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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.
Palo Duro Canyon State Park: 1976: Armstrong, Randall: state/Texas Department of Parks and Wildlife Spectacular canyon that is an excellent example of a landform created by running water. Santa Ana National Wildlife Refuge: 1966
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.
Texas Outdoor Musical is performed in Palo Duro Canyon State Park in 2023. CANYON — The TEXAS Outdoor Musical recently announced its upcoming 58th season, with tickets on sale now.
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
The Palo Duro basin is centered in the southern Texas Panhandle. It is bounded on the north by the Amarillo Uplift and other structures that separate it from the Anadarko Basin. To the south, it is bounded by the Matador Arch. Its east and west margins are defined by broad structural divides. [2]
This is a list of the National Register of Historic Places listings in Texas' High Plains. The High Plains region is an area of 41 counties defined by the Texas Comptroller for economic reporting in 2022, as mapped here .
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.
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