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Western World Sketches of Nature and Natural History in North & South America, a non-fiction book by William H. G. Kingston

Part 3 - Chapter 3. Valley Of The Amazon

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_ PART THREE
CHAPTER THREE. VALLEY OF THE AMAZON.


Standing on the eastern spur of the Andes, between 3 degrees and 4 degrees south of the equator, the eye of the traveller may see in imagination a vast valley, clothed with a dense forest, stretching towards the far-distant Atlantic. Behind him, on the west, tower the lofty peaks of the Cordilleras; on his left, in a northerly direction, appear the mountains and highlands of Venezuela and Guiana; while to the south rise the serras and table-lands of the Brazils. It is the Valley of the Amazon, in which more than half of Europe might be contained. Down the centre flows a mighty stream, the tributaries of which alone contain a bulk of water greater than all the European rivers put together.

Upwards of five hundred miles away to the south of the spot where the traveller stands, is the little lake of Lauricocha, near the silver-mines of Cerro de Pasco in Peru, just below the limit of perpetual snow--14,000 feet above the level of the sea. This lake has the honour of giving birth to the mighty stream: its waters forming the River Tunguragua, which, roaring and foaming in a series of cataracts and rapids through rocky valleys, flows northerly till it reaches the frontier of Ecuador. It then turns suddenly to the east, which direction it maintains, with a slightly northerly inclination, for two thousand miles--its volume greatly increased by numerous large streams, each of which is by itself a mighty river--till, attaining a width which may vie with that of the Baltic, it rushes with such fierce force into the Atlantic as to turn aside on either hand the salt-waters of the ocean. Thus the seaman approaching the shore of South America, when still out of sight of land, may lower his bucket and draw up the fresh-water which, it may be, has issued forth weeks before from the sides of the Andes. The whole length of the river, following its main curves, is but little under three thousand miles, while the tributaries from north to south stretch over seventeen hundred miles.

The basin of the Amazon may be considered like a shallow trough lying parallel to the equator, the southern sides having double the inclination of the northern, the whole gently sloping eastward. The channel of the river lies rather to the north of the basin, some hills rising directly above its waters; while the falls of several rivers to the south are two hundred miles above their mouths. Two thousand miles from its mouth the depth of the river is never less than eighteen feet, while many of its tributaries at their embouchures are of equal depth; and at the junction of the great rivers the hollows of its bed attain a depth of twenty-four fathoms. At Tabalingua, two thousand miles from its mouth, it is a mile and a half broad; and lower down, at the entrance of one of its tributaries--the Madeira--it measures three miles across. Still further to the east its sea-like reaches extend to the north for ten miles, with still wider lake-like expanses, so that the eye of the voyager can scarcely reach the forest-covered banks on the opposite side; while if the River Para is properly considered one of its branches, its measurement from shore to shore, across a countless number of islands, is one hundred and eighty miles--equal to the breadth of the widest part of the Baltic.

After receiving the waters of numerous streams, many of which flow for considerable distances parallel with its shores, and are united by a network of channels, it is joined by its most considerable northern tributary--the Rio Negro. This stream, rising in the mountains of Venezuela, and passing amidst the Llanos, robbing the Orinoco of part of its waters, has already, before it reaches the Amazon, flowed for a course of one thousand five hundred miles. It is called the Negro from its black colour. It is here not less than nineteen fathoms deep, and three thousand six hundred paces broad. The next great affluent is the Yapura, which, rising in the mountains of New Granada, takes a south-easterly course for one thousand miles, its principal mouth entering the Amazon opposite the town of Ega; but it has numberless small channels, the streams of which, two hundred miles apart, flow into the great river. The upper part of the Amazon is frequently called the Solimoens, which name it retains as far south as the mouth of the River Negro.

About sixty miles further east, its largest southern affluent--the gigantic Madeira--unites its milky waters with the turbid stream of the main river. One branch, the Beni, rises in the neighbourhood of the ancient Cuzco in Peru, near Lake Titicaca, its whole extent from the centre of the province of Bolivia being nearly the length of the Amazon itself. At its mouth it is two miles wide and sixty-six feet deep; and five hundred miles up it is a mile wide. Numerous islands are found in its course: for nearly five hundred miles it is navigable for large vessels, when a cataract intervenes. Were it not for this, there would be a free navigation from the centre of the province of Bolivia to the ocean, embracing islands the size of many of the Old World provinces, and widening into broad lakes. The monarch of waters flows on between its low forest-clothed banks till, four hundred miles from its mouth, it reaches the Strait of Obydos, where it is narrowed to two thousand paces. Through this channel its waters rush with immense force, calculated at five hundred thousand cubic feet in one second--sufficient to fill all the streams in Europe, and swell them to overflowing. No plummet has hitherto sounded the depth of its bed at this point, the force of the stream probably rendering the operation almost impracticable.

Its last two great tributaries are the Tapajos, six times the length of the Thames, and the Xingu, twice that of the Rhine; while further east a narrow channel unites it with the River Para, into which flows the broad stream of the Tocantins. This river, rising in the Minas-Geraes, six hundred miles from Rio Janeiro, is one thousand six hundred miles long, and ten miles wide at its mouth. Opposite to Para is the large island of Marajo; and if Professor Agassiz is right in supposing that the continent once extended much further to the east than it now does, this island may properly be considered in the centre of the mouth of the river, and the River Para might then properly be called one of its true embouchures. But only a few of the streams which feed the Amazon have been named. Numberless other rivers swell its waters, united to it by countless channels which form a wonderful network throughout the whole region, joining also many of the main rivers together, with the intricate navigation of which the natives alone are acquainted.

These curious water-paths, or igarapes, as they are called, are often so narrow that the branches of the lofty trees meet overhead, enabling the traveller in his canoe to proceed for miles together sheltered from the noonday sun. Here and there a glimpse of the sky can be discovered through the umbrageous foliage overhead, while birds of gay plumage flit to and fro, or sit perched on the branches uttering their strange and varied cries. In the intervals, or sometimes forming the termination of the water-path, numerous pools of various sizes exist--some a few yards across, others expanding into lakes--filled mostly by the overflowing of the main river during the rainy season. They are the habitations of a great variety of fishes. Here several species of turtles and alligators swarm in vast numbers; electric eels, too, abound in them, as well as many of the other curious water-creatures of that region. Water-fowl and various other aquatic birds dwell on their banks, while on the surface of their placid waters float the wide-spreading leaves and magnificent blossoms of the Victoria Regia, as also of other lilies and water-plants.

 

SCENES ON THE AMAZON.

The chief feature of the Lower Amazon is the vast expanse of smooth water, of a pale yellowish-olive colour, bearing on its bosom detached masses of aquatic grass floating down like islands, sometimes mixed with huge trees, their branches and roots interlocked, and often carrying among them wild animals, which, unconscious of their character, have there taken refuge from their foes, or have ventured thither in search of prey. The timid stag and fierce jaguar are sometimes thus entrapped and carried out to sea. At even and morn flocks of parrots and large and yellow macaws, fly backwards and forwards, uttering their wild and hoarse cries; herons and rails frequent the marshes on its banks; while all night long the cries of gulls and terns are heard over the sandy banks where they deposit their eggs, while they may be seen during the day sitting in rows on floating logs gliding down the stream, motionless and silent, as if contemplating the scenery. There are divers and darters, too, in abundance. Now and then a huge manatee comes gliding by, its cow-like head rising to breathe the upper air; while dolphins, porpoise-like, rear their backs above the surface, or leap half out of the water as they swim up the stream. On the low banks, huge alligators with open jaws are basking in the sun, or leisurely swimming across the river.

 

THE RAINY SEASON.

This magnificent region enjoys a perpetual summer, its various fruits coming to maturity, according to their character, at different periods throughout the year. It has, however, its wet and dry seasons. The rain occurs at one time in the Upper Amazon, and at another in the Lower,--greatly swelling the volume of water in the main stream, which, unable to find its way towards the ocean, rushes through the countless channels and igarapes, overflowing the lower portions of a vast district called the Gapo. The waters begin to rise in February, and progress inch by inch until the middle of June, gradually swelling the rivers and lakes, when, these becoming filled, the lower lands and sand-banks are overflowed even far-away in the interior. The forests are traversed by numerous gullies, which in the dry season are wide dells, but now become transformed into broad creeks, through which canoes can proceed to great distances under the shade of the lofty trees.

At this period of the year the inland pools are frequented by swarms of turtle, as well as alligators, and shoals of fish which leave the main river; while the flocks of wading birds migrate northerly, thus greatly dispersing the food on which the natives depend for their existence. The fishermen who have been employed during the dry months in catching turtle and fish on the sand-banks return to their villages, though some employ themselves in collecting the Brazil-nut and wild cacao, which are now ripe.

About the first week in June, the flood has risen sometimes to the height of forty feet above the usual level of the river, when it now begins to subside. The rains, however, do not fall continuously, though very heavy at times. Several days of beautiful sunny weather generally intervene. The fine season begins with a few days of brilliant weather--the rays of the sun breaking forth among the passing clouds. Towards the middle of July the sand-banks again appear, flocks of gulls and other water birds fly by, and the gaily-plumaged inhabitants of the forest come forth into full activity and life.

 

STORMS.

The navigation of the Amazon is not free from danger. Fierce storms arise; black clouds gather over the blue expanse, suffused anon with a lurid yellow tinge, and the fierce whirlwind howls along the river-banks, tearing the placid stream into masses of foam; the tall trees bend before the blast, and huge branches are wrenched off and hurled into the water. The long-legged waders and other water birds, unable to face it, throw themselves on the ground, and cling with claws and beak to the sand to escape being carried helplessly away.

 

THE POROROCCA.

Sometimes, too, the destroying pororocca--a vast wave rising across the whole width of the stream, to the height of twelve or fifteen feet-- sweeps up the stream. Advancing noiselessly over the deeper portions of the river-bed, it rises into an angry billow, with a fearful roar when passing over a shallow, or meeting any impediment in its course. A French traveller describes an island where he and his companions had rested on their voyage down the stream. They had happily gone over to the mainland on the previous evening, when, as they stood on the shore, the pororocca was heard approaching. Onward it came till the island was reached, when, with an angry roar, it burst into masses of foam, and swept over the devoted spot, carrying in its fierce embrace not only the whole mass of vegetation, but overturning the foundations of the island itself, so that in a few seconds not a vestige remained. Sometimes, too, the higher banks of the Upper Amazon, crowned by lofty trees, are worn away by the rapid current, increased during the rainy season, continually passing beneath them, till the upper portions, deprived of their support, fall over with a terrific roar into the stream, dragging with them their neighbours. The earth trembles with the concussion, the waters hiss and foam and rush furiously over the impediments in their course. Sometimes miles of the bank thus give way, the sound being heard far up and down the stream. Occasionally a canoe and its crew-- who, to avoid the current, have been toiling close along the bank--have been thus overwhelmed; while others, descending, unaware of the obstruction, have been dragged by the furious whirlpool thus formed amid the tangled branches, and destroyed. _

Read next: Part 3: Chapter 4. Character Of Vegetation On The Banks

Read previous: Part 3: Chapter 2. A General View Of South America

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