Island Park Caldera

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Island Park Caldera

Diagram of Island Park and Henry's Fork Caldera
Elevation 2,805 m (9,203 ft)
Location
Location Fremont County, Idaho, USA
Coordinates 44°20′N 111°20′W / 44.33°N 111.33°W / 44.33; -111.33
Geology
Type Caldera
Last eruption 2.1 myr
Left part of Island Park Caldera, with the circular structure of Henry's Fork Caldera in the center of this image

The volcanic feature commonly called the Island Park Caldera in the states of Idaho and Wyoming, U.S., is actually two calderas, one nested inside the other.[1] The Island Park Caldera is the older and much larger caldera, with approximate dimensions of 58 miles (93 km) by 40 miles (64 km). Its ashfall is the source of the Huckleberry Ridge Tuff that is found from southern California to the Mississippi River near St. Louis. This supereruption (2500 cubic kilometers) occurred 2.1 Ma and produced 2,500 times as much ash as the 1980 Mount St. Helens eruption.

The caldera clearly visible today is the later Henry's Fork Caldera that is the source of the Mesa Falls Tuff. It was formed in an eruption of more than 280 cubic kilometers 1.3 million years ago. The two nested calderas share the same rim on their western sides, but the older Island Park Caldera is much larger and more oval and extends well into Yellowstone Park.[2] The Island Park Caldera is sometimes referred to as the First Phase Yellowstone Caldera or the Huckleberry Ridge Caldera.

To the southwest of the caldera lies the Snake River Plain, which was formed by a succession of older calderas marking the path of the Yellowstone hotspot. The Plain is a depression, sinking under the weight of the volcanic rocks that formed it, through which the Snake River winds. Other observable volcanic features in the Plain include: the Menan Buttes, the Big Southern Butte, Craters of the Moon, the Wapi Lava Field and Hell's Half Acre.

These calderas are in an area called Island Park that is known for beautiful forests, large springs, clear streams, waterfalls, lakes, ponds, marshes, wildlife, and fishing. Harriman State Park is located in the caldera. Snowmobiling, fishing, and Nordic skiing, and wildlife viewing are popular activities in the area. The peaks of the Teton Range to the southeast are visible from places in the caldera.

[edit] See also

[edit] References

  1. ^ Wood and Kienle, 1990, Volcanoes of North America: United States and Canada Cambridge University Press, 354p., p.263-267
  2. ^ Newhall and Daniel Dzurisin, 1988, "Historical Unrest at Large Calderas of the World", U.S. Geological Survey Bulletin 1855.

[edit] External links

Coordinates: 44°20′N 111°20′W / 44.33°N 111.33°W / 44.33; -111.33

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