This field mapping project was undertaken as part of a 3-day field trip to Big Bend National Park with my structural geology class, taught by Dr. John Casey at the University of Houston in the Spring of 2018.
An extensive normal fault, the Chalk Draw Fault, also traverses the northeastern portion of the mapping area. The geology of this area is largely the result of deformation associated with the Laramide orogeny.
Additional information regarding the geologic background of Big Bend can be found here.