Colorado River (Colo.-Mexico); Grand Canyon (Ariz.); United States -- Discovery and exploration
River was flowing when the tilting commenced, and the upheaval was very
slow, so that the river cleared away the obstruction to its channel as
fast as it was presented, and this is the Grand Canyon. The rocks above
were carried away by rains and rivers, but not evenly all over the
country; nor by washing out valleys and leaving hills, but by carving
the country into terraces. The upper and later-formed rocks are found
far to the north, their edges standing in cliffs; then still earlier
rocks are found rising to the southward, until they terminate in cliffs;
and then a third series rises to the southward and ends in cliffs, and
finally a fourth series, the oldest rocks, terminating in the Grand
Canyon wall, which is a line of cliffs. There are in a general way four
great lines of cliffs extending from east to west across the district
and presenting their faces, or escarpments, southward. If these cliffs
are climbed it is found that each plateau or terrace dips gently to
the northward until it meets with another line of cliffs, which must be
ascended to reach the summit of another plateau. Place a book before you
on a table with its front edge toward you, rest another book on the back
of this, place a third on the back of the second, and in like manner a
fourth on the third. Now the leaves of the books dip from you and the
cut edges stand in tiny escarpments facing you. So the rock-formed
leaves of
91
V powell-canyons-57.jpg
A GROUP OF STONE CORRALS.
92 powell-canyons-58.jpg
RUINS.
CLIFFS AND TERRACES. 93
these books of geology have the escarpment edges turned southward, while
each book itself dips northward, and the crest of each plateau book
is the summit of a line of cliffs. These cliffs of erosion have been
described as running from east to west, but they diverge from that
course in many ways. First, canyons run from north to south through
them, and where these canyons are found deep angles occur; then sharp
salients extend from the cliffs on the backs of the lower plateaus. Each
great escarpment is made up more or less of minor terraces, or steps;
and at the foot of each grand escarpment there is always a great talus,
or sloping pile of rocks, and many marvelous buttes stand in front of
the cliffs.
Public-domain text, read in full here on John Shaqi.
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