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
Another 2½ miles around the south rim of Red Canyon and the head of
Columbus Canyon takes us to the junction with the paved county road
known as the DS Road, which leads south and southwest to Glade Park and
to the head of No Thoroughfare Canyon. This important intersection will
be included in trips through Glade Park and around the head of No
Thoroughfare Canyon, so it will be discussed later. Meanwhile, we will
continue our trip eastward from this intersection. About a third of a
mile to the northeast is a large parking area, with a path leading to a
fenced overlook at the rim of Columbus Canyon for viewing Cold Shivers
Point—perhaps the most aptly titled feature in the Monument (fig. 53). A
primitive path leads from the overlook to the toadstool-shaped platform
at upper right, on which some visitors dare to stand, but not me. When
the old, steep Serpents Trail was the only route for autos to ascend
from the East Entrance, barrels of water were kept at this parking area
to quench the thirst of boiling radiators.
HEAD OF SERPENTS TRAIL
[Mile-marker 31]
After leaving the parking area, the downgrade on the Kayenta Formation
begins to steepen to the northeast until it becomes advisable to shift
into second gear. In about half a mile we descend a series of steep
switchbacks cut into the Wingate Sandstone on the steepening Ladder
Creek monocline (figs. 8, 29), and we reach the present upper end of the
old Serpents Trail (fig. 54), which is now an interesting foot trail. As
noted earlier, it is convenient to hike down this steep 2½-mile trail
and to have one member of the party drive ahead and await the hikers at
the parking area in the Devils Kitchen Picnic Area, near the foot of the
trail. One of many rewarding views seen during the hike is shown in
figure 55, another was seen in figure 10.
[Illustration: COLD SHIVERS POINT, looking north from fenced
overlook on east edge of Columbus Canyon. Named feature is
toadstool-shaped rock at upper right. Note dark Proterozoic rocks in
canyon bottom. (Fig. 53)]
[Illustration: TOP OF OLD SERPENTS TRAIL, looking northeast from
switchbacks above tunnel. Top of trail is seen at sign on lower
right. Grand Mesa forms right skyline. (Fig. 54)]
Public-domain text, read in full here on John Shaqi.
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