Coordinates: 43°29′26″N 112°44′18″W / 43.4904351°N 112.7382169°W / 43.4904351; -112.7382169

Middle Butte

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Middle Butte
File:Middle Butte, ne.jpg
Northeast aspect
Highest point
Elevation6,391 ft (1,948 m)[1][2]
Prominence1,061 ft (323 m)[2]
Parent peakEast Butte (6,572 ft)[3]
Isolation3.73 mi (6.00 km)[3]
CoordinatesLua error in Module:Coordinates at line 489: attempt to index field 'wikibase' (a nil value).[4]
Geography
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CountryUnited States of America
StateIdaho
CountyBingham
Parent rangeSnake River Plain
Rocky Mountains[2]
Topo mapUSGS Middle Butte
Geology
Rock ageQuaternary[5]
Mountain typeCryptodome[5]
Rock typeBasalt[5]

Middle Butte is a 6,391-foot elevation (1,948 m) summit located in Bingham County, Idaho, United States.

Description

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Middle Butte is situated 40 miles east of Craters of the Moon National Monument and Preserve, 35 miles west of the community of Idaho Falls, and can be seen from Highway 20 midway between Idaho Falls and Arco at milepost 271. Middle Butte, so named because it is positioned between Big Southern Butte and line parent East Butte, were all landmarks for early explorers and pioneers.[4] Middle Butte is set on land belonging to the Idaho National Laboratory. Topographic relief is modest as the summit rises over 1,000 feet (300 meters) above the Eastern Snake River Plain in one-half mile. This landform's toponym has been officially adopted by the United States Board on Geographic Names.[4] Lewis and Clark recorded seeing Middle Butte during their 1805 expedition, noting its unusual shape in their journals.

Geology

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Middle Butte is a cryptodome composed of basalt which formed when an underlying mass of rhyolitic magma pushed up overlying layers of basalt of the Snake River Plain, but the magma never broke the surface.[6] This manner of formation is different than that of East Butte where rhyolitic magma did break through the surface layer of basalt.

Climate

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Middle Butte is located in a cold semi-arid climate zone with warm summers and cold winters (Köppen BSk).[7] Winter temperatures can drop below 0 °F with wind chill factors below −20 °F. Precipitation is relatively sparse.

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See also

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References

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  1. ^ United States Geological Survey topographical map - Middle Butte
  2. ^ a b c Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  3. ^ a b Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  4. ^ a b c Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  5. ^ a b c Scott S. Hughes (1999), Guidebook to the Geology of Eastern Idaho, Idaho Museum of Natural History Publisher, Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value)., p. 146
  6. ^ The Land Volcanoes Made: the Buttes of the Snake River Plain from Idaho Falls to Arco, Idaho, railsback.org
  7. ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
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