Titan of Chasms: The Grand Canyon of ArizonaPowell, John Wesley
History
Titan of Chasms: The Grand Canyon of Arizona
Powell, John Wesley
Grand Canyon (Ariz.)
The trip in winter from Peach Springs station down to the Colorado
River, through Diamond Creek Canyon, is most enjoyable. Owing to the low
altitude here (4,780 feet at Peach Springs and approximately 2,000 feet
at the river) the air is usually balmy from November to April; in summer
the heat is a considerable drawback.
A journey of but twelve miles leads you through a miniature Grand Canyon
with scenery increasingly sublime. On either side are abrupt walls and
wonderfully suggestive formations—castles, domes, minarets. On your
left, glancing backward, is an exact reproduction of Westminster Abbey.
This comparatively easy jaunt brings you by team to the very brink of
the swift-rolling Colorado, whereas by the other Grand Canyon gateways
you are landed on the rim and must go down thousands of feet by a steep
trail. The outlook here is restricted to the river itself and the great
walls rising precipitously from its banks—a scene well worth while, but
not so impressive as the wide sweep of the canyon visible from the rim.
Following Diamond Creek to its source you may walk along the bed of the
stream between walls thousands of feet high and glistening in the white
sunlight as if varnished. The upper part of Diamond Creek is a veritable
terrace of fern bowers, luxuriant vegetation, crystal cascades, and
sequestered meadow parks.
Flagstaff and Vicinity
The town itself is an interesting place, prettily situated in the heart
of the San Francisco uplift and surrounded by a pine forest.
Its hotels, business houses, lumber mills, and residences denote thrift.
On a neighboring hill is the Lowell Observatory, noted for its many
contributions to astronomical science.
[Illustration: San Francisco Peaks.]
Eight miles southwest from Flagstaff—reached by a pleasant drive along a
level road through tall pines—is Walnut Canyon, a rent in the earth
several hundred feet deep and three miles long, with steep terraced
walls of limestone. Along the shelving terraces, under beetling
projections of the strata, are scores of quaint cliff dwellings, the
most famous group of its kind in this region. The larger abodes are
divided into several compartments by cemented walls, many parts of which
are still intact. It is believed that these cliff dwellers were of the
same stock as the Pueblo Indians of to-day and that they lived here
about 800 years ago.
Nine miles from Flagstaff and only half a mile from the old stage road
to the Grand Canyon, upon the summit of an extinct crater, the
remarkable ruins of the cave-dwellers may be seen.
Public-domain text, read in full here on John Shaqi.
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