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JUNCTION OF THE APURE AND THE ORINOCO.
MOUNTAINS OF ENCARAMADA.
URUANA.
BARAGUAN.
CARICHANA.
MOUTH OF THE META.
ISLAND OF PANUMANA.
On leaving the Rio Apure we found ourselves in a country presenting a totally different aspect.
An immense plain of water stretched before us like a lake, as far as we could see.
White-topped waves rose to the height of several feet, from the conflict of the breeze and the current.
The air resounded no longer with the piercing cries of herons, flamingos, and spoonbills, crossing in long files from one shore to the other.
Our eyes sought in vain those waterfowls, the habits of which vary in each tribe.
All nature appeared less animated.
Scarcely could we discover in the hollows of the waves a few large crocodiles, cutting obliquely, by the help of their long tails, the surface of the agitated waters.
The horizon was bounded by a zone of forests, which nowhere reached so far as the bed of the river.
A vast beach, constantly parched by the heat of the sun, desert and bare as the shores of the sea, resembled at a distance, from the effect of the mirage, pools of stagnant water.
These sandy shores, far from fixing the limits of the river, render them uncertain, by enlarging or contracting them alternately, according to the variable action of the solar rays.
In these scattered features of the landscape, in this character of solitude and of greatness, we recognize the course of the Orinoco, one of the most majestic rivers of the New World.
The water, like the land, displays everywhere a characteristic and peculiar aspect.
The bed of the Orinoco resembles not the bed of the Meta, the Guaviare, the Rio Negro, or the Amazon.
These differences do not depend altogether on the breadth or the velocity of the current; they are connected with a multitude of impressions which it is easier to perceive upon the spot than to define with precision.
Thus, the mere form of the waves, the tint of the waters, the aspect of the sky and the clouds, would lead an experienced navigator to guess whether he were in the Atlantic, in the Mediterranean, or in the equinoctial part of the Pacific.
The wind blew fresh from east-north-east.
Its direction was favourable for sailing up the Orinoco, towards the Mission of Encaramada; but our canoes were so ill calculated to resist the shocks of the waves, that, from the violence of the motion, those who suffered habitually at sea were equally incommoded on the river.
The short, broken waves are caused by the conflict of the waters at the junction of the two rivers.
This conflict is very violent, but far from being so dangerous as Father Gumilla describes.
We passed the Punta Curiquima, which is an isolated mass of quartzose granite, a small promontory composed of rounded blocks.
There, on the right bank of the Orinoco, Father Rotella founded, in the time of the Jesuits, a Mission of the Palenka and Viriviri or Guire Indians.
But during inundations, the rock Curiquima and the village at its foot were entirely surrounded by water; and this serious inconvenience, together with the sufferings of the missionaries and Indians from the innumerable quantity of mosquitos and niguas,* led them to forsake this humid spot.
(* The chego (Pulex penetrans) which penetrates under the nails of the toe in men and monkeys, and there deposits its eggs.
) It is now entirely deserted, while opposite to it, on the right bank of the river, the little mountains of Coruato are the retreat of wandering Indians, expelled either from the Missions, or from tribes that are not subject to the government of the monks.
Struck with the extreme breadth of the Orinoco, between the mouth of the Apure and the rock Curiquima, I ascertained it by means of a base measured twice on the western beach.
The bed of the Orinoco, at low water, was 1906 toises broad; but this breadth increases to 5517 toises, when, in the rainy season, the rock Curiquima, and the farm of Capuchino near the hill of Pocopocori, become islands.
The swelling of the Orinoco is augmented by the impulse of the waters of the Apure, which, far from forming, like other rivers, an acute angle with the upper part of that into which it flows, meets it at right angles.
We first proceeded south-west, as far as the shore inhabited by the Guaricoto Indians on the left bank of the Orinoco, and then we advanced straight toward the south.
The river is so broad that the mountains of Encaramada appear to rise from the water, as if seen above the horizon of the sea.
They form a continued chain from east to west.
These mountains are composed of enormous blocks of granite, cleft and piled one upon another.
Their division into blocks is the effect of decomposition.
What contributes above all to embellish the scene at Encaramada is the luxuriance of vegetation that covers the sides of the rocks, leaving bare only their rounded summits.
They look like ancient ruins rising in the midst of a forest.
The mountain immediately at the back of the Mission, the Tepupano* of the Tamanac Indians is terminated by three enormous granitic cylinders, two of which are inclined, while the third, though worn at its base, and more than eighty feet high, has preserved a vertical position.
(* Tepu-pano, place of stones, in which we recognize tepu stone, rock, as in tepu-iri, mountain.
We here perceive that Lesgian Oigour-Tartar root tep, stone (found in America among the Americans, in teptl; among the Caribs, in tebou; among the Tamanacs, in tepuiri); a striking analogy between the languages of Caucasus and Upper Asia and those of the banks of the Orinoco.
) This rock, which calls to mind the form of the Schnarcher in the Hartz mountains, or that of the Organs of Actopan in Mexico,* composed formerly a part of the rounded summit of the mountain.
(* In Captain Tuckey's Voyage on the river Congo, we find represented a granitic rock, Taddi Enzazi, which bears a striking resemblance to the mountain of Encaramada.
) In every climate, unstratified granite separates by decomposition into blocks of prismatic, cylindric, or columnar figures.
Opposite the shore of the Guaricotos, we drew near another heap of rocks, which is very low, and three or four toises long.
It rises in the midst of the plain, and has less resemblance to a tumulus than to those masses of granitic stone, which in North Holland and Germany bear the name of hunenbette, beds (or tombs) of heroes.
The shore, at this part of the Orinoco, is no longer of pure and quartzose sand; but is composed of clay and spangles of mica, deposited in very thin strata, and generally at an inclination of forty or fifty degrees.
It looks like decomposed mica-slate.
This change in the geological configuration of the shore extends far beyond the mouth of the Apure.
We had begun to observe it in this latter river as far off as Algodonal and the Cano del Manati.
The spangles of mica come, no doubt, from the granite mountains of Curiquima and Encaramada; since further north-east we find only quartzose sand, sandstone, compact limestone, and gypsum.
Alluvial earth carried successively from south to north need not surprise us in the Orinoco; but to what shall we attribute the same phenomenon in the bed of the Apure, seven leagues west of its mouth?
In the present state of things, notwithstanding the swellings of the Orinoco, the waters of the Apure never retrograde so far; and, to explain this phenomenon, we are forced to admit that the micaceous strata were deposited at a time when the whole of the very low country lying between Caycara, Algodonal, and the mountains of Encaramada, formed the basin of an inland lake.
We stopped some time at the port of Encaramada, which is a sort of embarcadero, a place where boats assemble.
A rock of forty or fifty feet high forms the shore.
It is composed of blocks of granite, heaped one upon another, as at the Schneeberg in Franconia, and in almost all the granitic mountains of Europe.
Some of these detached masses have a spheroidal form; they are not balls with concentric layers, but merely rounded blocks, nuclei separated from their envelopes by the effect of decomposition.
This granite is of a greyish lead-colour, often black, as if covered with oxide of manganese; but this colour does not penetrate one fifth of a line into the rock, which is of a reddish white colour within, coarse-grained, and destitute of hornblende.
The Indian names of the Mission of San Luis del Encaramada, are Guaja and Caramana.
* (* All the Missions of South America have names composed of two words, the first of which is necessarily the name of a saint, the patron of the church, and the second an Indian name, that of the nation, or the spot where the establishment is placed.
Thus we say, San Jose de Maypures, Santa Cruz de Cachipo, San Juan Nepomuceno de los Atures, etc. These compound names appear only in official documents; the Inhabitants adopt but one of the two names, and generally, provided it be sonorous, the Indian.
As the names of saints are several times repeated in neighbouring places, great confusion in geography arises from these repetitions.
The names of San Juan, San Diego, and San Pedro, are scattered in our maps as if by chance.
It is pretended that the Mission of Guaja affords a very rare example of the composition of two Spanish words.
The word Encaramada means things raised one upon another, from encaramar, to raise up.
It is derived from the figure of Tepupano and the neighbouring rocks: perhaps it is only an Indian word caramana, in which, as in manati, a Spanish signification was believed to be discovered.
) This small village was founded in 1749 by Father Gili, the Jesuit, author of the Storia dell' Orinoco, published at Rome.
This missionary, learned in the Indian tongues, lived in these solitudes during eighteen years, till the expulsion of the Jesuits.
To form a precise idea of the savage state of these countries it must be recollected that Father Gili speaks of Carichana,* which is forty leagues from Encaramada, as of a spot far distant; and that he never advanced so far as the first cataract in the river of which he ventured to undertake the description.
(* Saggio di Storia Americana volume 1 page 122. ) In the port of Encaramada we met with some Caribs of Panapana.
A
cacique was going up the Orinoco in his canoe, to join in the famous fishing of turtles' eggs.
His canoe was rounded toward the bottom like a bongo, and followed by a smaller boat called a curiara.
He was seated beneath a sort of tent, constructed, like the sail, of palm-leaves.
His cold and silent gravity, the respect with which he was treated by his attendants, everything denoted him to be a person of importance.
He was equipped, however, in the same manner as his Indians.
They were all equally naked, armed with bows and arrows, and painted with onoto, which is the colouring fecula of the Bixa orellana.
The chief, the domestics, the furniture, the boat, and the sail, were all painted red.
These Caribs are men of an almost athletic stature; they appeared to us much taller than any Indians we had hitherto seen.
Their smooth and thick hair, cut short on the forehead like that of choristers, their eyebrows painted black, their look at once gloomy and animated, gave a singular expression to their countenances.
Having till then seen only the skulls of some Caribs of the West India Islands preserved in the collections of Europe, we were surprised to find that these Indians, who were of pure race, had foreheads much more rounded than they are described.
The women, who were very tall, and disgusting from their want of cleanliness, carried their infants on their backs.
The thighs and legs of the infants were bound at certain distances by broad strips of cotton cloth, and the flesh, strongly compressed beneath the ligatures, was swelled in the interstices.
It is generally to be observed, that the Caribs are as attentive to their exterior and their ornaments, as it is possible for men to be, who are naked and painted red.
They attach great importance to certain configurations of the body; and a mother would be accused of culpable indifference toward her children, if she did not employ artificial means to shape the calf of the leg after the fashion of the country.
As none of our Indians of Apure understood the Caribbee language, we could obtain no information from the cacique of Panama respecting the encampments that are made at this season in several islands of the Orinoco for collecting turtles' eggs.
Near Encaramada a very long island divides the river into two branches.
We passed the night in a rocky creek, opposite the mouth of the Rio Cabullare, which is formed by the Payara and the Atamaica, and is sometimes considered as one of the branches of the Apure, because it communicates with that river by the Rio Arichuna.
The evening was beautiful.
The moon illumined the tops of the granite rocks.
The heat was so uniformly distributed, that, notwithstanding the humidity of the air, no twinkling of the stars was observable, even at four or five degrees above the horizon.
The light of the planets was singularly dimmed; and if, on account of the smallness of the apparent diameter of Jupiter, I had not suspected some error in the observation, I should say, that here, for the first time, we thought we distinguished the disk of Jupiter with the naked eye.
Towards midnight, the north-east wind became extremely violent.
It brought no clouds, but the vault of the sky was covered more and more with vapours.
Strong gusts were felt, and made us fear for the safety of our canoe.
During this whole day we had seen very few crocodiles, but all of an extraordinary size, from twenty to twenty-four feet.
The Indians assured us that the young crocodiles prefer the marshes, and the rivers that are less broad, and less deep.
They crowd together particularly in the Canos, and we may say of them, what Abdallatif says of the crocodiles of the Nile,* "that they swarm like worms in the shallow waters of the river, and in the shelter of uninhabited islands."
(* Description de l'Egypte translated by De Sacy.
) On the 6th of April, whilst continuing to ascend the Orinoco, first southward and then to south-west, we perceived the southern side of the Serrania, or chain of the mountains of Encaramada.
The part nearest the river is only one hundred and forty or one hundred and sixty toises high; but from its abrupt declivities, its situation in the midst of a savannah, and its rocky summits, cut into shapeless prisms, the Serrania appears singularly elevated.
Its greatest breadth is only three leagues.
According to information given me by the Indians of the Pareka nation, it is considerably wider toward the east.
The summits of Encaramada form the northernmost link of a group of mountains which border the right bank of the Orinoco, between the latitudes of 5 degrees and 7 degrees 30 minutes from the mouth of the Rio Zama to that of the Cabullare.
The different links into which this group is divided are separated by little grassy plains.
They do not preserve a direction perfectly parallel to each other; for the most northern stretch from west to east, and the most southern from north-west to south-east.
This change of direction sufficiently explains the increase of breadth observed in the Cordillera of Parime towards the east, between the sources of the Orinoco and of the Rio Paruspa.
On penetrating beyond the great cataracts of Atures and of Maypures, we shall see seven principal links, those of Encaramada or Sacuina, of Chaviripa, of Baraguan, of Carichana, of Uniama, of Calitamini, and of Sipapo, successively appear.
This sketch may serve to give a general idea of the geological configuration of the ground.
We recognize everywhere on the globe a tendency toward regular forms, in those mountains that appear the most irregularly grouped.
Every link appears, in a transverse section, like a distinct summit, to those who navigate the Orinoco; but this division is merely in appearance.
The regularity in the direction and separation of the links seems to diminish in proportion as we advance towards the east.
The mountains of Encaramada join those of Mato, which give birth to the Rio Asiveru or Cuchivero; those of Chaviripe are prolonged by the granite chain of the Corosal, of Amoco, and of Murcielago, towards the sources of the Erevato and the Ventuari.
It was across these mountains, which are inhabited by Indians of gentle character, employed in agriculture,* (* The Mapoyes, Parecas, Javaranas, and Curacicanas, who possess fine plantations (conucos) in the savannahs by which these forests are bounded.
) that, at the time of the expedition for settling boundaries, General Iturriaga took some horned cattle for the supply of the new town of San Fernando de Atabapo.
The inhabitants of Encaramada then showed the Spanish soldiers the way by the Rio Manapiari,* which falls into the Ventuari.
(* Between Encaramada and the Rio Manapiare, Don Miguel Sanchez, chief of this little expedition, crossed the Rio Guainaima, which flows into the Cuchivero.
Sanchez died, from the fatigue of this journey, on the borders of the Ventuari.
) By descending these two rivers, the Orinoco and the Atabapo may be reached without passing the great cataracts, which present almost insurmountable obstacles to the conveyance of cattle.
The spirit of enterprise which had so eminently distinguished the Castilians at the period of the discovery of America, was again roused for a time in the middle of the eighteenth century, when Ferdinand VI was desirous of knowing the true limits of his vast possessions; and in the forests of Guiana, that land of fiction and fabulous tradition, the wily Indians revived the chimerical idea of the wealth of El Dorado, which had so much occupied the imagination of the first conquerors.
Amidst the mountains of Encaramada, which, like most coarse-grained granite rocks, are destitute of metallic veins, we cannot help inquiring whence came those grains of gold which Juan Martinez* (* The companion of Diego Ordaz.
) and Raleigh profess to have seen in such abundance in the hands of the Indians of the Orinoco.
From what I observed in that part of America, I am led to think that gold, like tin,* is sometimes disseminated in an almost imperceptible manner in the very mass of granite rocks, without our being able to perceive that there is a ramification and an intertwining of small veins.
(* Thus tin is found in granite of recent formation, at Geyer; in hyalomicte or graisen, at Zinnwald; and in syenitic porphyry, at Altenberg, in Saxony, as well as near Naila, in the Fichtelgebirge.
I
have also seen, in the Upper Palatinate, micaceous iron, and black earthy cobalt, far from any kind of vein, disseminated in a granite destitute of mica, as magnetic iron-sand is in volcanic rocks.
) Not long ago the Indians of Encaramada found in the Quebrada del Tigre* (* The Tiger-ravine.
) a piece of native gold two lines in diameter.
It was rounded, and appeared to have been washed along by the waters.
This discovery excited the attention of the missionaries much more than of the natives; it was followed by no other of the same kind.
I cannot quit this first link of the mountains of Encaramada without recalling to mind a fact that was not unknown to Father Gili, and which was often mentioned to me during our abode in the Missions of the Orinoco.
The natives of those countries have retained the belief that, "at the time of the great waters, when their fathers were forced to have recourse to boats, to escape the general inundation, the waves of the sea beat against the rocks of Encaramada."
This belief is not confined to one nation singly, the Tamanacs; it makes part of a system of historical tradition, of which we find scattered notions among the Maypures of the great cataracts; among the Indians of the Rio Erevato, which runs into the Caura; and among almost all the tribes of the Upper Orinoco.
When the Tamanacs are asked how the human race survived this great deluge, the age of water, of the Mexicans, they say, a man and a woman saved themselves on a high mountain, called Tamanacu, situated on the banks of the Asiveru; and casting behind them, over their heads, the fruits of the mauritia palm-tree, they saw the seeds contained in those fruits produce men and women, who repeopled the earth.
Thus we find in all its simplicity, among nations now in a savage state, a tradition which the Greeks embellished with all the charms of imagination!
A few leagues from Encaramada, a rock, called Tepu-mereme, or the painted rock, rises in the midst of the savannah.
Upon it are traced representations of animals, and symbolic figures resembling those we saw in going down the Orinoco, at a small distance below Encaramada, near the town Caycara.
Similar rocks in Africa are called by travellers fetish stones.
I shall not make use of this term, because fetishism does not prevail among the natives of the Orinoco;
and the figures of stars, of the sun, of tigers, and of crocodiles, which we found traced upon the rocks in spots now uninhabited, appeared to me in no way to denote the objects of worship of those nations.
Between the banks of the Cassiquiare and the Orinoco, between Encaramada, the Capuchino, and Caycara, these hieroglyphic figures are often seen at great heights, on rocky cliffs which could be accessible only by constructing very lofty scaffolds.
When the natives are asked how those figures could have been sculptured, they answer with a smile, as if relating a fact of which only a white man could be ignorant, that "at the period of the great waters, their fathers went to that height in boats."
These ancient traditions of the human race, which we find dispersed over the whole surface of the globe, like the relics of a vast shipwreck, are highly interesting in the philosophical study of our own species.
Like certain families of the vegetable kingdom, which, notwithstanding the diversity of climates and the influence of heights, retain the impression of a common type, the traditions of nations respecting the origin of the world, display everywhere the same physiognomy, and preserve features of resemblance that fill us with astonishment.
How many different tongues, belonging to branches that appear totally distinct, transmit to us the same facts!
The traditions concerning races that have been destroyed, and the renewal of nature, scarcely vary in reality, though every nation gives them a local colouring.
In the great continents, as in the smallest islands of the Pacific Ocean, it is always on the loftiest and nearest mountain that the remains of the human race have been saved; and this event appears the more recent, in proportion as the nations are uncultivated, and as the knowledge they have of their own existence has no very remote date.
After having studied with attention the Mexican monuments anterior to the discovery of the New World; after having penetrated into the forests of the Orinoco, and observed the diminutive size of the European establishments, their solitude, and the state of the tribes that have remained independent; we cannot allow ourselves to attribute the analogies just cited to the influence exercised by the missionaries, and by Christianity, on the national traditions.
Nor is it more probable, that the discovery of sea-shells on the summit of mountains gave birth, among the nations of the Orinoco, to the tradition of some great inundation which extinguished for a time the germs of organic life on our globe.
The country that extends from the right bank of the Orinoco to the Cassiquiare and the Rio Negro, is a country of primitive rocks.
I saw there one small formation of sandstone or conglomerate; but no secondary limestone, and no trace of petrifactions.
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