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Yellowstone Plateau Volcanic Field

From Wikipedia, the free encyclopedia

Yellowstone Plateau Volcanic Field
Mount Sheridan, the highest peak in the Yellowstone Plateau Volcanic Field, from Heart Lake
Highest point
Elevation10,313[1] ft (3,143 m)
Coordinates44°28′16″N 110°30′07″W / 44.471031°N 110.501862°W / 44.471031; -110.501862 (Yellowstone Plateau Volcanic Field)
Geography
Location
Parent rangeRocky Mountains
Topo mapUSGS Yellowstone National Park
Geology
Age of rock~2,080,000–70,000 years[3]
Mountain typeComplex volcano, volcanic plateau and volcanic field[2]
Last eruptionapproximately 631,000 years ago (caldera-forming); 70,000 years ago (in the caldera)
Climbing
Easiest routeHike/auto/bus

The Yellowstone Plateau Volcanic Field, also known as the Yellowstone Supervolcano or the Yellowstone Volcano, is a complex volcano, volcanic plateau and volcanic field located mostly in the western U.S. state of Wyoming but also stretches into Idaho and Montana. It is a popular site for tourists.

Map of the United States showing volcanic ash fall from Yellowstone eruptions in some case covering over one third of the country.
Map of Yellowstone Volcano ash beds

The plateau developed through three volcanic cycles spanning two million years that included some of the world's largest known eruptions. The eruption of the >2,500 km2 (970 sq mi) Huckleberry Ridge Tuff about 2 million years ago created the more than 75 km (47 mi) long Island Park Caldera. The second cycle concluded with the eruption of the Mesa Falls Tuff around 1.3 million years ago, forming the 25 km (16 mi) wide Henry's Fork Caldera at the western end of the first caldera. Activity subsequently shifted to the present Yellowstone Plateau and culminated 630,000 years ago with the eruption of the >1,000 km2 (390 sq mi) Lava Creek Tuff and the formation of the present 45 km × 75 km (28 mi × 47 mi) caldera. Resurgent doming then occurred at both the NE and SW sides of the caldera and voluminous 1,000 km2 (390 sq mi) intracaldera rhyolitic lava flows were erupted between 150,000 and 70,000 years ago. Phreatic eruptions produced local tephras during the early Holocene. The caldera presently contains one of the world's largest hydrothermal systems including the world's largest concentration of geysers.[4] Much of the plateau is located within Yellowstone National Park.

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Transcription

References

  1. ^ "Yellowstone Plateau". Peakbagger.com.
  2. ^ "Yellowstone". Global Volcanism Program. Smithsonian Institution. Retrieved December 31, 2008.
  3. ^ USGS. "The evolution of the Yellowstone Plateau Volcanic Field: Past, present, and future!". United States Geological Survey.
  4. ^ "Volcanic History of the Yellowstone Plateau Volcanic Field". U.S. Geological Survey. Retrieved 2007-02-18.

44°28′16″N 110°30′07″W / 44.471031°N 110.501862°W / 44.471031; -110.501862

This page was last edited on 8 February 2024, at 15:42
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