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The oldest rocks in the area that now includes Death Valley National Park are extensively metamorphosed by intense heat and pressure and are at least 1700 million years old. These rocks were intruded by a mass of granite 1400 Ma (million years ago) and later uplifted and exposed to nearly 500 million years of erosion.
nps.gov /deva. Death Valley National Park is a national park of the United States that straddles the California – Nevada border, east of the Sierra Nevada. The park boundaries include Death Valley, the northern section of Panamint Valley, the southern section of Eureka Valley and most of Saline Valley. The park occupies an interface zone ...
Titus Canyon is a narrow gorge in the Grapevine Mountains near the eastern boundary of Death Valley National Park. It features megabreccia and other rock formations, petroglyphs, and wildlife of various kinds, including bighorn sheep. Along the road to the canyon stands Leadfield, a ghost town dating to the 1920s.
Zabriskie Point. Coordinates: 36°25′12″N 116°48′40″W. Zabriskie Point is a part of the Amargosa Range located east of Death Valley in Death Valley National Park in California, United States, noted for its erosional landscape. It is composed of sediments from Furnace Creek Lake, which dried up 5 million years ago—long before Death ...
The Walker Lane is a geologic trough roughly aligned with the California / Nevada border southward to where Death Valley intersects the Garlock Fault, a major left lateral, or sinistral, strike-slip fault. The north-northwest end of the Walker Lane is between Pyramid Lake in Nevada and California's Lassen Peak [1][2] where the Honey Lake Fault ...
Death Valley. Death Valley is a desert valley in Eastern California, in the northern Mojave Desert, bordering the Great Basin Desert. It is thought to be the hottest place on Earth during summer. [3] Death Valley's Badwater Basin is the point of lowest elevation in North America, at 282 feet (86 m) below sea level. [1]
Death Valley National Park. The Ubehebe Craters are a volcanic field in the northern Death Valley of California, consisting of 14–16 craters in a 3-square-kilometre (1.2 sq mi) area. The largest of the craters is the 800 metres (2,600 ft) wide and 235 metres (771 ft) deep Ubehebe Crater. Many of the craters, though, are partially buried and ...
Wood Canyon Formation. The Wood Canyon Formation is a geologic formation in the northern Mojave Desert of Inyo County, California and Nye County and Clark County, Nevada. [1][2] It can be seen in the Panamint Range and Funeral Mountains adjoining Death Valley, within Death Valley National Park; and in the Spring Mountains in Clark County. [1]