Springerville volcanic field

Landform in Apache County, Arizona From Wikipedia, the free encyclopedia

Springerville volcanic field is a monogenetic volcanic field located in east-central Arizona between Springerville and Show Low. The field consists of 405 discrete vents[3] covering approximately 3,000 square kilometers (1,200 sq mi)[2] and is the third-largest such field in the continental United States;[4] only the San Francisco volcanic field and Medicine Lake volcanic field are larger.[5] The total erupted volume is estimated at 90 cubic kilometers (22 cu mi).[6]

Quick Facts Highest point, Coordinates ...
Springerville volcanic field
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Highest point
Coordinates34°15′N 109°34′W[1]
Geography
LocationArizona, United States
Geology
Rock age2.1–0.3 million years[2]
Mountain typeVolcanic field[1]
Volcanic arc/beltBasin and Range Province
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The field is located towards the western end of the Jemez Lineament.[7]

Notable vents

More information Name, Elevation ...
NameElevationCoordinatesLast eruption
Cerro Hueco[1]6,516 feet (1,986 m)[8]34.3161517°N 109.5548218°W / 34.3161517; -109.5548218unknown
Twin Knolls[1]7,379 feet (2,249 m)[9]34.2089319°N 109.9098283°W / 34.2089319; -109.9098283unknown
Wolf Mountain[1]8,284 feet (2,525 m)[10]34.1978216°N 109.7401007°W / 34.1978216; -109.7401007unknown
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Economic resources

The St. Johns carbon dioxide reservoir is located in the northwest part of the Springerville volcanic field and has estimated reserves of 445 billion cubic meters. Effort since the mid-1990s to either extract helium from the reservoir or to ship carbon dioxide to the Permian Basinc for enhanced oil recovery have not come to fruition. A more recent US Department of Energy proposal is to use carbon dioxide from the reservoir as a heat exchange fluid for extraction of geothermal energy from the volcanic field.[6]

See also

References

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