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Untitled - The Alfred Russel Wallace Website

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IN THE CINCHONA FORESTS 271<br />

to be seen in the bottom of the valleys a fine-grained ferruginous<br />

sandstone of a deep brown colour, in thick strata, and usually in<br />

large detached masses, lying either horizontally or variously tilted<br />

up. I suppose, therefore, that, so far from having been deposited<br />

over the trachyte, it is merely the remains of a large bed of rock<br />

which once extended conformably over the whole region, and has<br />

been shivered and dislocated by the upheaval of the trachyte<br />

itself. It seems the same sort of rock as exists about the base of<br />

Tunguragua, and forms the lofty<br />

volcano, where the cataract of Guandisagua comes down at three<br />

bounds from the edge of the snow to the warm valley of Capil, in<br />

cliffs on the southern side of that<br />

which grow oranges and the sugar-cane. I have never been able<br />

to find any trace of fossils in this rock. . . . Nowhere in the<br />

Quitonian Andes have I seen the stratified rocks limestones,<br />

friable sandstones, and fossiliferous shales all, I believe, belonging<br />

to the lias formation, which constitute the eastern declivity of<br />

the Andes of Peru, or, at least, of the Province of Maynas. No<br />

Bark tree was seen growing on rock of any kind. <strong>The</strong> soil at<br />

Lirnon is the same deep loamy alluvial deposit, with very few<br />

stones intermixed, as we had seen from Llullundengo downwards,<br />

nor does a bit of rock crop out in the whole of the descent. . . .<br />

<strong>The</strong> n.orthern and eastern sides of the trees had borne most<br />

(lowers, and, except on one tree of more open growth than the<br />

rest, scarcely a capsule ripened on their southern and western<br />

sides. <strong>The</strong>se phenomena are explained by the fact that, in the<br />

summer season, the trees receive most sun from the east and<br />

north, for the mornings are generally clear and afternoons are almost invariably foggy, and the<br />

sunny, whilst the<br />

sun's declination<br />

is northerly. Another notable circumstance is that the trees<br />

standing in open ground -pasture, cane -<br />

field, etc.- are far<br />

healthier and more luxuriant than those growing in the forest,<br />

where they are hemmed in and partially shaded by other trees,<br />

and that, while many of the former had flowered freely, the latter<br />

were, without exception, sterile. This plainly shows that, although<br />

the Red Bark may need shade whilst young and tender, it iv,ill\<br />

requires (like most trees) plenty of air, light, and room wherein to<br />

develop its proportions.<br />

<strong>The</strong> cascarilleros have found out that the bark is worth money,<br />

but neither they nor the greater part of the inhabitants of Ecuador<br />

have any correct idea of the use that is made of it in foreign<br />

countries; the prevalent opinion being that a permanent coffee- or<br />

chocolate-coloured dye (still a desideratum in Ecuador) is extracted<br />

from it. I explained to the people of Limon how it yielded the<br />

precious quinine which was of such vast use in medicine: but I<br />

afterwards heard them saying one to another, "It is all very line<br />

tor him to stuff us with such a tale of ; course //< won't tell us how

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