Navajo Sandstone

Staircase Escalante Monuments)，地質上位於科羅拉多高原(Colorado Plateau)。 納瓦霍砂岩 (Navajo Sandstone)以土丘和山脊的形式暴露在高原上。這些大多是淡紅色的侵蝕遺跡，但在白袋地區中的那些侵蝕遺跡卻被一層白色的岩石層覆蓋，看起來像花椰菜岩（

Jurassic Navajo Sandstone, Geophys. Res. Lett., 37, L22306, doi:10.1029/2010GL044909. ) Seiler, W.M. (August 1, 2008). "Jurassic Navajo sandstone of Coyote

J.A. (October 22, 2006). "Landforms generated by wind erosion of Navajo Sandstone outcrops at The Wave (Colorado Plateau, Utah / Arizona border.) Vol

Vincent , 编. A New Basal Sauropodomorph Dinosaur from the Lower Jurassic Navajo Sandstone of Southern Utah. PLoS ONE. 2010, 5 (3): e9789 [2015-12-12]. PMC 2844413 

Canyon-Vermilion Cliffs Wilderness）的一部分。狼丘又可以分為北狼丘和南狼丘。 Seiler, W. M., Jurassic Navajo sandstone of Coyote Buttes, Utah/Arizona: coloration and diagenetic history,