Excellent descriptions of geology, soils, climate, vegetation, and history ol the study area are provided in Gieseker et al (1953), Cole (1 956), Bayless (1969), and Jorgensen (1979). The following summarizes those accounts while adding details particularly relevant to antelope eeology. Location The Yellow Water Triangle (266 mi^) is near the geographie center of Montana (Fig. 2); 62% of the land area falls within Petroleum County and 38% within Fergus County (Jorgensen 1979). The area is enclosed by U.S. Highway 87 (20 mi from Grass Range to FlatwiUow Road), Montana Highway 200 (23 mi from Grass Range to Winnett), Montana Highway 244 (18 mi from Winnett to FlatwiUow Road), and FlatwiUow Road (5 mi from U.S. Highway 87 to Montana Highway 244). Drainages of two minor permanent streams (FlatwiUow and McDonald Creeks) and three intermittent streams (Pike, Elk, and YeUow Water Creeks) paraUel one another across the study area. The name "YeUow Water" is derived from the discoloration of the stream by yellowish bentonite from certain geologieal formations (Jorgensen pers. comm.). Geology and Soils Relief slopes upward from east to west. AU geologieal formations tilt easterly and thus have lower strata exposed at higher elevations toward the west. Elevations range from 3,000 ft at Winnett to 4,500 ft atop Button Butte in the northwest quarter near Grass Range. The topography varies from flat to gently roUing along an elevational gradient that increases an average of approximately 20 ft/mi along MeDonald Creek between Winnett and Grass Range. Most topographical rehef stems from geological relics of hiUs, buttes, and ridges or stream erosion vaUeys, coulees, and draws cut below the level of the prairie plateau. Most of these topographic relics have immediate elevational changes of less than 100 ft.