The Caprock Escarpment is a prominent geological feature located in the Texas Panhandle. It marks the boundary between the high plains to the east and the rolling plains to the west. This escarpment is characterized by steep cliffs and flat-topped mesas, formed by erosion of softer rock layers beneath harder caprock, primarily composed of sandstone. The escarpment stretches approximately 200 miles and is part of the larger Llano Estacado region. It is home to diverse ecosystems, including grasslands and canyons, and supports various wildlife. The area is also significant for agriculture and ranching, contributing to the local economy.