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
Although some two-wheel-drive cars or trucks have traversed the White
Rim and Shafer Trails, they may encounter trouble with deep sand,
washouts, or fallen rocks, so four-wheel-drive vehicles are recommended.
In the summer these trails should not be attempted without plenty of
water, and two vehicles traveling together provide an added margin of
safety. All vehicles should carry emergency equipment including a
shovel, tow chain or rope, jack, tire tools, and other necessary items.
Geologists and uranium prospectors working along the White Rim Trail
have obtained good drinking water from small springs that flow from the
base of the White Rim Sandstone in many places (Neal Hinrichs, U.S.
Geol. Survey, oral commun., Feb. 1973). After rains, runoff gathers in
large potholes in the White Rim Sandstone in some places and affords
emergency drinking water. Several such potholes filled with water are
shown in figure 17. Some potholes occur also in the Cedar Mesa Sandstone
in the Needles district.
GRAND VIEW POINT
About a mile southwest of The Neck, the road crosses Grays Pasture—the
widest and flattest part of Island in the Sky. The drive over this flat
grassland yields not the slightest hint of the awesome cliff-walled
chasms on either side of the island. Some 5 miles southwest of The Neck,
both the island and the road branch like a Y. At a point 0.4 mile north
of the Y, Mesa Trail leads one-quarter mile east to Canyon Viewpoint
Arch, which frames the Colorado River canyon and the La Sal Mountains
(fig. 18). This arch, at the very top edge of the cliff, is composed of
the lower part of the Navajo Sandstone. The only other arch of Navajo
Sandstone in or near the park that I know of is the small one shown in
figure 33, but of course there may be others.
[Illustration: NATURAL TANKS, filled with runoff from rain, serve as
emergency sources of drinking water. Largest tank in foreground
contains 4 feet of water and small fresh-water shrimp. So-called
tanks, or potholes, are formed partly by water dissolving the
calcium carbonate cement and partly by wind or water removing the
resulting loose sand grains. View is north toward Junction Butte
from point about a mile south of the White Rim Trail. Red rocks in
hill on right are in lower part of Moenkopi Formation. Photograph by
E. N. Hinrichs. (Fig. 17)]
[Illustration: CANYON VIEWPOINT ARCH, framing Colorado River canyon
at east end of Mesa Trail 0.4 mile north of Y in Island in the Sky
road. Arch is in lower part of Navajo Sandstone. (Fig. 18)]
[Illustration: INDEX MAP showing localities where most of the
photographs were taken. Arrows point to distant views. Numbers refer
to figure numbers. (Fig. 19)]
Public-domain text, read in full here on John Shaqi.
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