MORRISON FORMATION

[Mile-marker 9]

From the Fruita interchange on I-70, the overpass leads north into the

town of Fruita, and Colorado Highway 340 leads south about 2½ miles to

the West Entrance of Colorado National Monument. One mile south we cross

the new bridge over the Colorado River; the old bridge formerly

connecting Fruita with the Monument may be seen half a mile upstream.

Just south of the new bridge we see sandstone on the left and green

shale on the right, both part of the Burro Canyon Formation. The high

hill on the left is made up of brightly colored siltstones and mudstones

of the Brushy Basin Member of the Morrison Formation capped by the basal

sandstone of the Burro Canyon Formation. On the southeast side of this

hill is another bronze plaque set in a masonry monument, similar to the

one at Riggs Hill (fig. 39), commemorating the discovery and removal in

1900 by Elmer S. Riggs of a skeleton of the immense dinosaur

_Apatosaurus excelcus_ Marsh. (See figure 23_B_). About 1¾ miles

northwest of the new bridge is the Fruita Paleontological area discussed

on page 50.

Just south of the hill, the highway curves gently to the left across a

relatively flat surface of the Morrison Formation. To the right may be

seen good exposures of the Entrada Sandstone, at the north end of which

curbstones were quarried from thin beds of the white Moab Member for use

in some of the parking areas along Rim Rock Drive. Some of the beds are

ripple marked[36] from wave action along ancient beaches or within

ancient lagoons. Some ripple-marked curbstones from this quarry may be

seen in the parking area at Red Canyon Overlook, and elsewhere in the

Monument.

As we approach the Monument we see that to the left the rock strata are

bent downward toward us along what geologists call a monocline (see

figs. 27 and 30), but to the right may be seen cliffs of dark

Proterozoic rocks surmounted by slopes of the red Chinle Formation and

cliffs of the buff Wingate Sandstone capped by the lowermost beds of the

resistant Kayenta Formation. The bent and broken rocks ahead are well

shown in figure 33.

About 1½ miles south of the Colorado River we reach the T-intersection

noted previously—at the end of the trip from Grand Junction through The

Redlands to the West Entrance of the Monument—and we are ready for our

trip through the Monument.

The Geologic Story of Colorado National Monument Revised Edition · 第 61 / 115 题