Colorado River (Colo.-Mexico); Grand Canyon (Ariz.); United States -- Discovery and exploration
These are the elements with which the walls are constructed, from black
buttress below to alabaster tower above. All of these elements weather
in different forms and are painted in different colors, so that the wall
presents a highly complex facade. A wall of homogeneous granite, like
that in the Yosemite, is but a naked wall, whether it be 1,000 or 5,000
feet high. Hundreds and thousands of feet mean nothing to the eye when
they stand in a meaningless front. A mountain covered by pure snow
10,000 feet high has but little more effect on the imagination than a
mountain of snow 1,000 feet high--it is but more of the same thing;
but a facade of seven systems of rock has its sublimity multiplied
sevenfold.
Let the effect of this multiplied facade be more clearly realized. Stand
by the river side at some point where only the black gneiss
381 powell-canyons-245.jpg
A GABLE WITH PINNACLES.
382 powell-canyons-246.jpg
NICHES OR PANELS THE RED WALL LIMESTONE.
THE GRAND CANYON. 383
is seen. A precipitous wall of mountain rises over the river, with
crag and pinnacle and cliff in black and brown, and through it runs an
angular pattern of red and gray dikes of granite. It is but a mountain
cliff which may be repeated in many parts of the world, except that it
is singularly naked of vegetation, and the few plants that find footing
are of strange tropical varieties and are conspicuous because of their
infrequency.
Now climb 800 feet and a point of view is reached where the variegated
quartzites are seen. At the summit of the black gneiss a terrace is
found, and, set back of this terrace, walls of elaborate sculpture
appear, 800 feet in height. This is due to the fact that though the
rocks are exceedingly hard they are in very thin layers or strata, and
these strata are not horizontal, but stand sometimes on edge, sometimes
highly inclined, and sometimes gently inclined. In these variegated beds
there are many deep recesses and sharp salients, everywhere set with
crags, and the wall is buttressed by a steep talus in many places. In
the sheen of the midday sun, these rocks, which are besprinkled with
quartz crystals, gleam like walls of diamonds.
A climb of 800 feet over the variegated beds and the foot of the cliff
sandstone is reached. It is usually olive green, with spots of brown and
black, and presents 500 feet of vertical wall over the variegated sand-
stone. The dark green is in fine contrast with the variegated beds below
and the red wall above.
Public-domain text, read in full here on John Shaqi.
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