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You do the Hoodoos by markthurman53 PALO DURO CANYON
Palo Duro Canyon is located 25 miles southeast of Amarillo Texas, in the Texas panhandle, and is the second-longest canyon in the US; you can guess the first. The creek that runs through the canyon is part of the Prairie Dog Town Fork of the Red River. The canyon formed when the river cut down through the Llano Estacado Plateau as it was uplifted during the Pleistocene Period. This canyon has been called the Grand Canyon of Texas. The rock formations are of the Permian and Triassic periods. The lower Permian section was formed when this was a near-shore shallow marine environment. The upper Triassic layer was formed when this was a stream environment and formed the Sandstone cap rock of the park. Palo Duro gets its name from the Spanish, meaning “hard stick”. This area was first occupied by Native Americans, the Apaches and then replaced by the Comanche and Kiowa. It was visited by Coronado in 1541, then around the 1870’s ranching. It became a state park in the 1930s. A lot of history was glanced over in those last few sentences; more detail is readily available online.
UPPER COMANCHE TRAIL Overview The Upper Comanche Trail is a 3.5-mile trail with its northern trailhead at the Mack Dick Pavilion, which is the first turn-off along the park road when you get down to the canyon floor. The southern terminus is at the Hackberry Campground. The trail follows the Prairie Dog Town Fork of the Red River on its eastern bank 100 to 200 feet up. The trail stays in the Permian/Triassic red Mudstones most of the way, with many hoodoos formed by Triassic weather-resistant sandstones capping earlier Triassic mudstones and shale. Description The Upper Comanche Trail starts out heading north from the Mack Dick Pavilion parking lot and, within 0.2 miles, heads in an easterly direction to cross the Prairie Dog Town Fork of the Red River. There is a wooden bridge to assist in crossing. This river looks more like a creek most of the time, but it has cut a deep narrow ravine that can be difficult to cross without the aid of a bridge. Once past the bridge, the trail starts a gradual 200 foot climb up onto the lower slopes of the eastern cliffs of Palo Duro Canyon. The trail begins in a southerly direction that maintains the rest of the way. Twice along the way, the trail drops back down to near the river level as it crosses Brushy Creek and South Brushy Creek. This trail ends at the Junction with the Soapberry Spur trail and the beginning of the Lower Comanche Trail. This is a signed intersection complete with a map of the trails in Palo Duro. The Soapberry Spur Trail is a short 0.3-mile connector that will take you to the Soapberry day-use area along the park road. This trail is well maintained and signed every tenth mile with placards marked “UC” for Upper Comanche and mileage in tenths. As you walk along this trail, the rocks and hoodoos will keep this easy to walk trail exciting. It is easy to do a three MPH pace, but with all the stopping for photos or just to gaze, the pace will probably be much less. The cliffs to the east are part of the Rylander Fortress Cliffs, and they are quite amazing; they look like large portions of it could come down at any time. One of the more prominent structures along this cliff is the Fractures in the Rock formation visible above the trail near the junction with the Soapberry spur trail junction. Vegetation along the trail consists of grasses, prickly pear, yucca, mesquite, and juniper. Closer to the river are hackberry, willow, and cottonwood. This trail can be quite muddy after heavy rain due to the clays from the Permian and Triassic mudstones, so be prepared to add a few pounds to your boots when hiking the trails if they are muddy. Check out the Official Route and Triplogs. Leave No Trace and +Add a Triplog after your hike to support this local community. One-Way Notice This hike is listed as One-Way. When hiking several trails on a single "hike", log it with a generic name that describes the hike. Then link the trails traveled, check out the example. |