The arid climate of Wingate time was followed by a wet period, when
streams from the northeast gradually covered the sand dunes with mud,
sand, and some gravel. The sand and gravel of the stream channels were
cemented into hard sandstone and conglomerate, and the mud of the flood
plains hardened into red and purple siltstone and mudstone. The
resulting Kayenta Formation makes up the bench between the two cliffs
upon which the Visitor Center, campgrounds, and most of scenic Rim Rock
Drive were built. Here, nature was kind, for this gently sloping bench
was an ideal place to build the road from which to look down into the
deep chasms. The Kayenta also caps the broad mesas between the canyons.
It is about 350 feet thick in eastern Utah, only 45 to 80 feet thick in
the Monument, and it is absent altogether not far east of the Monument.
The reasons for the eastward thinning and ultimate disappearance of the
Kayenta and some younger rocks are given in the next section.
[Illustration: RED CANYON, looking northeast toward Grand Junction
from Red Canyon Overlook. Dark notch at the bottom of the northeast
end of the canyon is known as the Gunsight. Linear feature in the
Grand Valley beyond is the Denver and Rio Grande Western Railroad.
Prominent point near middle of Book Cliffs is Mount Garfield (Fig.
25). Battlement and Grand Mesas form left and right skylines,
respectively. Dark green bush in right foreground is Mormon Tea.
(Fig. 12)]
[Illustration: THIN BEDDED KAYENTA FORMATION protecting underlying
cliff of softer Wingate Sandstone. Rim Rock Drive is on bench of the
Kayenta close to thinner cliff of Entrada Sandstone in background.
Looking northwest from a point northeast of Monument Canyon View.
(Fig. 13)]
As noted earlier, the sandstone beds and lenses of the Kayenta generally
are coarser grained (some even contain small pebbles) and much harder
than the underlying Wingate Sandstone—particularly the lower beds of the
Kayenta, which serve as a protective capping, as shown in figure 13 and
in many of the other photographs. Unlike the dominantly fine grained,
well sorted, windblown sands of the Wingate, the coarser stream-laid
sands of the Kayenta are angular and poorly sorted, so that small grains
fill spaces between larger ones. Moreover, in addition to the calcite
cement (which also holds together the sand grains in the Wingate and
Entrada Sandstones), most of the sand grains and pebbles in the Kayenta
are covered by interconnected “overgrowths” of silica (SiO₂), which make
up about 10 percent of the rocks and serve as a nearly insoluble hard
cement.[20]
The combination of the coarse and fine grains and interlocking silica
“overgrowths” makes the Kayenta one of the most resistant rocks in the
Colorado Plateau.
In distant views of weathered outcrops the Kayenta appears to consist
mainly of thin beds or lenses of sandstone, which indeed it does, but in
some fresh exposures, such as roadcuts, the highly lenticular red
flood-plain deposits form striking features which may wedge out from 3
or 4 feet thick to a featheredge within horizontal distances of only a
few feet (fig. 14).
The Kayenta has yielded fossil bones of dinosaurs and other reptiles in
northeastern Arizona and freshwater shells in eastern Utah. As yet,
however, no fossils have been reported from it in or near the Monument.