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Geological Formation

Valley of Fire State Park

Sedimentary and Stratigraphic Formations

Valley of Fire State Park covers about 46,000 acres of the Mojave Desert in Clark County, Nevada, roughly 16 miles south of Overton and 50 miles northeast of Las Vegas. Its defining red sandstone, the Aztec Sandstone, formed from shifting sand dunes about 150 million years ago and was later reshaped by complex regional uplift and faulting followed by extensive erosion; the park also contains limestone, shale and conglomerate. The red rock often appears to be on fire when it catches the sun's light, which gave the park its name, and its rough floor and jagged walls display brilliant eroded sandstone formations and fossilized dunes across a basin roughly 4 by 6 miles wide, with elevations ranging from 1,320 to 3,009 feet. The park borders Lake Mead National Recreation Area near the Virgin River confluence to its east, was designated Nevada's oldest state park in 1935, and became a National Natural Landmark in 1968, preserving a geological record spanning some 150 million years. This entity documents Valley of Fire State Park specifically as a geological formation.

Facts
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Protected Status
National Monument or Landmark 1
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Source Valley of Fire State Park (Wikipedia)

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Source Valley of Fire State Park (Wikipedia)
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Sources
1. Valley of Fire State Park (Wikipedia)
  • Wikipedia article lead, protection designation
    ark, as commemorated with Nevada Historical Marker #150. It was designated as a National Natural Landmark in 1968.
  • Caused By: Sedimentation, Article text
    The state park derives its name from red sandstone formations, the Aztec Sandstone, which formed from shifting dunes 150 million years ago.
  • In Discipline: Geomorphology, Lead paragraph
    Valley of Fire State Park is a public recreation and nature preservation area covering nearly 46,000 acres (19,000 ha) located 16 miles (26 km) south of Overton, Nevada.
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