Wasatch Plateau, Utah 2008 |
Axhandle Canyon, where sediments of the North Horn Formation spanning the Paleocene-Eocene boundary are exposed. |
Gabe Bowen, undergraduate assistant Jonathan Foreman, and grad student Justin VanDeVelde near Axhandle Canyon.. |
Ferron Mountain, on the Wasatch Plateau, is composed of early Paleogene carbonates of the Flagstaff Formation. |
Harmonica Point, displaying outcrop of Flagstaff carbonates and underlying North Horn clastic sediments |
On Cove Mountain, carbonates of the Flagstaff Formation are extensively dolomitized, and deposition of evaporite minerals such as gypsum indicate severe desiccation of the ancient lake. |