Conglomeratic channel fill in Browns Park Formation at measured section B-14, unit 7, near mouth of Jesse Ewing Canyon. Channel is about 10 feet deep at base of conglomeratic sequence, 64 feet thick. Conglomerate is derived mainly from Uinta Mountain Group but contains pebbles and cobbles derived from Red Creek Quartzite and from reworked limestones of Paleozoic age. Daggett County, Utah. ca. 1953. Figure 39 in U.S. Geological Survey. Professional paper 490. 1965. Professional Paper-0490

Digital File:hwr00096

ID. Hansen, W.R. 96