spot which produces the wind, diminishes as the sun de- chnesj and consequently the velocity of the wind abates. Emily, Since the air is a gravitating fluid, is it not affect- ed by the attraction of the moon and the sun, in the same manner as the waters ? Mrs. B. Undoubtedly ; but the aerial tides are as much greater than those of water, as the density of water exceeds that of air, which, as you may recollect, we found to be about 800 to 1. Caroline. What a prodigious protuberance that must occasion ; How much the weight of such a column of air must raise the mercury in the barometer ! Emily.. As this enormous tide of air is drawn up and supported, as it were by the moon, its weight and pressure, I should suppose, would be rather diminished than increased ? Mrs. B. The weight of the atmosphere is nehher increas- ed nor diminished by the aerial tides. The moon's attraction augments the bulk as much as it diminishes the weight of the column of air ; these effects, therefore, counterbalancing each other, the aerial lldes do not affect the barometer. Caroline. I do not quite understand that. Mrs, B. Let us suppose that the additional bulk of air at high tide raises the barometer one inch ; and on the other hand, that the support which the moon's attraction affords the air diminishes its weight or pressure, so as to occasion the mercury to fall one inch ; under these circumstances the mer- cury must remain stationary. Thus you see, that we can never be sensible of aerial tides by the barometer, on account of the equahty of pressure of the atmosphere, whatever be its height. The existence of aerial tides is not, however, hypothetical ; it is proved by the effect they produce on the apparent posi- tion of the heavenly bodies ; but this I cannot explain to you, till you understand the properties of light. Emily. And when shall we learn them ? Mrs. B. I shall first explain to you the nature of sound, which is intimately connected with that of air ; and I think at our next meeting we may enter upon the subject of optics. We have now considered the effects produced by the wide and extended agitation of the air ; but there is another kind of agitation of which the air is susceptible — a sort of vibratory lOO ON WIND AND SOUND. trembling motion, which, striking on the drum of the ear produces sound. Caroline. Is not sound produced by solid bodies ? The voice of animals, the ringing of bells, musical instruments, are all solid bodies. I know of no sound but that of the wind which is produced by the air. Mrs. B. Sound, I assure you, results from a tremulous motion of the air ; and the sonorous bodies you enumerate,, are merely the instruments by which that peculiar species of motion is communicated to the air. Caroline. What ! when I ring this little bell, is it the air that sounds, and not the bell ? Mrs. B. Both the bell and the air are concerned in the production of sound. But sound, strictly speaking, is a per- ception excited in the mind by the motion of the air on the nerves of the ear ; the air, therefore, as well as the sonorous bodies which put it in motion, is only the cause of sound, the immediate effect is produced by the sense of hearing : for, without this sense, there would be no sound. Emily. I can with difficulty conceive that. A person born deaf, it is true, lias no idea ^£ sound, because he hears none ; yet that does not prevent the real existence of sound, as all those who are not deaf can testify. Mrs. B, I do not doubt the existence of sound to all those who possess the sense of hearing ; but it exists neither in the sonorous body nor in the air, but in the mind of the person whose ear is struck by the vibratory motion of the air, pro- duced by a sonorous body. To convince you that sound does not exist in sonorous bodies, but that air or some other vehicle is necessary to its production, endeavor to ring the little bell, after I have sus- pended it under a receiver in the air-pump, from which I shall exhaust the air Caroline. This is indeed very strange : though I agitate it so violently, it does not produce the least sound. Mrs. B. By exhausting the receiver, I have cut off the communication between the air and the bell ; the latter, therefore, cannot impart its motion to the air. Caroline. Are you sure that it is not the glass, whicli covers the bell, that prevents our hearing it ? Mrs. B. That you may easily ascertain by letting the air into the receiver, and then ringing the belL ON WIND AND SOUND. lOl Caroline. Very true : I can hear it now almost as loud as if the glass did not cover it ; and I can no longer doubt but that air is necessary to the production of sound. Mrs, B. Not absolutely necessary, though by far the most common vehicle of sound. Liquids, as well as air are capa- ble of conveying the vibratory motion of a sonorous body to the organ of hearing ; as sound can be heard under water. Solid bodies also convey sound, as I can soon convince you by a very simple experiment. I shall fasten this string by the middle round the poker ; now raise the poker from the ground by the two ends of the string and hold one to each of your ears : — I shall now strike the poker with a key, and you will find that the sound is conveyed to the ear by means of the strings, in a much more perfect manner than if it had no other vehicle than the air. Caroline. That it is, certainly, for I am almost stunned by the noise. But what is a sonorous body, Mrs. B. ? for all bodies are capable of producing some kind of sound by the motion they communicate to the air. Mrs. B. Those bodies are called sonorous, which produce clear, distinct, regular and durable sounds, such as a bell, a drum, musical strings, wind-instruments, &c. They owe this property to their elasticity ; for an elastic body, after having been struck, not only returns to its former situation, but hav- ing acquired momentum by its velocity, like the pendulum, it springs out on the opposite side. If I draw the string A B, which is made fast at both ends to C, it will not only return to its original position, but proceed onwards to D. This is its first vibration, at the end of which it will retain sufficient velocity to bring it to E, and back again to F which constitutes its second vibration ; the third vibration will carry it only to G and H, and so on till the resistance of the air destroys its motion. The vibration of a sonorous body gives a tremulous motion to the air around it, very similar to the motion communicated to smooth water when a stone is thrown into it. This first produces a small circular wave around the spot in which the stone falls ; the wave spreads, and gradually communicates its motion to the adjacent waters, producing similar waves to a considerable extent. The same kind of waves are produced in the air by the motion of a sonorous body, but with this , difference, that as air is an elastic fluid, the motion does not consist of regularly extending waves, but of vibrations, and 14* i 62 On wind and sound. are composed of a motion forwards and backwards, similar to those of the sonorous body. They differ also in the one taking place in a plane, the other in all directions. The aerial undulations being spherical. Emily, But if the air moves backwards as well as for- wards, how can its motion extend so as to convey sound to a distance. Mrs. B. The first sphere of undulations which are pro- duced immediately around the sonorous body, by pressing against the contiguous air, condenses it. The condensed air, though impelled forward by the pressure, re-acts on the first set of undulations, driving them back again. The second set of undulations v/hich have been put in motion, in their turn communicate their motion, and are themselves driven back by te-action. Thus there is a succession of waves in the air, corresponding with the succession of waves in the water. Caroline. The vibrations of sound must extend much further than the circular weaves in water, since sound is con- veyed to a great distance. Mrs. B. The air is a fluid so much less dense than water, that motion is more easily communicated to it. The report of a cannon produces vibrations of the air which extend to several miles around. Emily. Distant sound takes some time to reach us, since it is produced at the moment the cannon is fired ; and we see the light of the flash long before we hear the report. Mrs. B. The air is immediately put in motion by the firing of a cannon ; but it requires time for the vibrations to extend to any distant spot. The velocity of sound is computed to be at the rate of 1142 feet in a second. Caroline. With what astonishing rapidity the vibrations must be communicated ! But the velocity of sound varies, I suppose, with that of the air which conveys it. If the wind sets towards us from the cannon, we must hear the report sooner than if it set the other way. Mrs. B. The direction of the wind makes less difference in the velocity of sound than you would imagine. If the wind sets from us, it bears most of the aerial waves away and ren- ders the sound fainter ; but it is not very considerably longer in reaching the ear than if the wind blew towards us. This Tmiform velocity of sound enables us to determine the distance of the object from which it proceeds ; as that of a vessel at sea firing a cannon; or that of a thunder cloud. If we do not ON WIND AND SOUND. l6S hear the thunder till half a minute after we see the lightning, we conclude the cloud to be at the distance of six miles and a half. Emily. Pray how is the sound of an echo produced ? Mrs, B. When the aerial vibrations meet with an obsta- cle, having a hard and regular surface^ such as a wall, or rock^ they are reflected back to the ear, and produce the same sound a second time ; but the sound will then appear to proceed from the object by which it is reflected. If the vibrations fall perpendicularly on the obstacle, they are reflected back in the same line ; if obliquely, the sound returns obliquely in the opposite direction, the angle of reflection being equal to the angle of incidence. Caroline, Oh, then, Emily, I now understand why the echo of my voice behind our house is heard so much plainer by you than it is by me, when we stand at the opposite ends of the gravel walk. My voice, or rather, I should say, the vibrations of air it occasions, fall obliquely on the wall of the house, and are reflected by it to the opposite end of the gravel walk. Emily, Very true ; and we have observed that when we stand in the middle of the walk, opposite the house, the echo returns to the person who spoke. Mrs, B, Speaking-trumpets are constructed on the princi- ple of the reflection of sound. The voice, instead of being diflused in the open air, is confined within the trumpet ; and the vibrations which spread and fall against the sides of the instrument, are reflected according to the angle of incidence, and fall into the direction of the vibrations which proceed straight forwards. The whole of the vibrations are thus collected into a focus ; and if the ear be situated in or near that spot, the sound is prodigiously increased. Figure 7. plate XIV. will give you a clearer idea of the speaking-trumpet : the reflected rays are distinguished from those of incidence, by being dotted ; and they are brought to a focus at F. The trumpet used by deaf persons acts on the same principle ; but as the voice enters the trumpet at the large instead of the small end of the instrument, it is not so much confined, nor the sound so much increased. Emily, Are the trumpets used as musical instruments also constructed on this principle ? Mrs, B, So far as their form tends to increase the sound, they are ; but, as a musical instrument, the trumpet becomes 164 ON WIND AND SOUND. itself the sonorous body, which is made to vibrate by blowing into itj and communicates its vibrations to the air. I will attempt to give you in a few words, some notion of the nature of musical sounds, which as you are fond of music must be interesting to you. If a sonorous body be struck in such a manner, that its vibrations are all performed in regular tim.es, the vibrations of the air will correspond with them ; and striking in the same regular manner on the drum of the ear, will produce the same uniform sensation on the auditory nerve and excite the same uniform idea in the mind ; or, in other words, we shall hear one musical tone. But if the vibrations of the sonorous body are irregular, there will necessarily follow a confusion of aerial vibrations ; for a second vibration may commence before the first is finished, meet it half way on its return, interrupt it in its course, and produce harsh jarring sounds which are called discords, Emily. But each set of these irregular vibrations, if repeat- ed at equal intervals, would, I suppose, produce a musical tone ? It is only their irregular succession which makes them interfere, and occasions discord. Mrs, B, Certainly. The quicker a sonorous body vibrates, the more acute^ or sharp, is the sound produced. Caroline, But if I strike any one note of the piano-forte repeatedly, whether quickly or slowly, it always gives the same tone. Mrs, B, Because the vibrations of the same string, at the same degree of tension, are always of a similar duration. The quickness or slowness of the "vibrations relate to the single tones, not to the various sounds which they may compose by succeeding each other. Striking the note in quick succession, produces a more frequent repetition of the tone, but does not increase the velocity of the vibrations of the string. The duration of the vibrations of strings or chords depends upon their length, their thickness or weight, and their degree of tension : thus, you find, the low bass notes are produced by long, thick, loose strings ; and the high treble notes by short, small, and tight strings. Caroline, Then the different length and size of the strings of musical instruments, serves to vary the duration of the vibrations, and consequently, the acuteness of gravity of the notes ? ON WIND AND SOUND. l65 Mrs, B. Yes. Among the variety of tones, there are some whichj sounded together, please the ear, producing what we call harmony, or concord. This arises from the agree- ment of the vibrations of the two sonorous bodies ; so that some of the vibrations of each strike upon the ear at the same time. Thus, if the vibrations of two strings are performed in equal times, the same tone is produced by both, and they are said to be in unison. Emily, Now, then, I understand why, when I tune my harp in unison with the piano-forte, I draw the strings tighter if it is too low, or loosen them if it is at too high a pitch ; it is in order to bring them to vibrate, in equal times, with the strings of the piano-forte. Mrs, B, But concord, you know, is not confined to unison ; for two different tones harmonize in a variety of cases. If the vibrations of one string (or sonorous body whatever) vibrate in double the time of another, the second vibration of the latter will strike upon the ear at the same instant as the first vibration of the former 5 and this is the concord of an octave. If the vibrations of two Strings are as two to three, the second vibration of the first corresponds with the third viura^ tion of the latter, producing the harmony called a fifth. Caroline, So, then, when I strike the key-note with its fifth, I hear every second vibration of one, and every third of the other at the same time ? Mrs, B, Yes ; and the key-note struck with the fourth is likewise a concord, because the vibrations are as three to four. The vibrations of a major third with the key-note, are as four to five ; and those of a minor third, as five to six. There are other tones which, though they cannot be struck together without producing discord, if struck successively, gives us the pleasure which is called melody. Upon these general principles the science of music is founded ; but I am not sufficiently acquainted with it to enter any further into it. We shall now, therefore, take leave of the subject of sound ; and, at our next interview, enter upon that of optics, in which we shall consider the nature of vision, light, an^ colors. CONVERSATION XIV. ON OPTICS. Of Luminous J Transparent^ and Opaque Bodies : Of the Radiation of Light ; Of Shadows ; Of the Reflection of Light ; Opaque Bodies seen only hy Reflected Light ; Fision explained ; Camera Obscura ; Image of Objects on the Retina, CAROUNE. I LONG to begin our lesson to-day, Mrs, B., for I expect that it will be ver}^ entertaining. Mrs, B. Optics is certainly one of the most interesting branches of Natural Philosophy, but not one of the easiest to understand ; I must therefore beg that you will give me the whole of your attention. I shall first inquire, whether you comprehend the meaning of a luminous body^ an opaque body^ and a transparent body. Caroline, A luminous body is one that shines ; an opaque .... Mrs, B. Do not proceed to the second, until we have agreed upon the definition of the first. All bodies that shine are not luminous ; for a luminous body is one that shines by its own light, as the sun, the fire, a candle, &c.* Emily, Polished metal then, when it shines with so much brilliancy, is not a luminous body ? Mrs, B. No, for it would be dark if it did not receive light from a luminous body ; it belongs, therefore, to the class * The direct light of the sun is calculated to be equal to that of 6560 candles, placed at the distance of one foot from the object ; and that of the moon, to the light of one candle at 7 J feet distance ; of Jupiter s.t 1620 feet, and of Venus at 421 fee^. Fi^. 1. PZATE :nr F^. S. ON OPTICS. 167 of opaque or dark bodies, which comprehend all such as are neither luminous nor will admit the light to pass through them. Emily. And transparent bodies, are those which admit the light to pass through them ; such as glass and water ? Mrs, B. You are right. Transparent or pellucid bodies, are frequently called mediums ; and the rays of light which pass through them, are said to be transmitted by them. Light, when emanated from the sun, or any other luminous body, is projected forwards in straight lines in every possible direction ; so that the luminous body is not only the general centre from whence all the rays proceed, but every point of it may be considered as a centre which radiates light in every durection. (fig. 1. plate XV.) Emily, But do not the rays which are projected in differ- ent directions, and cross each other, interfere, and impede each other's course ? Mrs, B, Not at all. The particles of light are so ex- tremely minute, that they are never known to interfere with each other. A ray of light is a single line of light projected from a luminous body ; and a pencil of rays, is a collection of rays, proceeding from any one point of a luminous body, as fig. 2. Caroline, Is light then a substance composed of particles like other bodies ? Mrs, B, This is a disputed point upon which I cannot pretend to decide. In some respects, light is obedient to the laws which govern bodies ; in others it appears to be inde- pendent of them: thus though its corrse is guided by the laws of motion, it does not seem to be influenced by those of gravity. It has never been discovered to have weight, though a variety of interesting experiments have been made with a view of ascertaining that point ; but we are so ignorant of the intimate nature of light, that an attempt to investigate it would lead us into ^ labyrinth of perplexity, if not of error ; we shall therefore confine our attention to those properties of light which are well ascertained. Let us return to the examination of the effects of the radia- tion of light from a luminous body. Since the rays of light are projected in straight lines, when they meet with an opaque body through which they are unable to pass, they are stop- ped short in their course 5 for they cannot move in a curve line round the body. 168 ON OPTICS. Caroline, No, certainly ; for it would require some other force besides that of projection, to produce motion in a curve line. Mrs. B. The interruption of the rays of light, by the opaque body, produces, therefore, darkness on the opposite side of it ; and if this darkness fall upon a wall, a sheet of paper, or any object whatever, it forms a shadow. Emily, A shadow then is nothing more than darkness produced by the intervention of an opaque body, which prevents the rays of light from reaching an object behind the opaque body. Caroline, Why then are shadows of different degrees of darkness ; for I should have supposed from your definition of a shadow, that it would have been perfectly black ? Mrs, B, It frequently happens that a shadow is produced by an opaque body interrupting the course of the rays from one luminous body, while light from another reaches the space where the shadow is formed, in wliich case the shadow- is proportionally fainter. This happens if the opaque body be lighted by two candles : if you extinguish one of them^ the shadow will be both deeper and more distinct. Caroline. But yet it will not be perfectly dark. Mrs. B, Because it is still slightly illumined by light reflected from the walls of the room, and other surrounding objects. You must observe, also, that when a shadow is produced by the interruption of rays from a single luminous body, the darkness is proportional to the intensity of the light. Emily. I should have supposed the contrary ; for as the light reflected from surrounding objects on the shadow, must be in proportion to the intensity of the light, the stronger the light, the more the shadow will be illumined. Mrs. B. Your remark is perfectly just ; but as we have no means of estimating the degrees of light and of darkness but by comparison, the strongest light will appear to produce the deepest shadow. Hence a total eclipse of the sun occa- sions a more sensible darkness than mid-night, as it is imme- diately contrasted with the strong light of noon-day. Caroline. The re-appearance of the sun after an eclipse, must by the same contrast, be remarkably brilliant. Mrs. B. Certainly. There are several things to be ob- served in regard to the form and extent of shadows. If the luminous body A (Jig. 3.) is larger than the opaque body B, ON OPTICS. 169 the shadow will gradually diminish in size, till it terminate in a point. Caroline. This is the case with the shadows of the earth and the moon, as the sun which illumines them, is larger than either of those bodies. And why is it not the case with the shadows of terrestrial objects, which are equally illumined by the sun ? but their shadows, far from diminishing, are always larger than the object, and increase with the distance from it. Mrs. B. In estimating the effect of shadows, we must consider the apparent not the re«/ dimensions of the lumin- ous body ; and in this point of view, the sun is a small object compared wdth the generality of the terrestrial bodies which it illumines : and when the luminous body is less than the opaque body, the shadow will increase with the distance to infinity. All objects, therefore, which are apparently larger than the sun, cast a magnified shadow. This will be best exemplified, by observing the shadow of an object lighted by a candle. Emily, I have often noticed, that the shadow of my fig- ure against the wall, grows larger as it is more distant from me, which is owing, no doubt, to the candle that shines on me being much smaller than m3^self ? Mrs. B. Yes. The shadow of a figure A, (fig. 4.) varies in size, according to the distance of the several surfaces B C D E, on which it is described. Caroline. I have observed, that two candles produce two shadows from_ the same object ; whilst it would appear, from what you said, that they should rather produce only half a iihadow, that is to say, a very faint one. Mrs. B. Th^ number of lights (in different directions) while it decreases the intensity of the shadow, increases their number which always corresponds with that of the lights ; for each light makes the opaque body cast a different shadow, as illustrated by fig. 5. It represents a ball A, lighted by three candles B, C, D, and you observe the light B produces tlie shadow 6, the light C the shadow c, and the light D the shadow d. Emily. I think we now understand the nature of shadows very well ; but pray what becomes of the rays of light which opaque bodies arrest in their course, and the interruption of which is the occasion of shadows ? Mrs. B. Your question leads to a very important property of light, Reflection, When rays of light encounter an opaque 15 170 ON OPTICS. body, which they cannot traverse, part of them are absorbed by it, and part are reflected, and rebound just as an elastic ball which is struck against a wall. Emily, And is light in its reflection governed by the same laws as solid elastic bodies ? Mrs, B, Exactly. If a ray of light fall perpendicularly on an opaque body, it is reflected back in the same line, to- wards the point whence it proceeded. If it fall obliquely, it is reflected obliquely, but in the opposite direction ; the angle of incidence being equal to the angle of reflection. You re- collect that law in mechanics ? Emily, Oh yes, perfectly. Mrs, B, If you will shut the shutters, we shall admit a ray of the sun's light through a very small aperture, and I can show you how it is reflected. I now hold this mirror, so that the ray shall fall perpendicularly upon it. Caroline, I see the ray which falls upon the mirror, but not that which is reflected by it. Mrs. B, Because its reflection is directly retrograde. The ray of incidence and that of reflection both being in the same line, though in opposite directions, are confounded together. Emily, The ray then which appears to us single, is really double, and is composed of the incident ray proceeding to the mirror, and of tl^e reflected ray returning from the mirror. Mrs, B, Exactly so. We shall now separate them by holding the mirror M, (fig. 6.) in such a manner, that the incident ray A B shall fall obliquely upon it — you see the reflected ray B C, is marching ofl' in another direction. If we draw a line from the point of incidence B, perpendicular to the mirror, it will divide the angle of incidence from the angle of reflection, and you will see that they are equal. Emily. Exactly ; and now that you hold the mirror so, that the ray falls more obliquely on it, it is also reflected more obliquely, preserving the equality of the angles of inci- dence and reflection. Mrs, B, It is by reflected rays only that we see opaque objects. Luminous bodies send rays of light immediately to our eyes, but the rays which they send to other bodies are invisible to us, and are seen only when they are reflected or transmitted by those bodies to our eyes. Emily, But have we not just seen the ray of light in it^ tv>^o other rays from the focus, falling on the mirror at B and F ; the dotted linob are perpendicular to those points, and die two rays will thereibre be reflected to A and E. Caroline, Oh, now I understand it clearly. The rays which proceed from a light placed in the focus of a concave mirror fall divergent upon it, and are reflected parallel. It is exactly the reverse of the former experiment, in which the sun's rays fell parallel on the mirror, and were reflected to a focus. Mrs. B, Yes : when the incident rays are parallel, the reflected rays, converge to a focus ; when, on the contrary, the incident rays proceed from the focus, they are reflected parallel. This is an important law of optics, and since you are now acquainted with the principles on which it is founded, I hope that you will not forget it. Caroline, I am sure that we shall not. But, Mrs. B., you said that the image was formed in the focus of a concave mirror ; yet I have frequently seen glass concave mirrors, where the object has been represented within the mirror, in the same manner as in a convex mirror. Mrs, B, That is the case only, when the object is placed between the mirror and its focus ; the image then appears magnified behind, or, as you call it, within the mirror. Caroline, I do not understand why the image should be larger than the object, Mrs. B, It proceeds from the convergent property of the concave mirror. If an object, A B, (fig. 7.) be placed between the mirror and its focus, the rays from its extremities fall divergent on the mirror, and on being reflected, becomes less divergent, as if they proceeded from C : to an eye placed in that situation the image will appear magnified behind the mirror at a 6, since it is seen under a larger angle than the object. You now, I hope, understand the reflection of light by opaque bodies. At our next meeting, we shall enter upon another property of light no less interesting which is called refraction. CONVERSATION XVI. ONREFRACTIOxN AND COLORS. Transmission of Light by Transparent Bodies ; Refrac- tion ; Refraction of the Atmosphere ; Refraction of a Lens ; Refraction of the Frism ; Of the Colors of Rays of Light ; Of the Colors of Bodies, MRS. B. The refraction of light will furnish the subject of to-day's tesson. Caroline, That is a property of which I have not the iaintest idea. Mrs. jB. It is the effect which transparent mediums pro- duce on light in its passage through them. Opaque bodies, you know, reflect the rays, and transparent bodies transmit them ; but it is found, that if a ray, in passing from one medium into another of different density, fall obliquely, it is turned out of its course. Caroline* It must then be acted on by some new power, otherwise it would not deviate from its first direction. Mrs. B, The power which causes the deviation of the ray appears to be the attraction of the denser medium. Let us suppose the two mediums to be air and water ; if a ray of light passes from air into water it is more strongly attracted by the latter on account of its superior density. Emily. In what direction does the water attract the ray ? Mrs. B. It must attract it perpendicularly towards it, in the same manner as gravity acts on bodies. If then a ray A B, (fig. 1. plate XIX.) fall perpendicularly on water, the attraction of the water acts in the same direction as the course of the ray : it will not therefore cause a devia« Fiff. 1. A''- ^ TLATE.Xn: E ]f D Fiq. 4. T«E REFRACTION OF LIGHT. 191 tioiij and the ray will proceed straight on to E. But if it fall obliquely, as the ray C B, the water will attract it out of its course. Let us suppose the ray to have approached the sur- face of a denser medium, and that it there begins to be af- fected by its attraction ; this attraction, if not counteracted by some other power, would draw it perpendicularly to the water, at B ; but it is also impelled by its projectile force, which the attraction of the denser medium cannot overcome ; the ray, therefore, acted on by both these powers, moves in a direction between them, and instead of pursuing its original course to D, or being implicitly guided by the water to E, proceeds towards F, so that the ray appears bent or broken. Caroline, I understand that very well ; and is not this the reason that oars appear bent in water ? Mrs. B, It is owing to the refraction of the rays reflected by the oar ; but this is in passing from a dense to a rare me- dium, for you know that the rays, by means of which you see the oar, pass from water into air, Emily. But I do not understand why a refraction takes place when a ray passes from a dense into a rare medium ; I should suppose that it would be rather less, than more attracted by the latter. Mrs. B. And it is precisely on that account that the ray is refracted. C B, fig. 2. represents a ray passing obliquely from glass into water : glass being the denser medium, the ray will be more strongly attracted by that which it leaves than by that which it enters. The attraction of the glass acts in the direction A B, while the impulse of projection would carry the ray to F ; it moves therefore between these directions towards D. Emily. So that a contrary refraction takes place when a ray passes from a dense into a rare medium. Caroline. But does not the attraction of the denser medium affect the ray before it touches it ? Mrs. B. The distance at which the attraction of the den- ser medium acts upon a ray is so small as to be insensible ; it appears therefore to be refracted only at the point at which it passes from one medium to the other. Now that you understand the principle of refraction, I will show you Jhe refraction of a real ray of light. Do you see the flower painted at the bottom of the inside of this tea-cup ? (Fig. 3.) 102 THE REFRACTION OP LIGHT. Emily. Yes. But now you have moved it just out of sight, the rim of the cup hides it. Mrs. B. Do not stir. I will fill the cup with water, and you will see the flower again. Emily. I do indeed ! Let me try to explain this : when you drew the cup from me so as to conceal the flower, the rays reflected by it no longer met my eyes, but were directed above them ; but now that you have filled the cup with water, they are refracted by the attraction of the water, and bent downwards so as again to enter my eyes. Mrs. B. You have explained it perfectly : Fig. 3. wiir help to imprint it on your memory. You must observe that when the flower becomes visible by the refraction of the ray, 3^ou do not see it in the situation which it really occupies, but an image of the flower higher in the cup ; for as objects always appear to be situated in the direction of the rays which enter the eye, the flower will be seen in the direction of the reflected ray at B. Emily, Then, when we see the bottom of a clear stream of water, the rays which it reflects being refracted in their passage from the water into the air, will make the bottom appear higher than it really is. Mrs. B. And the water will consequently appear more shallow. Accidents have frequently been occasioned by this circumstance ; and boys who are in the habit of bathing should be cautioned not to trust to the apparent shallowness of water, as it will always prove deeper than it appears ; unless, indeed, they view it from a boat on the water, which will enable them to look perpendicularly upon it ; when the rays from the bottom passing perpendicularly, no refraction will take place. The refraction of light prevents our seeing the heavenly bodies in their real situation ; the light they send to us being refracted in passing into the atmosphere, we see the sun and stars in the direction of the refracted ray ; as described in fig. 4. plate XIX., the dotted line represents the extent of the atmosphere, above a portion of the earth, E B E : a ray of light coming from the sun S falls obliquely on it, at A, and is refracted to B : then, since we see the object in the direction of the refracted ray, a spectator at B will see an image of the sun at C, instead of the real object at S. Emily. But if the sun were immediately over our heads, THE REFRACTION OP LIGHT. . 193 it s rays failing perpendiculariy on tlie atmosphere would not be refractedj and we sliould tlien see the real sun, in its true situation. Mi's, B. You must recollect that the sun is vertical only to the inhabitants of the torrid zone ; its rays, thereforCj are always refracted in these climates. There is also anotliier obstacle to our seeing the heavenly bodies in their real situa- tions ; light, though it moves with extreme velocity, is about eight minutes and an half in its passage from the sun to the earth : therefore, when the rays reach us, the siui must have quitted the spot he occupied on their departure ; yet we see him in the direction of those rays, and consequently in a situation wliich he had abandoned eight minutes and an half before. Emily, When you speak of the sun's motion, you mean, I suppose, his apparent motion, produced by the diurnal motion of the earth ? Mrs, B. No doubt ; the eflect being the same, whether it is our earth, or the heavenly bodies which move : it is more easy to represent things as they appear to be, than as the}^ realh" are. Caroline. During the morning, then, when the sun is rising towards the meridian, v/e must (from the length of time the light is in reaching us) see an image of the sun below that spot which it really occupies. Emily. But the refraction of the atmosphere counteract- ing this effect, we may perhaps, between the two, see the sun in its real situation. Caroline. And in the afternoon, when the sun is sinking in the west, refraction and the length of time which the light is in reaching the earth, will conspire to render the image of the sun higher than it really is. Mrs. B. The refraction of the sun's rays by the atmos- phere prolongs our days, as it occasions our seeing an image of the sun both before he rises and after he sets ; for below the horizon, he still shines upon the atmosphere, and his rays are thence refracted to the earth. So likewise we see an image of the sun before he rises, the rays that previously fall upon the atmosphere being reflected to the earth. Caroline. On the other hand we must recollect that light is eight minutes and an half on its journey ; so that, by the time it reaches the earth, the sun may perhaps be risen above the horizon. 17 194 THE REFRACTION OF LIGHT. Emily, Pray, do not glass windows refract the llglit r Mrs, B. They do ; but this refraction is not perceptible, because, in passing through a pane of glass the rays suffer two refractions, wiiich being in contrary directions, produce the same effect as if no refraction had taken place. Emily, I do not understand that. Mrs, B, Fig. 5. plate XIX. will make it clear to you : A A represents a thick pane of glass seen edgeways. When the ray B approaches tlie glass at C, it is refracted by it ; and instead of continuing its course in the same direction, as the dotted line describes, it passes through the pane to D ; at that point returning into the air, it is again refracted by the glass, but in a contrary direction to the first refraction, and in consequence proceeds to E. Now you must observe that the ray B C and the ray D E being parallel, the light does not appear to have suffered any refraction. Emily, So that the effect v/hich takes place on the ray entering the glass, is undone on its quitting it. Or, to express myself more scientifically, when a ray of light passes from one medium into another, and through that into the first again, the two refractions being equal and in opposite directions, no sensible effect is produced. Mr«. B, This is the case when the two surfaces of the refracting medium are parallel to each other ; if they are not, the two refractions may be made in the same direction, as I shall show you. When parallel rays (fig. 6.) fall on a piece of glass having a double convex surface, and which is called a Lens^ that only which falls in the direction of the axis of the lens is perpendicular to the surface ; the other rays falling obUquely are refracted towards the axis, and will meet at a point be- yond the lens called its focus. Of the three rays, ABC, which fall on the lens D E, the rays A and C are refracted in their passage through it, to a, and c, and on quitting the lens they undergo a second refrac- tion in the same direction which unites them with the ray B, at the focufej F. Emily, And what is the distance of the focus from the surface of the lens ? Mrs, B, The focal distance depends both upon the form of the lens, and of the refractive power of the substance of which it is made : in a glass lens, both sides of which are equally convex, the focus is situated nearly at the centre of PLATE XL ON KEFRAC TION AND COLORS. 195 the Sphere of which the surface of the lens forms a portion ; it is at the distance^ therefore, of the radius of the sphere. There are lenses of various forms, as you will find describ- ed in fig. 1. plate XX. The property of those which have a convex surface is to collect the rays of light to a focus ; and of those which have a concave surface, on the contrary, to disperse them. For the rays A C falling on the concave lens X Y, (fig. 7. plate XIX.) instead of converging towards the ray B, which fails on the axis of the lens, will each be attracted tow^ards the thick edges of the lens, both on entering and quitting it, and will, therefore, by the first refraction, be made to diverge to a, r, and by the second to d, e. Caroline, And lenses which have one side flat and the otiier convex or concave, as A and B, fig. 1, plate XX., are, I suppose, less powerful in their refractions ? Mrs, B. Yes ; they are called plano-convex, and plano- concave lenses : the focus of the former is at the distance of the diameter of a sphere, of which the convex surface of the lens forms a portion ; as represented in fig. 2. plate XX. The three parallel rays, ABC, are brought to a focus by the plano-convex lens, X Y at F. I must now explain to you the refraction of a triangular pieceof glass, called a prism. (Fig. 3.) Emily, The three sides of this glass are flat ; it cannot therefore bring the rays to a focus ; nor do I suppose that its refraction will be similar to that of a flat pane of glass, because it has not two sides parallel ; I cannot there- fore conjecture what eflect the rehaction of a prism can produce. Mrs. B, The refractions of the light, on entering and on quitting the prism, are both in the same direction. (Fig. 3.) On entering the prism F, the ray A is refracted from B to C, and on quitting it from C to D. I will show you this in nature ; but for this purpose it will be advisable to close the window-shutters, and admit, through the small aperture, a ray of light, which I shall refract by means of this prism. Caroline, Oh, what beautiful colors are represented on the opposite wall ! There are all the colors of the rainbow, and with a brightness I never saw equalled. (Fig. 4. plate Xa. j Emihj, I have seen an effect, in some respect similar to this, produced by tjie rays of the sun shining upon glass 19G ON REFilACTION AND COLOKS, lustres ; but how is it possible that a piece of wiiite glass cun produce such a variety of brilliant colors ? Mrs. ii. The colors are not formed by the prism, but existed in the ray previous to its refraction. Caroline, Yet^ before its refraction, it appeared perfectly wliite. Mrs, B. The white rays of the sun are composed of colored rays, which, v/hen blended together, appear colorless or white. Sir Isaac Newton., to whom we are indebted for the most important discoveries respecting light and colors, was the first who divided a white ray of light, and found it to consist of an assemblage of colored rays, which formed an image upon the wall, such as you now see exhibited, (fig. 4.) in which are displa3'ed the following series of colors : red, orange, yellow, green, blue, indigo, and violet. Erailij, But how does a prism separate these colored rays ? Mrs, B. By refraction. It appears that the colored rays have different degrees of refrangibility ; in passing through the prism, therefore, they take different directions according to their susceptibility of refraction. The violet rays deviate most from their original course ; they appear at one of the ends of the spectrum A B : contiguous to the violet, are the blue rays, being those which have somewhat less refrangi- bility ; then follow, in succession, the green, yellow, orange, and, lastly, the red, which are the least refrangible of the colored rays. Caroline, I cannot conceive how these colors, mixed together, can become white ? Mrs. B, That I cannot pretend to explain ; but it is a fact that the union of these colors, in the proportions in which they appear in the spectrum, produce in us the idea of white- ness. If you paint a card in compartments with these sevei\ colors, and whirl it rapidly on a pin, it will appear white. But a more decisive proof of the composition of a white ray is afforded by reuniting these colored rays, and forming with them a ray of white light. Caroline, If you can take a ray of white light to pieces, and put it together again, I shall be quite satisfied. Mis, B, This can be done by letting the colored rays, which have been separated by a prism, fall upon a lens, which will converge them to a focus ; and if, when thus reunited, we find that they appear white as they did before ON REFHACTION AND COLOrvS. 197 refractioDj I hope that you will be convinced that the white rays are a compound of the several colored rays. The prism P, 3^ou see, (iig. 5.) separates a ray of white light into seven colored rays, and the lens L L brings them to a focus at F, where they again appear v/hite. Caroline. You succeed to perfection : this is indeed a most interesting and conclusive experiment. Emily. Yet, Mrs. B., I cannot help thinking, that there may perhaps be bat three distinct colors in the spectrum, red, yellovv^, and blue ; and that the four others may consist of two of these colors blended together ; for, in painting, we find that by mixing red and yellovv^, we produce orange ; with different proportions of red and blue, we make violet or any shade of purple ; and yellow and blue form green. Now it is very natural to suppose, that the refraction of a prism may not be so perfect as to separate the colored rays of light completely, and that those which are contiguous in or- der of refrangibility may encroach on each other, and by mix- ing produce the intermediate colors, orange, green, violet, and indigo. Mrs. B. Your observation is, I believe, neither quite wrong, nor quite right. Dr. Wollaston, who has refracted light in a more accurate manner than had been previously done, by receiving a very narrow line of light on a prism, foiuid that it formed a spectrum, consisting of rays of four colors only ; but they were not exactly those you have nam- ed as primitive colors, for the}* consisted of red, green, blue, and violet. A very narrow line of yellow was visi- ble, at the limit of the red and green, which Dr. Wollaston attributed to the overlapping of the edges of the red and green light. Caroline. But red and green mixed together, do not pro- duce yellow ? Mrs. B. Not in painting ; but it may be so in the primi- tive rays of the spectrum. Dr. Wollaston observed that, by increasing the breadth of the aperture by which the line of light was admitted, the space occupied by each colored ray in the spectrum was augmented, in proportion as each por- tion encroached on the neighboring color and mixed with it ; so that the intervention of orange and yellow, between the red and green, is owing, he supposes, to the mixture of these two colors, and the blue is blended on the one side with the green, and on the other with the violet, forming the spectrum 17* 19S uN REFRACTION AND C0L0R3> as it was originally observed by Sir Isaac Ncwloiij and which I have just shown you. The rainbow, which exhibits a series of colors so analo- gous to those of the spectrum, is formed by the refraction of the sun's rays in their passage through a shower of rain, every drop of which acts as a prism, in separating the colored rays as they pass through it. Emily, Pray, Mrs. B., cannot the sun's rays be collected to a focus by a lens in the same manner as they are by a concave mirror ? Mrs. B, No doubt the same effect is produced by the re- fraction of a lens as by the reflection of a concave mirror : in the first, the rays pass through the glass and converge to a focus behind it ; in the latter, they are reflected from the mirror, and brought to a focus before it. A lens, when used for the purpose of collecting the sun's rays, is called a burning glass. The sun now shines veiy bright ; if we let the rays fa!! on this lens you will perceive the focus. Emily, Oh yes : the point of union of the rays is very luminous. I will hold a piece of paper in the focus, and see if it will take fire. The spot of light is extremely brilliant, but the paper does not burn ? Mrs. B. Try a piece of brown paper ; — that you see takes fire almost irnmediatel3\ Caroline. This is surprising : for the light appeared to shine more intensely on the white than on the brown paper. Mrs. B. The lens collects an equal number of rays to a focus, whether you hold the v/hite or the brown paper there ; but the white paper appears more luminous in the focus, be- cause most of the rays, instead of entering into the paper, are leflected by it ; and this is the reason that the paper is not burnt ; whilst, on the contrary, the brown paper, which ab- sorbs more light than it reflects, soon becomes heated and takes fire. Caroline. This is extremely curious ; but why should brown paper absorb more rays than white paper ? Mrs. B. I am far from being able to give a satisfactory answer to that question. We can form but mere conjecture on this point ; and suppose that the tendency to absorb, or reflect rays, depends on the arrangement of the minute parti- cles of the body, and that this diversity of arrangement ren- ders some bodies susceptible of reflecting one colored ray, and absorbing the others ; whilst other bodies have a ten- ON REFRACTION AND COLORS- 199 deiicy to reflect all the colors, and others again j to absorb them all. Emily, And how do you know which colors bodies have a tendency to reflect ; cr which to absorb ? Mrs, B. Because a body always appears to be of the color which it reflects ; for, as we see only by reflected rays^ it can appear but of the color of those rays. Caroline, But we see all bodies of their own natural color, Mrs. B. ; the grass and trees, green ; the sky, blue ; the flowers, of various hues. Mrs, B, True : but why is the grass green ? because it absorbs all except the green rays ; it is therefore these only which the grass and trees reflect to our eyes, and which makes them appear green. The sky and flovv^ers in the same manner, reflect the various colors of which they appear to us ; the rose, the red rays ; the violet, the blue ; the jonquil, the yellow, Szc, Caroline, But these are the permanent colors of the gi'ass and flowers, whether the sun's rays shine on them or not. Mrs, B. Whenever you see those colors, the flowers must be illumined by some light ; and light, from whatever source it proceeds, is of the same nature, composed of the various colored rays, which paint the grass, the flowers, and every colored object in nature. Caroline, But, Mrs. B., the grass is green, and the flow- ers are colored, whether in the dark, or exposed to the light ? Mrs, B, Why should you think so ? Caroline, It cannot be otherwise. Mrs, B, A most philosophical reason indeed ! But, as I never saw them in the dark, you will allow me to dissent from your opinion. Caroline, What color do you suppose them to be, then, in the dark ? Mrs, B, None at all ; or black, which is the same thing. You can never see objects without light. Light is composed of colors, therefore there can be no light without colors ; and though every object is black, or without color in the dark, it becomes colored, as soon as it becomes visible. It is visible, indeed, but by the colored rays which it reflects ; therefore we can see it only when colored. Caroline, All you say seems very true and I know not what to object to it ; yet it appears at the same time i»credi- 200 ON REFRACTION AND COLORS. ble ! What, Mrs. B., are we all as black as negroes, in the dark ? you make me shudder at the thought. Mrs, B. Your vanity need not be alarmed at the idea, as you are certain of never being seen in that slate. Caroline. That is some consolation, undoubtedly ! but what a melancholy reflection it is, that all nature which ap- pears so beautifully diversified with colors should be one uniform mass of blackness ! Mrs. B. Is nature less pleasing for being colored, as well as iliumlned by the rays of light ; and are colors less beautiful, for being accidental, rather than essential properties of bodies ? Providence appears to have decorated nature with the enchanting divei^ity of colors which we so much admire, for the sole purpose of beautifying the scene, and rendering it a source of pleasurable enjoyment : it is an ornament which etnbeliishes nature vvhenever we behold her. What reason is there to regret that she does not w^ar it when she is invisible ? Emihj. I confess, Mrs. B., that I have had my doubts, as well as Caroline, though she has spared me the pains of ex- pressing them ; bat I have just thought of an experiment, which, if it succeeds, will, I am sure, satisfy us both. It is certain, that we cannot see bodies in the dark, to know whether they have then any color. But we may place a colored body in a ray of light, which has been refracted by a prism ; and if your theory is true, the body, of whatever color it naturally is, must appear of the color of the ray in v/hich it is placed ; for since it receives no other colored rays, it can reflect no others. Carolbip,. Oh ! that is an excellent thought, Emily ; will you stand the test, Mrs. B. Mrs. B. I consent : but we must darken the room, and admit only the ray which is to be refracted ; otherwise, the white rays wall be reflected on the body under trial from various parts of the room. With what do you choose to make the experiment ? Caroline. This rose : look at it, Mrs. B., and tell me whether it is possible to deprive it of its beautiful color ? Mrs. B. We shall see. — I expose it first to the red rays, and the flower appears of a more brilliant hue ; but observe the green leaves — Caroline. They appear neither red nor green ; but of a dingy brown with a reddish glow i ON REl RACTiON AND COLORS. 201 Mrs. B* They cannot be green, because they have no green rays to reflect ; neither are they red, because green bodies absorb most of the red rays. But though bodies, from the arrangement of their particles, have a tendency to absorb some rays, and reflect others, yet it is not natural to suppose^ that bodies are so perfectly uniform in their arrangement, as to reflect only pure rays of one color, and perfectly absorb the others ; it is found, on the contrary, that a body reflects, in great abundance, the rays w hich determine its color, and the others in a greater or less degree, in proportion as they are nearer or further from its own color, in the order of refrangi- bility. The green leaves of the rose, therefore, will reflect a few of the red rays, which, blended with their natural black- ness, give them that brown tinge ; if they reflected none of the red rays, they would appear perfectly black. Now I shall hold the rose in the blue rays — Caroline, Oh, Emily, Mrs. B. is right ! look at the rose : it is no longer red, but of a dingy blue color. Emily, This is the most wonderful of any thing we have yet learnt. But, Mrs. B., what is the reason that the green leaves are of a brighter blue than the rose ? Mrs, B, The green leaves reflect both blue and yellow rays, which produces a green color. They are now in a col- ored ray, which they have a tendency to reflect ; they^ therefore, reflect more of the blue ?ays than tlie rose, (which naturally absorbs that color,) and will, of course, appear of a brighter blue. Emihj, Yet, in passing the rose through the different col« ors of the spectrum, the flower takes them more readily than the leaves. Mrs, B, Because the flower is of a paler hue. Bodies which reflect all the rays are white ; those which absorb them all are black : between these extremes, the body appears lighter or darker, in proportion to the quantity of rays they reflect or absorb. This rose is of a pale red : it approaches nearer to white than black ; it therefore reflects rays more abundantly than it absorbs them. Emily, But if a rose has so strong a tendency to reflect rays, I should have imagined that it would be of a deep red color. Mrs, B. I mean to say, that it has a general tendency to reflect rays. Pale-colored bodies reflect all the colored rays to ^ certain degree, which produces their paleness, approach- J02 ON REFRACTION AND COLORS. ing to whiteness ; but one color they reflect more than the rest ; this predominates over the white, and determines the color of the body. Since, then, bodies of a pale color in some degree reflect all the rays of light, in passing through the various colors of the spectrum, they will reflect them all with tolerable brilliancy ; but will appear most vivid in the ray of their natural color. The green leaves, on the contra- ry, are of a dark color, bearing a stronger resemblance to black, than to white ; they have, therefore, a greater tenden- cy to absorb, than to reflect rays ; and reflecting very few of any but the blue and*yellow rays, they will appear dingy in passing through the other colors of the spectrum. Caroline, They must, however, reflect great quantities of the green rays, to produce so deep a color. ^ rs. B, Deepness or darkness of color proceeds rather from a deficiency than an abundance of reflected rays. Re- member that bodies are, of themselves, black ; and if a body reflects only a few green rays, it will appear of a dark green ; it is the brightness and intensity of the color w hich show that a great quantity of rays are reflected. Emily, A white body, then, which reflects all the rays^ will appear equally bright in all the colors of the spectrum. Mrs. B, Certainly ; and this is easily proved by passing a sheet of white paper through the rays of the spectrum. Caroline, What is the reason that blue often appears green by candle-lis^ht ? Mrs. B. The light of a candle is not so pure as that of the sun ; it has a yellowish tinge, and when refracted by the prism, the yellow rays predominate ; and as blue bodies reflect the yellow rays in the next proportion, (being next in order of refransfibility,) the superabundance of yellow rays gives to blue bodies a greenish hue. Caroline, Candle-light must then give to all bodies a yellowish tinge, from the excess of yellow rays ; and yet it is a common remark, that people of a sallow complexion appear fairer or whiter by candle-light. Mrs. B, The yellow cast of their complexion is not so striking, when every object has a yellow tinge. Emily, Pray, w^hy does the sun appear red through a fog? Mrs. B, It is supposed to be owing to the red rays having a greater momentum, which gives them power to traverse so dense an atmosphere. For the same reason, the sun generally appears red at rising and sotting : as the increased quantity ON REFRACTION AND COLORS. 203 of atmosphere^ which the oblique rays must traverse, loaded with the mists and vapors which are usuall}^ formed at those times prevents the other rays from reaching us. Caroline. And, pray, why are the skies of a blue color ? Mrs, B, You should rather say, the atmosphere ; for the sky is a very vague term, the meaning of which it would be difficult to define philosophically. Caroline, But the color of the atmosphere should be white, since all the ra3^s traverse it in their passage to the earth. Mrs. B. Do not forget that we see none of the rays which pass from the sun to the earth, excepting those which meet our eyes ; and this happens only if we look at the sun, and thus intercept the ra3^s, in which case, you know, the sun appears white. The atmosphere is a transparent medium, through which the sun^s rays pass freely to the earth ; but when reflected back into the atmosphere, their momentum is considerably diminished ; and they have not all of them power to traverse it a second time. The momentum of the blue rays is least ; these, therefore, are the most impeded in their return, and are chiefly reflected by the atmosphere : this reflection is performed in every possible direction ; so that whenever we look at the atmosphere, some of these rays fall upon our eyes ; hence we see the air of a blue color. If the atmosphere did not reflect any rays, though the objects on the surface of the earth would be illumined, the skies would appear perfectly black. Caroline. Oh, how melancholy that would be ; and how pernicious to the sight, to be constantly viewing bright objects against a black sky. But what is the reason that bodies often change their color ; as leaves which wither in autumn, or a spot of ink which produces an iron-mould on linen ? Mrs. B. It arises from some chemical change, which takes place in the internal arrangement of the parts, by which they lose their tendency to reflect certain colors, and acquire the power of reflecting others. A withered leaf thus no lon- ger reflects the blue rays ; it appears, therefore, yellow, or has a slight tendency to reflect several rays which produce a dingy brown color. An ink-spot on linen at first absorbs all the rays ; but^ exposed to the air, it undergoes a chemical change, and the spot partially regains its tendency to reflect colors^ but with 204 ON REFRACTION AND COLORS. a preference to reflect the yellow rays^ and such is the color of the iron-mould. Emilij, Bodies, then, far from being of the color which they appear to possess, are of that color which they have the greatest aversion to, w^hich they will not incorporate with, but reject and drive from them. Mrs, B, It certainly is so ; though I scarcely dare ven- ture to advance such an opinion whilst Caroline is contem- plating her beautiful rose. Caroline. My poor rose ! you are not satisfied with depriving it of color, but even make it have an aversion to it ; and I am unable to contradict you. Emily, Since dark bodies absorb more solar rays than light ones, the former should sooner be heated if exposed to the sun ? Mrs, B, And they are found by experience to be so. Have you never observed a black dress to be warmer than a white one ? Emily, Yes, and a white one more dazzling : the black is heated by absorbing the rays, the white dazzling by reflect- ing them. Caroline, And this was the reason that the brown paper was burnt in the focus of the lens, whilst the white paper exhibited the most luminous spot, but did not take fire. Mrs, B, It was so. It is now full time to conclude our lesson. At our next meeting, I shall give you ^ (description of the eye. ^^•<' TLATE TTT t3STERSATI0N XVH. OPTICS. ON THE STRUCTURE OF THE EYE, AND OPTICAL INSTRUMENTS. Description of the Eye ; Of the Image on the Retina ; Refraction of the Humors of the Eye ; Of the Use of Spectacles; Of the Single Microscope ; Of the Double Microscope ; Of the Solar Microscope ; Magic LaU' thorn ; Refracting Telescope ; Refecting Telescope, MRS.B. The body of the eye is of a spherical form : (fig. 1. plate XXL) it has two membranous coverings ; the external one^ a a Oy is called the sclerotica; this has a projection in that part of the eye which is exposed to view, b b, which is called the cornea, because, when dried, it has nearly the consist- ence of very fine horn, and is sufficiently transparent for the light to obtain free passage through it. The second membrane which lines the cornea, and envel- opes the eye, is called the choroid, c c c ; this has an open- ing in front, just beneath the cornea, which forms the pupil, d 5, through which the rays of light pass into the eve. The pupil is surrounded by a colored border, called the" iris, e e, which by its muscular motion, always preserves the pupil of a circular form, whether it is expanded in the dark, or con- tracted by a strong light. This you will understand better by examining fig. 2. Emily. 1 did not know that the pupil was susceptible of varying its dimensions. Mrs, B. The construction of the eye is so admirable, that it is capable of adapting itself, more or less, to the circum- 18 20G OPTICS. stances in which it is placed. In a faint light the pupil di- lates so as to receive an additional quantity of rays, and in a strong light it contracts, in order to prevent the intensity of the light from injuring the optic nerve. Observe Emily's eyes, as she sits looking towards the windows : her pupils appear very small, and the iris large. Now, Emily, turn from the light, and cover your eyes with your hand, so as entirely to exclude it for a few moments. Caroline. How very much the pupils of her eyes are now enlarged, and the iris diminished. This is, no doubt, the reason why the eyes suffer pain, when from darkness they suddenly come into a strong light ; for the pupil being dilated, a quantity of rays must rush in before it has time to contract. Emily, And when we go from a strong light into obscu- rity, we at first imagine ourselves in total darkness ; for a sufficient number of rays cannot gain admittance into the contracted pupil, to enable us to distinguish objects : but in a iew minutes it dilates, and we clearly perceive objects which were before invisible. Mrs. B. It is just so. The choroid c c, is imbued with a black liquor which serves to absorb all the rays that are irregularly reflected, and to convert the body of the eye into a more perfect camera obscura. When the pupil is expand- ed to its utmost extent, it is capable of admitting ten times the quantity of light that it does when most contracted. In cats, and animals which are said to see in the dark, the power of dilatation and contraction of the pupil is still greater : it is computed that their pupils may receive one hundred times more light at one time than at another. Within these coverings of the eye-ball are contained three transparent substances, called humors. The first occupies the space immediately behind the cornea, and is called the aqueous humor, ff^ from its liquidity and its resemblance to w ater. Beyond this is situated the crystalline humor, g g, so called from its clearness and transparency : it has the form of a lens, and refracts the rays of light in a greater de- gree of perfection than any that have been constructed by- art : it is attached by two muscles, m m, to each side of the choroid. The back part of the eye, between the crystalline humor and the retina, is filled by the vitreous humor, h k, which derives its name from a resemblance it is supposed to bear to elass or vitrified substances. OPTICS. 207 The membranous coverings of the eye are intended chiefly for the preservation of the retina, i ?, which is by far the most important part of the eye, as it is that which receives the impression of the objects of sight, and conveys it to the mind. The retina consists of an expansion of the optic nerve, of a most perfect whiteness : it proceeds from the brain, enters the eye, at w, on the side next the nose, and is finely spread over the interior surface of the choroid. The rays of light which enter the eye by the pupil are refracted by the several humors in their passage through them, and unite in a focus on the retina. Caroline. I do not understand the use of these refracting humors : the image of objects is represented in the camera obscura, wdthout any such assistance. IMrs, B. That is true ; but the reoresentation would be much more strong and distinct, if we enlarge the opening of the camera obscura, and received tlie rays into it through a lens. I have told you that rays proceed from bodies in all possi- bFe directions. We must, therefore, consider every part of an object which sends rays to our eyes, as points from which the rays divergfe, as from a centre. Emilf/. These divergent rays, issuing* from a single point, I believe you told us, were called a pencil of rays ? Mrs. B. Yes. Now, divergent rays, on entering the pupil, do not cross each other ; the pupil, however, is suffi- ciently large to admit a small pencil of them ; and these, if not refracted to a focus by the humors, would continue diverg- ing after they had passed the pupil, would fall dispersed upon the retina, and thus the image of a single point would be expanded over a large portion of the retina. The divergent rays from every other point of the object would be spread over a similar extent of space, and would interfere and be confounded with the first ; so that no distinct image could be formed, and the retina would represent total confusion both of figure and color. Fig. 3. represents two pencils of rays issuing from two points of the tree A B, and entering the pupil C, refracted by the crystalline humor D, and forming distinct images of the spot they proceed from, on the retina at a b. Fig. 4. differs from the preceding, merely from not being supplied with a lens ; in consequence of which the pencils of rays are not refracted to a focus, and no distinct na true, that every person would be subject to one of these two defects, if we had it not in our power to increase or diminish the convexity of the crystalline humor, and to project it towards, or draw it back from the object, as circumstances require. In a young well-constructed eye, the two muscles to which the crystalline humor is attached have so perfect a command over it, that the focus of the rays constantly falls on the retina, and an image is formed equally distinct both of distant objects and of those which are near. Caroline, In the eyes of fishes, which are the only eyes I have ever seen separate from the head, the cornea does not protrude, in that part of the eye which is exposed to view. Mrs, B, The cornea of the eye of a iish is not more convex ihan the rest of the ball of the eye ; but to supply this defi- ciency, their crystalline humor is spherical, and refracts the rays so much, that it does not require the assistance of the cornea to bring them to a focus on the retina. Emily, Pray, w^hat is the reason that we cannot see an object distinctly, if we approach it very near to the eye ? Mrs, B, Because the rays fall on the crystalline humor too divergent to be refracted to a focus on the retina ; the confusion, therefore, arising from viewing an object too near the eye, is similar to that which proceeds from a flattened (^rystalline humor ; the rays reach the retina before they are ^^ollected to a focus, {Jig, 4.) If it were not for this imper- '■^ Plate XIII. ? 496. How high may a spring rise ? 497. On what principle does water ascend as well as de- scend in its course, as is often the case, in carrying it by the use of ducts ? 498. How would you explain figure 1, Plate XIV. ? 499. What is the name of the cup made on the principle of this figure ? 500. Why must wells on high land, as on hills, be dug deep in order to be supplied with water r 501. Why do rivers generally have their source in moun- tainous regions ? 502. How was the lake Geneva probably formed ? 503. How would you explain figure 2, Plate XIV. ? QUESTIONS TO CONVERSATION XH. ON THE MECHANICAL PROPERTIES OF AIR. Of the Spring or Elasticity of the Air ; Of the weight of the Air ; Experiments ivith the Air Pump ; Of the Ba- » rometer ; Mode of Weighing Air ; Specific Gravity of\ Air ; Of Pumps ; Description of the Sucking Pump ; Description of the Forcing Pump. 504. How are the fluids called air distinguished from liquids ? 505. What effect does heat have on elastic fluids ? , 506. To what distance from the earth does the atmosphere^) extend ? MECHANICAL PROPERTIES OF AIR. 241 507. What weight of air is a common or middling size man supposed to sustain ? 508. Why does not such a weight crush him to atoms ? 509. What would be the consequence if the weight of external air were removed from us ? 510. Why do not bodies of various weights in the open air fall in the same time ? 511. How may it be shown that the air has weight ? 512. How may the power of expansion in air be ascer* tained ? 513. How much does a column of air reaching to the top of the atmosphere of an inch in diameter, weigh ? 514. How can the weight of a small quantity of air be ascertained ? 515. How much heavier Is water than air ? 516. How can the weight of the atmosphere be determined by a Barometer ? 517. When is the air the heaviest, in wet or in dry weather? 518. But why do our feelings indicate that the air is heaviest in wet weather, if that is not the fact ? 519. Is the atmosphere of the same density on a high hill or mountain as in a valley ? 520. How may the height of mountains be ascertained by R Barometer ? 521. Does a person in such elevated situations feel any inconvenience from the thinness of the atmosphere ? 522. On what principle is the thermometer constructed ? 523. When are two fluids of different density in equili- brium ? 524. What causes water to rise in a pump ? 525. How high will it rise ? 526. What is the construction of a pump ? 527. How would you explain figure 4, Plate XIV. ? 528. On what principle is a liquid sucked through a straw or any small tube ? 529. How would you explain figure 5, Plate XIV. ? 21 QUESTIONS TO CONVERSATION XIII. ON WIND AND SOUND. Of Wind in General ; Of the Trade Wind; Of the Periodical Trade Winds ; Of the Aerial Tides ; Of Sounds in General ; Of Sonorous Bodies ; Of Musical Sounds ; Of Concord or Harmony ^ and Melody, 530. What is wind ? 531. How is the air put in motion so as to produce wind ? 532. What is the consequence where the winds from different quarters meet or interfere ? 533. Where does this mostly happen ? 534. What regular wind prevails at the equator ? 535. Why is there a regular east wind at and near the equator ? ^S6, How are the trade winds^ as they are called^ pro- duced ? bSJ, Why do not the polar regions become exhausted of air, if it is continually blowing from them to the equator ? 538. What familiar illustration or example can you give of the circulation of air — first from the poles to the equator^ and then rising and returning to the poles ? 539. Why are the periodical winds more regular at sea than on land ? 540. What winds are called monsoons ? 541. Why is it that the wind north of the equator does not regularly blow south ; and that on the south of the equator regularly north, according to the above hypothesis, instead of being almost continually variable as they now are ? 542. What are the sea breezes, as they are termed ? 543. Why does the wind generally subside at the going down of the sun ? 544. Does the moon have any effect on the wind ? 545. Is there any difference of weight to a column of atmosphere, when under the influence of the moon's attrac tion. from other times ? ON \V1ND AND SOUND. 243 546. Why is there not ? 547. AVhat produces sound ? 548. How can it be shewn that air is necessary to the pro- duction of sound ? 549. Is the atmosphere the only conductor of sound ? 550. How can it be shewn that solids are conductors of sound ? 551. What bociies are called sonorous ? 552. To what do they owe their sonorous property ? 553. How would you explain figure 6. Plate XIV. ? 554. To what is the tremulous motion given to the air by a sonorous body compared ? 555. W^hy is motion more easily communicated to air than to water ? 556. AVhy do we see the flash of a cannon at a distance, before we hear the report ? 5d7' What is the velocity of sound ? 558. How is the sound of an echo produced ? 559. How is harmony or concord in sounds produced ? 560. How is an octave concord produced ? 561. How is that species of harmony called a fifth pro- duced ? QUESTIONS TO CONVERSATION XIV. OPTICS. Of LinninouSy Transparent^ and Opaque Bodies ; Of the Radiation of Light ; Of Shadoivs ; Of the Reflection of Light ; Opaque Bodies seen only hy Reflected Light ; Vision Explained ; Camera Ohscura ; Image of Objects on the Retina, 562. What is the science called that treats of vision 563. What is a luminous body ? 564. What is an opaque body ? ^6^\ What are transparent bodies ? 244 OPTICS. 566* What are transparent bodies frequently called, wheu spoken of philosophically ? 567' In what manner is light projected from luminous bodies ? 568. Do the rays of light which cross each other impede * each other's course ? 569. Why do they not ? 570. What is a ray of light ? 571. What is a pencil of light ? 572. Is light a substance composed of particles like other bodies ? 573. In what respect is liglit subject to the laws of matter ? 574. In what respect is it not subject to the laws of matter ? 575. What is the consequence when rays of light fall upon an opaque body ? 576. What produces darkness ? 577' What produces a shadow ? 578. Why are shadows of different degrees of darkness ? ^79' When a shadow^ is produced by the interruption of rays of light from a single luminous body, to what is the darkness of the shadow proportioned ? 580. Why does a total eclipse of the sun occasion a mor€ sensible darkness than midnight ? 581. What will be the form of a shadow when the lumin- ous body is larger thra the opaque body upon which it shines ? 582. >Vhat will be the form of the shadow when the opaqup Dod}^ is the largest ? 583. Why is it, that shadows produced by the intervention of terrestrial objects in the sun and moon's light, are of increas- ed size, instead of terminating in a point according to the general principle ? 584. How may more shadows than one be produced by a single opaque body ? 5Sd. What is the reflection of light ? 586. Is all the light that falls upon an opaque body reflected ? 587. How will a ray of light be reflected that falls upon an opaque body perpendicularly ? 588. How will one be reflected that falls upon an opaque body obliquely ? 589. What is the angle of incidence ? 590. What is an angle of reflection ? 501. By what rays do we see opaque bodies ? OPTICS. 245 592. How are we able to see light that falls upon an opaque body and is reflected, but not in a direction to meet the eye ? 593. Why does one side of an opaque body appear to be in the sunshine and the other side in the shade ^ when by not seeing the rays that fall upon the object, both sides of it would appear shaded ? 594. Why is it that the whole of a surface of water on which the sun shines does not appear illumined ? 595. Why is it that objects on a hill appear more distinct than at an equal distance from us in a valley ? 596. How is it that the rays of light shew us or give us an idea of the objects from whiclithey proceed ? 597. What is camera obscura ? 598. How does a camera obscura represent the manner in which objects are pictured upon the retina of the eye ? 599. Why is it that the objects exhibited by a camera obscura are inverted ? 600. When an object is pictured upon the retina of the eye, how is the idea of the object conveyed to the mind ? 601. If objects are seen only by their pictures on the retina of the eye, why do they not appear inverted, as in the camera obscura ? 602. What is the reason that objects appear smaller at a distance than they really are ? 603. What is the a»gle of vision ? 604. What is the size of the angle of vision proportioned to? 605. Why is it that objects of the same size with which we are acquainted are known to be of the same size, if they form pictures of unequal sizes upon the retina of the eye ? 606. Why is it, that objects viewed in front appear larger than when viewed obliquely ? 607. On what principle are the laws of perspective founded ? 608. How is nature to be exhibited in sculpture ? 609. How in painting ? 610. When are objects invisible ? 611. Why is it that the motion of the celestial bodies is invisible ? 612. How would objects appear, as to distance, to a per- son, who had always been blind, on first being made to see ? 613. Why would they seem t© touch the eye ? 21* ,.'40 or TIC.-. 614. If the image of an object is formed on the retina oi each eye, why does not the object appear double ? 61 5. When we see the image of an object in a looking glasSj why does it not appear inverted^ as in the camera obscura ? 616. Explain figure 3, Plate XVII. 617. Why is the ray C D reflected just so as to meet the eye at A. ? 618. Why may we not see ourselves entire in a looking glass, less than half our own length ? 61 9- W^hy cannot persons see their own image in a looking glass, when they stand obliquely to the right or left of the glass ? 620. If you stand obliquely to the right of the glass, why is it that another person must stand just as much to the left of the glass in order to see your image ? 621. W hen you stand at the right of the glass and I stand at the left of it, why does your image appear directly oppo- site yourself ? G22. If all opaque bodies reflect light, why is it, that we cannot as well see ourselves when looking at any other ob- ject, as when viewing a looking glass ? 623. How many kinds of mirrors are there used in optics ? 624. What are they ? 625. How does a convex mirror exhibit an object ? 626. How does a concave mirror ? 627. Vv hat is a focus in optics ? 628. What is an imaginary focus ? 629. Explain figure 1, Plate XVIII. 630. Explain figure 2, Plate XVIII. 631. What is the focus of a concave mirror ? 632. Will the focus be in the same place whether the rays fall parallel or converging upon the mirror ? GSS, Which focus is most distant from the mirror ? 634. Will the focus be in the same place whether the rays fall parallel or diverging upon the mirror ? Go J. Which will be the farthest from the mirror ? 62>6, W^hat are concave mirrors sometimes called ? 637. W^hy are they called burning glasses ? 638. Why does a convex mirror make objects appeal smaller than they are ? 639. If a light is placed in the focus of a concave mirror, how will the rays fall upon the mirror ? ON REFHACTICN AND COLGflS. 247 640. Where must the object be placed in regard to a con- cave mirror in order that it may be magnified ? 641. Why is the image in a concave mirror larger than the object ? QUESTIONS TO CONVERSATION XVL ON REFRACTION AND COLORS. Transmission of Light hy Transparent Bodies ; Refrac- tion ; Refraction of the Atmosphere ; Refraction of a Lens ; Refraction of the Prism ; Of the Colors of Raji^ of Light ; Of the Colors of Bodies. 642. What is the refraction of light ? 643. When does refraction in light take place ? 644. What causes refraction ? 645. Explain the figure 1^ Plate XIX. 646. Why does the ray C. B. descend to F. instead of D. or E. ? 647. Why does a straight stick appear crooked when one end of it is placed obliquely in the water ? 648. Explain figure 2, Plate XIX. 649. Why is it, that water in a river or brook or in any vessel appears more shallow than it really is ? 650. In what situation may we view the bottom of a water, so that it will appear of its real depth ? 651. Do the sun and the other heavenly bodies appear to us in their real situation ? 652. Explain figure 4, Plate XIX. 6ij3, Why do not the sun and the other heavenly bodies appear in their real situation ? 654. In what situation may the sun be seen in its true place ? 655. Wliat besides the refraction of light is there to pre- vent our seeing the sun in its real situation ? 656. How long is light in comhig from the sun to the earth ? ^7 18 ON REFRACTION AND COLORS, Gd7* How is it that our days appear longer than they really are ? 658. Is light refracted in passing through a common win- dow glass ? 659. How would you explain figure 5, Plate XIX. ? 660. Do objects seen through common window glass ap- pear in a different place from that in which they really are ? 661. Why do they not, since they are seen by rays of light that are refracted ? 662. What is a lens ? 663. In parallel rays that fall upon a convex lens, what ones will be refracted ? 664. To what will they be refracted ? 665. What is the axis of a lens ? 666. How would you explain figure 6, Plate XIX. 9 667' What is the distance of the focus from the surface of the lens ? 668. What is the object or property of a convex lens ? 669. W^hat is the object or property of a concave lens ? 670. What is the object of figure 7, Plate XIX. ? 671. What is a radius ? 672. W^hat is a plano-convex lens ? 673. AVhat is a plano-concave lens.^ 674. How would you explain figure 2, Plate XX. ? 675' What is a prism ? 676. How would you explain figure 3, Plate XX. ? 677' Of what do the rays of the sun consist ? 678. How many colors are there in a ray of light ? 679. How can these colors be separated ? 680. What are the colors of a ray of light ? 681. How would you explain figure 4, Plate XX. ? 682. Why do the colors of a ray of light separate in pas- sing throur^h a prism ? 683. Hew can these colors once separated be again united ? 684. What is the object of figure 5, Plate XX. ? 685. What composes white ? 686. What simple ilhistration can be given of these seven colors makirg white on beirg united ? 687. What causes the rainbow ? 688. When is a lens called a burning glass ? 689. Why will a ^'iece of brown paper placed beneath a lens which collects the sun^s rays take fire sooner than a piece of white paper ? OPTICS. 249 690. What colors do different objects reflect and what ones do they absorb ? 691. How do we know, that opaque bodies absorb all the colors, that are not their own, and that they reflect their own and none others ? 692. Are colors essential properties of bodies ? 693. On what do they depend ? 694. To what is darkness of color owing ? 695. Why does blue often appear of a greenish cast by candle hght ? 696. Why are people of a sallow or yellow complexion fairer in the night, if the candle light gives all bodies a yel- lowish tinge ? 697' W^hy does the sun appear red through the clouds ? 698. Why does It appear red in the morning ? 699. Why does the sky appear blue ? 700. Why is a black di'ess warmer than a white one ? 701. Why is a white one more dazzling than a black one ? QUESTIONS TO CONVERSATION XVIL ON THE STRUCTURF^ OF THE EYE AND OPTICAL INSTRUMENTS. Description of the Eye ; Of the Image on the Retina ; Refraction of the Humors of the Eye ; Of the Use of Spectacles ; Of the Single Microscope ; Of the Double Microscope ; Of the Solar Microscope ; Magic Lan- thorn; Refracting Telescope ; Refecting Telescope, 702. What is the form of the body of the eye ? 703. W^hat is the sclerotica of the eye ? 704. What is the cornea of the eye ? 705. What is the choroid of the eye ? 706. What is the pupil of the eye ? 707. What is the iris ? 708. Is the pupil always of the same size ? ,30 OPTICS. 709. When does it enlarge ? 710. When is it contracted ? 711' Why does it give the eyes pain on first going into a bright light from a dark room ? 719., Why does it seem much darker on first going out in the night than after we have been out a short time ? 713. How much more Hght is admitted when the pupil is extended to the utmost, than when most contracted ? 714. Why can cats, horses, and some other animals, see so much better in the night than we can ? 71 ^^ How much is it thought that the pupil of their eyes extend and contract ? 716. What becomes of the rays that fall on the choroid? 717. W^hat are the transparent substances called enclosed within the membraneous coverings ? 718. How many humors are there ? 719. What are they called ? 720. From what does the aqueous humor derive its name ? 721. From what does the chrystalline humor derive its name ? 722. From what does the vitreous humor derive its name? 723. For what are the membraneous coverings of the eye chiefly intended ? 724. Explain figure 1, Plate XXI. 725. What is the us« of the refracting humors ? 726. Explain figure 3, Plate XXI. 727. Explain figure 4, Plate XXI. 728. How does the refracting humor remedy the defects exhibited in figure 4 ? 729. Why is not something like the refracting humors necessary in the camera obscura ? 730. What causes some persons to be short-sighted, as it is termed ? 731. Why can short-sighted persons see better by bringing the objects near to the eyes ? 732. What remedy have short-sighted persons in viewing distant objects ? 733. Explain figure 1, Plate XXII. 734. What is the reason that old people lose their sight ? 735. Explain figure 2, Plate XXII. 736. Why do old persons without convex glasses hold the objects to be seen at a distance from the eye ? QPTICS. 251 737. Why cannot we see distinctly when the object is placed close to the eye ? 738. Explain figure 4, Plate XXII. 739. In what way can objects be seen distinctly when placed near the eye ? 740. What is a microscope ? 741. Explain figure 5^ Plate XXII. 742. How is the magnifying power in the microscope increased ? 743. What is a double microscope? 744. How must an object be placed in regard to a lenS;, so that the object be magnified ? 745. How so that the object be diminished .^ 746. How would you explain Figure 1, Plate XXIII. ? 747. How would you explain Figure 2, Plate XXIII. ? 748. What is the design of Figure 3, Plate XXIII. ? 749. How does a magic lanthorn differ from the double lens and mirror ? 750. What is a magic lanthorn ? 751. What is the design of Figure 4, Plate XXIII. ? 752. How would you explain it ? DIRECTIONS FOR PLACING THE ENGRAVINGS. Plate I. to face page 31 II 49 III 65 IV 61 V 68 VI 78 VII 89 VIII 93 IX 100 X 110 XI 114 XII 118 XIII 128 XIV 141 XV 167 XVI 173 XVII 178 XVIIl 186 XIX 190 XX 195 XXI 205 XXII 209 XXIII 212