Geological Observations on South AmericaDarwin, Charles
Science
Geological Observations on South America
Darwin, Charles
Beagle Expedition (1831-1836); Geology -- South America; Mollusks, Fossil -- South America; Paleontology
The plain or basin, on the borders of which the famous bed of nitrate
of soda lies, is situated at the distance of about thirty miles from
the sea, being separated from it by the saliferous district just
described. It stands at a height of 3,300 feet; its surface is level,
and some leagues in width; it extends forty miles northward, and has a
total length (as I was informed by Mr. Belford Wilson, the
Consul-General at Lima) of 420 miles. In a well near the works,
thirty-six yards in depth, sand, earth, and a little gravel were found:
in another well, near Almonte, fifty yards deep, the whole consisted,
according to Mr. Blake, of clay, including a layer of sand two feet
thick, which rested on fine gravel, and this on coarse gravel, with
large rounded fragments of rock. (See an admirable paper “Geological
and Miscellaneous Notices of Tarapaca” in “Silliman’s American Journal”
volume 44 page 1.) In many parts of this now utterly desert plain,
rushes and large prostrate trees in a hardened state, apparently
Mimosas, are found buried, at a depth from three to six feet; according
to Mr. Blake, they have all fallen to the south-west. The bed of
nitrate of soda is said to extend for forty to fifty leagues along the
western margin of the plain, but is not found in its central parts: it
is from two to three feet in thickness, and is so hard that it is
generally blasted with gunpowder; it slopes gently upwards from the
edge of the plain to between ten and thirty feet above its level. It
rests on sand in which, it is said, vegetable remains and broken shells
have been found; shells have also been found, according to Mr. Blake,
both on and in the nitrate of soda. It is covered by a superficial mass
of sand, containing nodules of common salt, and, as I was assured by a
miner, much soft gypseous matter, precisely like that in the
superficial crust already described: certainly this crust, with its
characteristic concretions of anhydrite, comes close down to the edge
of the plain.
The nitrate of soda varies in purity in different parts, and often
contains nodules of common salt. According to Mr. Blake, the proportion
of nitrate of soda varies from 20 to 75 per cent. An analysis by Mr. A.
Hayes, of an average specimen, gave:—
Nitrate of Soda.... 64.98
Sulphate of Soda.... 3.00
Chloride of Soda... 28.69
Iodic Salts......... 0.63
Shells and Marl..... 2.60
99.90
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