The Geologic Story of Colorado National Monument: Revised EditionLohman, Stanley William
Science
The Geologic Story of Colorado National Monument: Revised Edition
Lohman, Stanley William
Colorado National Monument (Colo.); Geology -- Colorado -- Colorado National Monument
[Illustration: LOOKING NORTHEAST FROM OLD SERPENTS TRAIL, before
1950 when the trail was still used by autos and trucks. One of John
Otto’s old foot trails joins the old road at lower middle. Although
no thick lenses of sandstone appear in the Salt Wash Member of the
Morrison Formation in figure 21, in this view a lens about 50 feet
thick begins just around the corner near the base of the high bluff
across No Thoroughfare Canyon and is seen extending as far to the
left as the normally dry wash that drains the canyon. When water
flows down the wash after thundershowers (see p. 118) or from
melting snow, the sandstone lens takes in water (recharge) which
moves slowly down the dip of the lens to the northeast and supplies
several artesian wells. In turn, the light band of the Entrada
Sandstone beneath the cottonwood trees at the right middle and the
dark patch of Wingate Sandstone at the extreme lower right are
recharged in like manner, and they supply water to artesian wells to
the northeast. As the older and deeper sandstones on the right take
in water at higher altitudes, the water in them is under greater
artesian head when tapped by wells. If you think you see covered
wagons near the middle of the photograph arranged in a circle for
defense against attack by Indians, you are correct—a Western movie
was about to be filmed. (Fig. 55)]
[Illustration: Petroglyph]
[Illustration: SOUTH PORTAL OF TUNNEL THROUGH WINGATE SANDSTONE, on
west side of No Thoroughfare Canyon above East Entrance. (Fig. 56)]
FOOT OF SERPENTS TRAIL
Just beyond the lowest switchback shown in figure 54, we penetrate the
Wingate Sandstone through a tunnel, the south portal of which is shown
in figure 56. After we drive through a deep cut in the Wingate Sandstone
just south of the tunnel, we cross the entire red Chinle Formation, then
descend a series of switchbacks in old Proterozoic rocks. The Chinle
Formation is crossed again near the foot of the hill, where it is about
80 feet thick,[39] then we recross the Wingate Sandstone and Kayenta
Formation to the parking area in the Devils Kitchen Picnic Area, near
the foot of the old Serpents Trail.
DEVILS KITCHEN
[Mile-marker 32]
An improved marked trail leads southward from parking area at the foot
of the Serpents Trail, crosses No Thoroughfare Canyon, and continues as
an unimproved trail to the Devils Kitchen, a view of which is shown in
figure 57. The petroglyphs shown in figure 4 are northeast of this
parking area. Those interested in seeing them should inquire at the
ranger station or checking station at the East Entrance.
EAST ENTRANCE
Public-domain text, read in full here on John Shaqi.
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