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Aspects of nature, in different lands and different climates (Vol. 1 of 2)

Note 1 — STEPPES AND DESERTS.

Elizabeth Juliana Sabine translation

p. 1.—“The Lake of Tacarigua.”

In proceeding through the interior of South America from the Caraccas or Venezuela shore towards the boundary of Brazil, from the 10th degree of North latitude to the Equator, the traveller crosses first an elevated mountain-chain running in an east and west direction, next vast treeless Steppes or Plains (los Llanos), which stretch from the foot of the above-named mountains (the coast chain of Caraccas) to the left bank of the Orinoco, and lastly the range which occasions the Cataracts of Atures and Maypure. This latter range of mountains, to which I have given the name of the Sierra Parime, runs in an easterly direction from the Cataracts to Dutch and French Guiana. It is a mass of mountains divided into many parallel ridges, and is the site of the fabled Dorado. It is bordered on the south by the forest plain, through which the river of the Amazons and the Rio Negro have formed the channels in which their waters flow. Those who desire a fuller acquaintance with the geography of these regions will do well to consult and compare the great map of La Cruz-Olmedilla, bearing date 1775, (from which almost all the more recent maps of South America have been formed,) and the map of Columbia constructed by me from my own astronomical determinations of geographical positions, and published in 1825.

The coast chain of Venezuela, geographically considered, is a part of the chain of the Andes of Peru. The chain of the Andes divides itself, at the great mountain junction at the sources of the Magdalena, south of Popayan, (between 1° 55′ and 2° 20′ latitude), into three chains, the easternmost of which terminates in the snow-covered mountains of Merida. These mountains sink down towards the Paramo de las Rosas into the hilly land of Quibor and Tocuyo, which connects the coast chain of Venezuela with the Cordilleras of Cundinamarca. The coast chain forms an unbroken rampart from Porto Cabello to the promontory of Paria. Its mean height hardly equals 750 toises or 4795 English feet; yet single summits, like the Silla de Caracas (also called Cerro de Avila), decked with the purple-flowering Befaria the American Rose of the Alps, rise 1350 toises or 8630 English feet above the level of the sea. The coast of Terra Firma bears traces of devastation. We recognise everywhere the action of the great current which, sweeping from east to west, formed by disruption the West Indian Islands, and hollowed out the Caribbean gulf. The projecting tongues of land of Araja and Chuparipari, and especially the coast of Cumana and New Barcelona, offer a remarkable spectacle to the geologist. The precipitous Islands of Boracha, Caracas, and Chimanas, rise like towers from the sea, and bear witness to the terrible pressure of the waters against the mountain chain when it was broken by their irruption. Perhaps, like the Mediterranean, the Antillean gulf was once an inland sea, which became suddenly connected with the ocean. The islands of Cuba, Hayti, and Jamaica, still contain the remnants of the lofty mountains of mica slate which bounded this sea to the north. It is remarkable that where these three islands approach each other most nearly the highest summits are found; and we may conjecture that the highest part of this Antillean chain was situated between Cape Tiburon and Point Morant. The Copper Mountains (Montañas de Cobre) near Santiago de Cuba have not yet been measured, but their elevation is probably greater than that of the Blue Mountains of Jamaica, (1138 toises, 7277 English feet,) which somewhat exceeds the height of the St. Gothard Pass. My conjectures on the valley-form of the Atlantic Ocean, and on the ancient connection of the continents, were given more in detail in a memoir written in Cumana, entitled Fragment d’un Tableau Géologique de l’Amerique Meridionale (Journal de Physique, Messidor, An. IX.) It is worthy of remark, that Columbus himself, in his Official Reports, called attention to the connection between the direction of the equatorial current and the form of the coast line of the larger Antilles. (Examen critique de l’hist. de la Géographie, p. 104–108.)

The northern and most cultivated part of the province of Caraccas is a country of mountains. The coast chain is divided like the Swiss Alps into several subordinate chains enclosing longitudinal valleys. The most celebrated of these is the pleasant valley of Aragua, which produces a great quantity of indigo, sugar, cotton, and, what is most remarkable, European wheat. The southern margin of this valley adjoins the beautiful lake of Valencia, whose old Indian name is Tacarigua. The contrast between its opposite shores gives it a striking resemblance to the Lake of Geneva. It is true that the bare mountains of Guigue and Guiripa have less grandeur of character than the Savoy Alps; but, on the other hand, the opposite bank of the Tacarigua lake, which is thickly clothed with plantains, mimosas, and triplaris, far surpasses in picturesque beauty the vineyards of the Pays de Vaud. The lake is about thirty geographical miles in length, and is full of small islands, which, as the loss of water by evaporation exceeds the influx, are increasing in size. Within some years sand-banks have even become real islands, and have received the significant name of the “Newly Appeared,” Las Aparecidas. On the island of Cura the remarkable species of Solanum is cultivated which has edible fruit, and which Wildenow has described in the Hortus Berolinensis (1816, Tab. xxvii.) The height of the Lake of Tacarigua above the sea is almost 1400 French feet, (according to my measurement exactly 230 toises, or 1470 English feet,) less than the mean height of the valley of Caraccas. The lake has several kinds of fish (see my Observations de Zoologie et d’Anatomie comparée, T. ii p. 179–181), and is one of the most pleasing natural scenes which I know in any part of the globe. In bathing, Bonpland and myself were often alarmed by the appearance of the Bava, an undescribed crocodile-like lizard, three or four feet in length, of repulsive aspect, but harmless to men. We found in the lake a Typha (Cats-tail), identical with the European Typha angustifolia; a singular fact, and important in reference to the geography of plants.

Two varieties of sugar-cane are cultivated near the lake, in the valleys of Aragua: the common sugar-cane of the West Indies, Caña criolla; and the cane recently introduced from the Pacific, Caña de Otaheiti. The verdure of the Tahitian cane is of a much lighter and more agreeable tint, and a field of it can readily be distinguished at a great distance from a field of the common cane. The sugar-cane of Tahiti was first described by Cook and George Forster, who appear, however, from the excellent memoir of the latter upon the edible plants of the islands of the Pacific, to have been but little acquainted with its valuable qualities. Bougainville brought it to the Isle of France, from whence it was conveyed to Cayenne, and since 1792 it has been taken to Martinique, Hayti, and several of the smaller West Indian Islands. It was carried with the bread-fruit tree to Jamaica by the brave but unfortunate Captain Bligh, and was introduced from the Island of Trinidad to the neighbouring coast of Caraccas, where it became a more important acquisition than the bread-fruit, which is never likely to supersede a plant so valuable and affording so large an amount of sustenance as the plantain. The Tahitian sugar-cane is much richer in juice than the common cane, said to be originally a native of the east of Asia. On an equal surface of ground it yields a third more sugar than the caña criolla, which has a thinner stalk and smaller joints. As, moreover, the West India islands begin to suffer great want of fuel, (in Cuba the wood of the orange tree is used for sugar boiling,) the thicker and more woody stalk of the Tahitian cane is an important advantage. If the introduction of this plant had not taken place almost at the same time as the commencement of the bloody negro war in St. Domingo, the prices of sugar in Europe would have risen still higher than they did, in consequence of the ruinous effects of those troubles on agriculture and trade. It was an important question, whether the cane of the Pacific, when removed from its native soil, would gradually degenerate and become the same as the common cane. Experience hitherto has decided against any such degeneration. In Cuba a caballeria (nearly 33 English acres) planted with Tahitian sugar-cane produces 870 hundred weight of sugar. It is singular that this important production of the islands of the Pacific is only cultivated in those parts of the Spanish colonies which are farthest from the Pacific. The Peruvian coast is only twenty-five days’ sail from Tahiti, and yet, at the period of my travels in Peru and Chili, the Tahitian cane was unknown there. The inhabitants of Easter Island, who suffer much from deficiency of fresh water, drink the juice of the sugar-cane, and (a very remarkable physiological fact) also sea water. In the Society, Friendly, and Sandwich Islands, the light green, thick-stalked sugar-cane is always the one cultivated.

Besides the Caña de Otaheiti and the Caña Criolla, a reddish African variety, called Caña de Guinea, is cultivated in the West Indies: its juice is less in quantity than that of the common Asiatic cane, but is said to be better suited for making rum.

In the province of Caraccas the dark shade of the cacao plantations contrasts beautifully with the light green of the Tahitian sugar cane. Few tropical trees have such thick foliage as the Theobroma cacao. It loves hot and humid valleys: great fertility of soil and insalubrity of atmosphere are inseparable from each other in South America as well as in Asia; and it has even been remarked that as increasing cultivation lessens the extent of the forests, and renders the soil and climate less humid, the cacao plantations become less flourishing. For these reasons these plantations are diminishing in number and extent in the province of Caraccas, and increasing rapidly in the more eastern provinces of New Barcelona and Cumana, and particularly in the moist woody district between Cariaco and the Golfo Triste.

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