Guide to Yosemite: A handbook of the trails and roads of Yosemite valley and the adjacent region — John Shaqi
Guide to Yosemite: A handbook of the trails and roads of Yosemite valley and the adjacent regionHall, Ansel F. (Ansel Franklin)
History
Guide to Yosemite: A handbook of the trails and roads of Yosemite valley and the adjacent region
Hall, Ansel F. (Ansel Franklin)
Yosemite Valley (Calif.) -- Guidebooks
About midway between the north and south ends of this "Snowy Range"
and extending from the ragged summits of its eastern edge to the
semi-arid foothills at the west, lies Yosemite National Park, 1125
square miles of incomparable scenic beauty.
Yosemite Valley, contrary to most peoples' preconceived idea, lies
fully 25 miles west of the Sierra crest. It is countersunk 4000 feet
into the granite of the gently inclined plateau, which above its rim
averages from 7000 to 8000 feet in elevation. The characteristics of
this region immediately adjacent to Yosemite Valley are different from
those of the High Sierra to the past. Very little of it is above the
timber-line, as the dominating summits--Mount Hoffman (10,921) at the
north, Clouds Rest (9924) at the east, Mount Starr King (9179) at the
southeast, and Horse Ridge (9600) at the south--average less than
10,000 feet in altitude. The magnificent forests with which the slopes
are clothed are interspersed with perfectly formed granite domes, with
meadows and wild-flower gardens, with polished granite pavements, and
with innumerable manifestations of Nature which give the trails of the
region an ever-changing charm.
YOSEMITE VALLEY
Bisecting this district from east to west is the great trough of
Yosemite Valley, its bottom gouged down more than half way to sea
level. The same type of geological architecture is exemplified by the
Hetch Hetchy a few miles to the north and by the canyons of the San
Joaquin, Kings and Kern to the south. In none of these however, are
magnitude, beauty and accessibility so ideally combined as in
Yosemite.
ORIGIN
As to the origin of these valleys, and of Yosemite in particular,
there is still some discussion among scientists. Whitney's old theory
of a great cataclysm and the sinking of a small block of the earth's
crust has been entirely displaced, and geologists are now seeking to
determine if glaciers have been solely responsible for the present
landscape or whether ice and water worked hand in hand. A good summary
of the various theories of geological history, as well as a popular
discussion of all the geological phenomena of the region, is contained
in the "Sketch of Yosemite National Park and an Account of the Origin
of Yosemite and Hetch Hetchy Valleys," by Dr. F. E. Matthes of the
U.S. Geological Survey. This government publication may be obtained in
Yosemite at the office of the Superintendent for ten cents.
EARLY HISTORY
Public-domain text, read in full here on John Shaqi.
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