Proceedings of the California Academy of Sciences, Volume III, 1863-1867Various
Science
Proceedings of the California Academy of Sciences, Volume III, 1863-1867
Various
California Academy of Sciences -- Periodicals; Science -- Periodicals
The name of the “Sierra Madre” is usually applied to the main
range of mountains of this country, or the western border of
the plateau which stretches north through the territories
of the United States, forming what may be called the great
orographical feature of the continent. In Northwestern
Mexico this crumpled border of the great plateau comprises
an extensive mountainous region, by no means forming a
continuous single chain, but rather several central ranges,
with associated groups of parallel ridges, all having the
same general course, which is approximately north-northwest,
and south-southeast. As the breadth of the chain widens as we
go towards the north, so, too, that of the valleys increases
in that direction, the whole system of mountains and valleys
spreading out in something like a fan shape.
Going north, the chain appears to sink gradually, although
determinations of altitude in Northern Mexico are extremely
few in number. It is certain that there is, in about latitude
32°, a depression of the mountain ranges which extends entirely
across the continent, and which would enable the traveler to
cross from the Atlantic to the Pacific, without necessarily
surmounting any elevation greater than four thousand feet.[22]
The southeastern range is the highest, and the culminating
point is said to be the Cerro de Cuiteco, sixty leagues
northeast of Jesus Maria, on the western border of Chihuahua.
The approximate altitude of the Cumbre de Basascachic is
seven thousand four hundred and twenty-nine feet, and that of
Guadalupe y Calvo, seven thousand eight hundred and twenty-five
feet. To the north, the ranges east of Sahuaripa are also very
high; but they have never been measured. No peaks or ridges,
however, in this portion of Mexico attain anything like the
elevation of the higher portion of the Sierra Nevada, few if
any points exceeding ten thousand feet in altitude.
The direction of the sierra is nearly that of a line connecting
some of the best mining districts in Mexico, which are situated
on or very near the summit of the mountains. These districts
are the following, enumerating them in their geographical order
from the south towards the north: In Durango, San Antonio de
las Ventanas, Guarisamey, and San Dimas, remarkable for their
auriferous silver ores, and sixty-two Mexican leagues northeast
of Mazatlan; in Chihuahua, Guadalupe y Calvo, and San Pedro
de Batopilas, yielding fine specimens of native silver; also,
Jesus Maria, in the same State, and the Real del la Cieneguita,
Sonora, with silver and gold mines.
2. GENERAL GEOLOGY.
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