The Geologic Story of Palo Duro CanyonMatthews, William Henry
Science
The Geologic Story of Palo Duro Canyon
Matthews, William Henry
Geology -- Texas -- Palo Duro State Park; Palo Duro State Park (Tex.)
After viewing the canyon from Coronado Lodge, one should take the scenic
drive on Park Road 5. This paved, all-weather road descends the
northwest rim of the canyon and continues on to the turnaround at Cow
Camp, a distance of about 8 miles. Although the present scenic drive was
completed in 1951, the path that it follows is essentially that which
was laid out by Colonel Charles Goodnight when he established Palo Duro
ranch in 1876. The road descends to the canyon floor in a series of
well-engineered turns, but because it drops some 800 feet in little more
than a mile it is wise to use second or low gear on the descent. One
should also observe the posted speed limits (10 to 20 miles per hour)
and keep to the right side of the road at all times.
In the 800-foot drop from rim to floor, the complete geologic section of
the canyon is traversed, as one passes from the Pleistocene sands
through the Ogallala, Trujillo, and Tecovas Formations, before reaching
the Quartermaster Formation which is exposed in the canyon floor. Each
of these geologic formations is discussed elsewhere in this publication
(pp. 16-28).
_Pioneer Amphitheatre_ (3).—
Upon reaching the canyon floor, Park Road 5 flattens out and from this
point it is but a short distance to the Pioneer Amphitheatre, one of the
canyon’s newest and most popular attractions. Here, located at the foot
of a colorful 600-foot cliff, is a remarkable 1500-seat outdoor theatre
of latest design (fig. 23). Each evening during a ten-week summer
season, a symphonic drama portraying the history of the Texas Panhandle
is presented in the amphitheatre. Information about these productions
can be obtained at the Park Entrance, Coronado Lodge, and other points
within the park.
[Illustration: Fig. 21. The entrance gate to Palo Duro Canyon State
Park.]
[Illustration: Fig. 22. Coronado Lodge on the canyon’s northwest rim
affords panoramic views of the canyon.]
_Sad Monkey Train Ride_ (4).—
The Sad Monkey Railroad begins—and ends—at Sad Monkey, Texas, a small
“community” that lies at the foot of Triassic Peak (fig. 24). Unlike
most miniature railroads, the Sad Monkey Special is not a “kiddie” ride.
Instead, this 2-mile journey provides an opportunity to get away from
the road for a closer look at the geologic formations exposed along the
track. There are especially good views of the Spanish Skirts (fig. 26),
Catarina Cave (fig. 27), and Triassic Peak (fig. 25). These, and other
features of geologic interest, are pointed out by an experienced
lecturer who also presents a brief review of the geologic history of the
area.
_Triassic Peak_ (5).—
Long used by Indians and ranchers as a Palo Duro landmark, the canyon
visitor will find Triassic Peak to be equally useful as a geologic
landmark. When viewed from the Sad Monkey Railroad Terminal, the south
face of Triassic Peak clearly reveals three of the four major geologic
formations of the canyon (fig. 25).
Public-domain text, read in full here on John Shaqi.
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