Named by Bowers (1972); Inferred to be Paleocene, possibly Eocene by Goldstrand (1994). Pine Hollow Formation is referenced in Davis and Pollock (2000):
Bowers, W.E., 1972, The Canaan Peak, Pine Hollow, and Wasatch
Formations in the Table Cliff region, Garfield County, Utah, IN Contributions to general geology: U.S. Geological Survey Bulletin, 1331-B, p. B1-B39.
Goldstrand, P.M., 1994, Tectonic development of Upper Cretaceous to Eocene strata of southwestern Utah: Geological Society of America Bulletin, v. 106, no. 1, p. 145-154.
Davis, G. H., and Pollock, G. L., 2000, Geology of Bryce Canyon
National Park, Grand County, Utah: In Geology of Utah's Parks and Monuments,
Sprinkel, D.A., Chidsey, T.C., and Anderson, P.B., editors, Utah Geological
Association Publication 28., p. 37-60.