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Setting Hen Butte

Coordinates: 37°16′17″N 109°48′25″W / 37.2712539°N 109.8070119°W / 37.2712539; -109.8070119
From Wikipedia, the free encyclopedia
Setting Hen Butte
South aspect
Highest point
Elevation5,055 ft (1,541 m)[1]
Prominence235 ft (72 m)[1]
Parent peakRooster Butte[1]
Isolation0.42 mi (0.68 km)[1]
Coordinates37°16′17″N 109°48′25″W / 37.2712539°N 109.8070119°W / 37.2712539; -109.8070119[2]
Geography
Setting Hen Butte is located in Utah
Setting Hen Butte
Setting Hen Butte
Location in Utah
Setting Hen Butte is located in the United States
Setting Hen Butte
Setting Hen Butte
Setting Hen Butte (the United States)
LocationValley of the Gods
San Juan County, Utah, U.S.
Parent rangeColorado Plateau
Topo mapUSGS Cigarette Spring Cave
Geology
Age of rockPermian
Mountain typeButte
Type of rockSandstone
Climbing
Easiest routeclass 5.7 climbing[1]

Setting Hen Butte is a 5,055-foot-elevation (1,541-meter) summit in San Juan County, Utah, United States.

Description

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Setting Hen Butte is situated 13.5 miles (21.7 km) west of Bluff, Utah, in the Valley of the Gods, on land administered by the Bureau of Land Management.[3] Precipitation runoff from this iconic landform's slopes drains to the San Juan River via Lime Creek. Access to the butte is via the 17-mile Valley of the Gods Road which passes east this butte. Topographic relief is significant as the summit rises 300 feet (91 meters) above the surrounding terrain in 0.1 mile (0.16 km). This landform's descriptive toponym has been officially adopted by the United States Board on Geographic Names.[2] It is also known as "The Anvil" by some rock climbers.[1] Setting Hen Butte should not be confused with another butte named Setting Hen within the same county but further southwest at Monument Valley.

Geology

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Setting Hen Butte is composed of two principal strata of the Cutler Formation. The bottom layer is slope-forming Halgaito Formation and the upper stratum is cliff-forming Cedar Mesa Sandstone.[4] Cedar Mesa Sandstone is the remains of coastal sand dunes deposited about 270 to 300 million years ago, during the Wolfcampian (early Permian).[5] The buttes of Valley of the Gods are the result of the Halgaito Formation being more easily eroded than the overlaying sandstone. The valley floor is Honaker Trail Formation.[6]

Climate

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Spring and fall are the most favorable seasons to visit Setting Hen Butte. According to the Köppen climate classification system, it is located in a cold semi-arid climate zone with cold winters and hot summers.[7] Summers highs rarely exceed 100 °F (38 °C). Summer nights are comfortably cool, and temperatures drop quickly after sunset. Winters are cold, but daytime highs are usually above freezing. Winter temperatures below 0 °F (−18 °C) are uncommon, though possible. This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and snowfall is generally light during the winter.

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See also

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References

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  1. ^ a b c d e f "Setting Hen Butte - 5,055' UT". listsofjohn.com. Retrieved 2024-08-31.
  2. ^ a b "Setting Hen Butte". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2024-08-31.
  3. ^ Valley of the Gods, Bureau of Land Management, Retrieved 2024-08-31.
  4. ^ Robert Brett O'Sullivan, Geology of the Cedar Mesa-Boundary Butte Area, San Juan County, Utah, U.S. Government Printing Office, 1965, p. 36.
  5. ^ Baars, D.L. (1962). "Permian System of Colorado Plateau". AAPG Bulletin. 46 (2): 149–218. doi:10.1306/BC74376F-16BE-11D7-8645000102C1865D.
  6. ^ Dan S. Chaney, The Carboniferous-Permian Transition, New Mexico Museum of Natural History and Science, 2013, p. 64.
  7. ^ Peel, M. C.; Finlayson, B. L. & McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11 (5): 1633–1644. Bibcode:2007HESS...11.1633P. doi:10.5194/hess-11-1633-2007. ISSN 1027-5606. S2CID 9654551.
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