The Geologic Story of Canyonlands National ParkLohman, Stanley William
Science
The Geologic Story of Canyonlands National Park
Lohman, Stanley William
Canyonlands National Park (Utah) -- Guidebooks; Geology -- Utah -- Canyonlands National Park -- Guidebooks
A mile and a half above the confluence is The Slide, a jumbled mass of
angular blocks of rock that fell from the northwest canyon wall and
originally probably extended all the way to the southeast bank of the
river. As shown in figure 78, it still extends nearly across the river,
leaving only a narrow deep chute along the southeast bank. Just after
the photograph was taken, we hit rough fast water in the chute, with
waves about 2 feet high. At higher stages of the river, progressively
more of The Slide is covered by water, and there is less tendency for
waves to form. The date of this landslide is not known, but it is shown
on a map by Herron (1917, pl. 22A) made prior to 1917 and may well have
occurred during prehistoric times.
Soon we reach the confluence of the Green and Colorado Rivers (figs. 59,
60). This important junction of two mighty rivers was noted by all
previous voyagers, but their impressions of it differed considerably.
Powell (1875, p. 56) remarked:
These streams unite in solemn depths, more than one thousand two
hundred feet below the general surface of the country. The walls of
the lower end of Stillwater Cañon are very beautifully curved [see
fig. 67], as the river sweeps in its meandering course. The lower end
of the cañon through which the Grand comes down, is also regular, but
much more direct, and we look up this stream, and out into the country
beyond, and obtain glimpses of snow clad peaks, the summits of a group
of mountains known as the Sierra La Sal [La Sal Mountains]. Down the
Colorado, the cañon walls are much broken.
Dellenbaugh (1902, p. 277) gave a fuller description but concluded: “In
every way the Junction is a desolate place”—an appraisal with which I
disagree. The most colorful account I have read is that of Captain
Francis Marion Bishop, a member of Powell’s 1871 expedition, who
recorded in his journal for September 15, 1871 (1947, p. 202):
Well, we are at last, after many days of toil and labor, here at the
confluence of the two great arteries of this great mountain desert. No
more shall our frail boats dash through thy turbid waters, Old Green,
and no more shall we press on to see the dark flood from the peaks and
parks of Colorado. Grand and Green here sink to thy rest, and from thy
grave the _Colorado de Grande_ shall flow on forever, and on thy bosom
henceforth will we battle with rock and wave. One can hardly tell
which is the largest of the two rivers. Neither seems to flow into the
other, but there seems to be a blending of both, and from their union
rolls the Colorado River.
Public-domain text, read in full here on John Shaqi.
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