Ads
related to: palo duro canyon geology campground texas
Search results
Results From The WOW.Com Content Network
Palo Duro Canyon is a canyon system of the Caprock Escarpment located in the Texas Panhandle near the cities of Amarillo and Canyon. [2] A large canyon system in the south-central United States, it is roughly 25–40 mi (40–64 km) long and has an average width of 6 mi (9.7 km), but reaches a width of 20 mi (32 km) at places.
The formation crops out along Palo Duro Canyon and the Canadian River and their tributaries. [1] It is also widespread in the Sangre de Cristo Mountains. [4] The formation is interpreted as deposition in a braided stream system. [5] The lower beds at Palo Duro Canyon contain unusual cone-shaped iron concretions that likely formed in the vadose ...
The escarpment's features formed by erosion from rivers and streams, creating arroyos and highly diverse terrain, including the large Palo Duro Canyon southeast of Amarillo, Texas. [1] One will notice the change in elevation of several hundred feet while crossing the Caprock Escarpment on Interstate 40 between Adrian, Texas and San Jon, New Mexico.
The event will celebrate 100 years of Texas State Parks on Saturday, beginning at 7:30 a.m. Enjoy a day in Palo Duro Canyon as Texas State Parks celebrate 100 years Skip to main content
Permian rocks are the best-known of the Texas Paleozoic. They are widespread in north Texas, where their characteristic red beds are spectacularly exposed in Palo Duro Canyon. The strata are also oil-rich where buried in west Texas, such as in the Midland and Odessa region. This crude oil-rich area is known as the Permian Basin.
Caprock Canyons State Park and Trailway is a Texas state park located along the eastern edge of the Llano Estacado in Briscoe County, Texas, United States, approximately 100 miles (160 km) southeast of Amarillo. The state park opened in 1982 and is 15,314 acres (6,197 ha) in size, making it the third-largest state park in Texas. [2] [3]
The canyon is now about 800 feet (240 meters) deep and about 20 miles (30 kilometers) across, making it the second largest canyon in the United States behind Arizona’s Grand Canyon. Comprised of sedimentary rock layers, the oldest exposed rocks in Palo Duro were deposited more than 250 million years ago, during the Permian Period.
Canyon Group/Caddo Creek Formation: Carboniferous: Canyon Group/Graford Formation: Carboniferous: Canyon Group/Palo Pinto Formation: Carboniferous: Canyon Group/Winchell Formation: Carboniferous: Canyon Group/Wolf Mountain Formation: Carboniferous: Canyon Group/Wolf Mountain Shale: Carboniferous: Capitan Formation: Permian: Capote Mountain Tuff ...