Willow Mountain is the most spectacular display of rock joints in the southern Big Bend area.[8] The mountain mass is an intrusiveplug, which cooled below the surface and was subsequently uncovered by erosion. On cooling, the rock mass contracted and was uniformly jointed. After erosion uncovered this mass, weathering and erosion removed the soft areas to expose the joint pattern.
^Charles E. Corry, Geology of the Solitario, Trans-Pecos Texas, Geological Society of America, 1990, ISBN9780813722504, p. 95.
^ abWillow Mountain, Texas State Historical Association, Retrieved 2024-11-07.
^Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11. ISSN1027-5606.
^A Gazetteer of Texas, Henry Gannett, U.S. Government Printing Office, 1904, p. 174.