The formation consists mostly of gray to brown or red sandstone, but with some conglomerate and mudstone. Conglomerate is more common in the middle beds while mudstone is more common in the middle and upper beds. The sandstone is typically crossbedded and is fine-grained in the lower beds and more coarse in the middle and upper beds. The lower sandstone beds tend to form a prominent cliff. The total thickness varies from 45–210 feet (14–64 m). The formation overlies the Tecovas Formation.[1]
The Cuervo Sandstone Member is preempted by the Trujillo Formation.[3]
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 zone.[6]
^ abcdGould, C.N. (1907). "Geology and water resources of the western portion of the Panhandle of Texas". U.S. Geological Survey Water-Supply Paper. 191.
^ abBarnes, V.E. (1983). Geologic atlas of Texas. University of Texas-Austin, Bureau of Economic Geology. p. Tucumcari sheet.
^Asquith, George B.; Cramer, Scott L. (September 1975). "Transverse Braid Bars in the Upper Triassic Trujillo Sandstone of the Texas Panhandle". The Journal of Geology. 83 (5): 657–661. doi:10.1086/628148. S2CID140676202.
^Dinwiddie, C. L.; Chan, M. A.; McGINNIS, R. N.; Myers, J. L.; Holliday, W. S. (February 2011). "Chronicles of vadose zone diagenesis: cone-shaped iron oxide concretions, Triassic Trujillo Formation, Palo Duro Canyon, Texas: Cone-shaped iron oxide concretions". Geofluids. 11 (1): 87–96. doi:10.1111/j.1468-8123.2010.00321.x.
^Ash, Sidney R. (1976). "Occurrence of the Controversial Plant Fossil Sanmiguelia in the Upper Triassic of Texas". Journal of Paleontology. 50 (5): 799–804. JSTOR1303573.