Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 3 - By Alexander Von Humboldt And Aime Bonpland.
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Formations Of Quartzose Porphyry, Pyroxenic Porphyry And
Trachyte, Of Grauwacke, Muschelkalk And Quadersandstein, Which Are
Frequent Towards The West, Have
Not yet been seen in Venezuela; but it
may be also observed that in the system of secondary rocks of
The old
continent muschelkalk and quadersandstein are not always clearly
developed, and are often, by the frequency of their marls, confounded
with the lower layers of Jura limestone. The muschelkalk is almost a
lias with encrinites; and quadersandstein (for there are doubtless
many above the lias or limestone with gryphites) seems to me to
represent the arenaceous layers of the lower shelves of Jura
limestone.
I have thought it right to give at some length this geologic
description of South America, not only on account of the novel
interest which the study of the formations in the equinoctial regions
is calculated to excite, but also on account of the honourable efforts
which have recently been made in Europe to verify and extend the
working of the mines in the Cordilleras of Columbia, Mexico, Chile and
Buenos Ayres. Vast sums of money have been invested for the attainment
of this useful end. In proportion as public confidence has enlarged
and consolidated those enterprises, from which both continents may
derive solid advantage, it becomes the duty of persons who have
acquired a local knowledge of these countries to publish information
calculated to create a just appreciation of the relative wealth and
position of the mines in different parts of Spanish America. The
success of a company for the working of mines, and that of works
undertaken by the order of free governments, is far from depending
solely on the improvement of the machines employed for draining off
the water, and extracting the mineral, on the regular and economical
distribution of the subterraneous works, or the improvements in
preparation, amalgamation, and melting:
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