COLUMBIA LIBRARIES OFFSITE HEALTH SCIENCES STANDARD HX641 38810 RA823 .C83 The medical report o RECAP Qlnlmnbia Inttr^raitg in tlj? Olil^ at ^m ^avk ^J&tfnmtt ICtbrarg Digitized by tine Internet Arciiive in 2010 witii funding from Open Knowledge Commons (for the Medical Heritage Library project) http://www.archive.org/details/medicalreportofrOOcoun THE MEDICAL REPORT OF THE RICE EXPEDITION TO BRAZIL BY W. T. COUNCILMAN, M.D. AND R. A. LAMBERT, M.D. FROM THE SCHOOL OF TROPICAL MEDICINE HARVARD UNIVERSITY CAMBRIDGE HARVARD UNIVERSITY PRESS LONDON: HUMPHREY MILFORD Oxford University Press 1918 fittt 9i the i-'rcSiUoDi AUG 7- 1918 COPYRIGHT, 1918 HARVARD UNIVERSITY PRESS TO MRS. A. HAMILTON RICE AS AN APPRECIATION OF HER ENDURANCE, PATIENCE, FORTITUDE, AND CHEERFULNESS THIS WORK IS RESPECTFULLY DEDICATED BY THE AUTHORS INTRODUCTION The expedition, primarily undertaken for geographical research, was organized by Doctor A. Hamilton Rice, and left New York on the steam yacht Alberta, Novem- ber 16, 1916. The members of the expedition were Doctor and Mrs. A. H. Rice, Mr. Howe, geologist, Mr. Swanson, wireless operator, Mr. Cousens, engineer, Mr. Church, cartographer, and the writers. Stops were made on the way to and from Brazil at Barbados and at Porto Rico. From Barbados we proceeded on the yacht to Para, to Manaos, and to Iquitos in Peru, returning from there to Manaos. At Manaos a river steamer was taken to San Isabel on the Rio Negro, and from there we proceeded to San Gabriel on a launch which was constructed in New York for this purpose, and sent to Manaos on a commercial steamer. The main purpose of the expedition was the study of the physical geography of the Casiquiare Canal (a natural waterway between the Rio Negro and the Ori- noco River), the branches of this, and the region. This particular region has enjoyed an unenviable reputation from the great numbers, the variety, and the rapacity of the insects, and from the severe character of the endemic diseases. It is also a region which is rarely visited save by the rubber traders and about which little is known. Owing to the unprecedented low water in the Rio Negro it was not possible to go further up than to San Gabriel, where we waited for three weeks in daily expectation of a rise in the river. The river. vi INTRODUCTION however, continued to fall, and reports from higher up were that the canal was not passable even for a large canoe. From San Gabriel the return to Manaos was made on the launch, one of the party only (W. T. C.) coming down the river from San Isabel on a steamer. In the ascent of the Rio Negro the south bank, the usual route, was followed, and the descent to Manaos, which was made in the launch, was to a considerable extent along the north bank, which is little known. Both going and coming stops were made at the small towns and villages, and at many of the rubber estates, and the inhabitants were examined. The prolonged stay at San Gabriel gave a good opportunity for the study of the conditions of the region. From Manaos one of the party (W. T. C.) made a trip on a river steamer through the series of rivers, lakes, and streams on the south of the Amazon between Manaos and the Madeira river. In passing up the Amazon to Iquitos a number of stops were made at the small towns along its banks. In Para, Manaos, and Iquitos the hospitals were visited and the cases in the wards were studied. All of the physicians encountered were most kind, and all medical facilities were freely placed at our disposal. This was in accord with the hospitality shown us everywhere. MEDICAL REPORT OF THE RICE EXPEDITION TO BRAZIL MEDICAL REPORT OF THE RICE EXPEDITION TO BRAZIL The Amazon Valley It is necessary before a consideration of the diseases of this region to give some account of its physical char- acteristics, for the two are closely interlinked. The land of the Amazons, including the great valley and the lower watershed, is in several respects the most remarkable and interesting region on earth. It is the largest area on earth which can be treated as a unit and in which practically the same conditions prevail. There are various estimates of its extent, ranging from 1,500,000 to 2,722,000 square miles, the difference depending upon what are regarded as the limits of the region. The region extends in the west to the Andes, to the high table-lands of the Matto Grosso in the south, to the high lands and the coastal range of mountains on the east, broken only by a few hundred miles at the mouth of the river, and to the mountains of Venezuela and Guiana on the north. The valley itself is almost as flat as the sea. There has been much difficulty in ascertain- ing altitude owing to the influence of atmospheric con- ditions on the barometer. The very careful estimates of Rice made on this expedition give 83 feet at Manaos, and 315 feet at Iquitos, 151 at San Isabel and 225 at San Gabriel. The trade winds sweep across the valley from east to west carrying, in great purple and white cumulus clouds, masses of water vapor, which partly is preci- pitated over the valley in passing, but the height of 3 4 THE RICE EXPEDITION TO BRAZIL discharge is reached on the slopes of the Andes, where the clouds meet the cold air of the mountains.^ A glance at a map shows great numbers of rivers coming from the north and south, which flow into the Amazon, and these become more numerous in the west as the Andes are approached. The volume of water discharged is ^ " The northeast trade winds commence to blow about the Tropic of Cancer, and coming from the quarter thej^ do, they blow obliquelj^ across the Atlantic. Thej' evaporate from the sea as they go; and, impinging at right angles upon the South American shore-line that extends from Cape St. Roque to Cabo La Vela, they carry into the interior the vapor that forms the clouds that give the rain which supplies with water the Mag- dalena, the Orinoco, and the northern tributaries of the Amazon. The volume of water discharged by these rivers into the sea is expres- sive of the quantity which those northeast trade winds take up from the sea, carry in the clouds, and precipitate upon the water-shed that is drained by these streams. They are but pipes and gutters which Nature has placed under the eaves of the great water-shed that has the Andes for a ridge-pole, the Caribbean sea and North Atlantic for a cistern. The trade-wind region of the North Atlantic affords the water-surface where the evaporation is carried on that supplies with rains, dews, and moisture. New Granada, Venezuela, the three Guianas, and the Atlantic slopes of Ecuador. On the other hand, the southeast trade winds commence to blow about the parallel of 30° or 35° south. They, too, come obliquely across the Atlantic, and strike perpendicularly upon the South American coast-line which extends from Cape St. Roque towards Cape Horn. They pass into the interior with their whole load of moisture, every drop of which is wrung from them before they cross the Andes. The quantity of moisture which is taken up from the sea and rained down upon this wonderfully fruitful country may be seen in what the La Plata and the Amazon dis- charge back into the ocean. Now, there is no tropical country in the world which has to windward, and so exactly to windward of it, such an extent of ocean in the trade-wind region. Consequently there is no inter-tropical country in the world that is so finely watered as is this great Amazon country of South America. Along the Atlantic coast of the LTnited States, along the coast of China, and the east coast of New Holland, the land trends along with the direction of the trade winds of those regions. These winds, with their moisture, travel along parallel with the land. They do not blow perpendicularly upon it, nor push their vapors right across it into the interior, as they do in South America. The consequence is, none of those inter-tropical countries can boast of streams and water-courses like those of South America." — " The Amazon," and " The Atlantic Slopes of South America," by M. F. Maury, LL.D., Lieutenant U. S. Navy. MEDICAL REPORT 5 enormous. Leaving out of consideration that of the Para estuary which receives the Tocantins and several smaller rivers, the discharge of the Amazon proper is greater than that of the Mississippi and Nile combined, the great flood converting the ocean into a fresh water sea for one hundred and fifty miles from the coast. This statement is based on estimates made of the outflow at Obidos, where the river bed is constricted between high terra firme to a width variously estimated at one and one and a half miles. Wallace made his estimate of the discharge, 750,000 cubic feet per second, by taking an average depth of fifty feet, a width of one mile, and a current of four miles an hour. Herndon, however, has made soundings here, showing depths of one hundred and fifty, one hundred and seventy, two hundred and ten and two hundred and forty feet, and the great rivers, Tapajos and Xingu, enter the Amazon stream below Obidos. Wallace has also estimated the rainfall of the valley and finds that the estimated rainfall 1,500,000 feet per second corresponds with the estimated discharge estimating the evaporation at one-half the rainfall.^ The color of the Amazon is a pale cloudy yellow; the color is due to a finely divided silt which precipitates slowly and imperfectly. Many of the tributary streams have the same character, while others are clear and of various shades of amber, and these are known as the black water rivers, -the best type being the Rio Negro.^ The height of the land along the river varies, being much lower in certain places, and has received in relation 1 Estimates play a predominating part in all descriptions of the phj^sical features of South America. 2 " Soon afterwards we discovered a river, on the left hand, with water as black as ink, the force of wliich was so great that for more than twenty leagues its waters flowed separately, without mingling with the Amazons river." - — Orellana, 1539. 6 THE RICE EXPEDITION TO BRAZIL to its height above water certain designating names. The entire low region subject to flood is known as the flood plain, and this is divided into igapo and varzea. The igapo, really a swamp forest, (Fig. 1) is the lowest land, but a few feet above the mean level, and is subject to overflow by the tides in the east and by slight rises in the river. The principal area of the igapo is the flat ►f ||rf*v aJiij^Mtal A|,^ JMflrf^^T 'Biiii6tH &h im^^ jb-^i^ > ^, „:^aBf ^^_ m (-yKKSSuiUKI^L. vu ^i^^V^:. t» ^ I.f-^--.. - « ■M-^m 1 f 1 .LL. Fig. 1. Igap6 on lower Amazon. coastal region east of Obidos. It is a country of islands separated by sluggish but often deep channels, of rivers and of lakes, the whole unstable and constantly chang- ing. The varzea is the higher land which is overflowed only during the high floods. The terra firme is still higher land, which is not subject to overflow. All of the rivers in the valley have igapo and varzea on both sides of them and extending a varying distance, broken here and there by higher terra firme. The terra firme rep- resents more than a difference in altitude, for it has a clay or rock foundation, a sand surface and is stable. MEDICAL REPORT 7 The igapo and varzea are formed of alluvium; the land constantly changing, disappearing in one place, forming in another; large islands disappear in the floods, others are formed, igapo becomes varzea and vice versa (Figs. 2 and 3). While on the way to Iquitos we saw a large section of the bank covered with high forest fall into the river and completely disappear. The best conception of the condition is gained by regarding the entire flood plain as a great lake which has been filled with sediment until only the rivers remain. The region is covered with forest, in extent the largest forest in the world; the towns and the clearings in it represent merely pin pricks. On the outskirts of the valley there are great regions, known as campas, free from forest, resembling the American prairies and cap- able of pasturing immense herds of cattle. Wallace states that from Tabatinga on the border of Peru a circle can be drawn with a radius of eleven hundred miles, all of which will be within the forest. Outside of this, smaller circles with radii up to four hundred miles can still be included. The varieties of trees and the density of the forest vary somewhat in different regions, but the general characteristics are the same. The trees are tall and closely placed; the trunks generally smooth and pale in color, giving off no branches until the forest roof, eighty to a hundred feet above the ground, is reached. Above this roof the domes of many of the higher trees project. Between the tall trees there is another forest of slender, shade-loving trees, and of others which await an opening in the roof through which to get their heads into the light. Vines are everywhere, trailing over the ground, extending up the trunks of trees and as long tightly stretched ropes descending from the trees to the earth. Most of the latter are the aerial roots of 8 THE RICE EXPEDITION TO BRAZIL I"n;. ■i. \ AHZKA K)l{h_ST WITH HKill SIIAHI* HANK DTK TO liK« KNT