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Death Valley National Park, California. Typical stand of burroweed near the road along Furnace Creek Wash, above Corkscrew Canyon. Circa 1960 Death Valley National Park, California. Typical stand of burroweed near the road along Furnace Creek Wash, above Corkscrew Canyon. This shrub grows on the high parts of the gravel fans above the main stands of creosote bush. Burroweed grows in washes between bare surfaces on the fans with desert pavement. Commonly, desert holly grows along the sides of the washes, and burroweed on the bottom. Photo by J.R. Stacy, circa 1960. Figure 18, U.S. Geological Survey Professional paper 509. Sketch of photo. Categories: Image; Tags: Death Valley National Park, Hunt, C.B. Collection, Photographers, Sketches, photo print Death Valley National Park, California. Desert pavement on surface of old gravel (No. 2 gravel). circa 1960. Death Valley National Park, California. Desert pavement on surface of old gravel (No. 2 gravel). The pavement is composed of closely spaced angular stones that are fragments of the large rounded ones that originally comprised the gravel deposit. Photo by J.R. Stacy, circa 1960. Figure 49, U.S. Geological Survey Professional paper 494-A. Sketch of photo. Categories: Image; Tags: Death Valley National Park, Hunt, C.B. Collection, Photographers, Sketches, photo print Death Valley National Park, California. Desert holly, half a mile northwest of the Park's service area, forms nearly pure stands along the lower edges of the gravel fans where they border the salt pan. Circa 1960 Death Valley National Park, California. Desert holly, half a mile northwest of the Park's service area, forms nearly pure stands along the lower edges of the gravel fans where they border the salt pan. Photo by J.R. Stacy, circa 1960. Figure 9, U.S. Geological Survey Professional paper 509. Sketch of photo. Categories: Image; Tags: Death Valley National Park, Hunt, C.B. Collection, Photographers, Sketches, photo print Death Valley National Park, California. The last big earthquake in Death Valley accompanied the faulting that produced this escarpment near the road just south of the Furnace Creek fan. Circa 1960. Death Valley National Park, California. The last big earthquake in Death Valley accompanied the faulting that produced this escarpment near the road just south of the Furnace Creek fan. The fault movement occurred about 2,000 years ago, and since that time the fault escarpment has been buried where it crossed the mouths of the canyons issuing from the Tertiary formations at the north end of the Black Mountains. Photo by J.R. Stacy, circa 1960. Figure 72, U.S. Geological Survey Professional paper 494-A. Sketch of photo. Categories: Image; Tags: Death Valley National Park, Formations, Hunt, C.B. Collection, Photographers, Sketches, All tags... photo print, Fewer tags