Castle Butte (Valley of the Gods) explained

Castle Butte
Other Name:Eagle Plume Tower
Elevation Ft:5700.
Elevation Ref:[1]
Prominence Ft:560.
Isolation Mi:2.34
Parent Peak:Bears Ears
Map:Utah#USA
Map Size:230
Label Position:top
Location:Valley of the Gods
San Juan County, Utah, U.S.
Range:Colorado Plateau[2]
Coordinates:37.3144°N -109.8542°W
Coordinates Ref:[3]
Topo:USGS Cigarette Spring Cave
Rock:Sandstone
Age:Permian
Type:Butte
First Ascent:1976
Easiest Route: climbing

Castle Butte is a 5700feet summit in San Juan County, Utah, United States.[3]

Description

Castle Butte is situated 16miles west of Bluff, Utah, in the Valley of the Gods, on land administered by the Bureau of Land Management.[4] Precipitation runoff from this iconic landform's slopes drains to the San Juan River via Lime Creek.[2] Access to the butte is via the 17-mile Valley of the Gods Road which makes a change of direction loop around this butte. Topographic relief is significant as the summit rises 600abbr=offNaNabbr=off above the surrounding terrain in 0.15 mile (0.24 km). This landform's toponym has been officially adopted as Castle Butte by the United States Board on Geographic Names,[3] however it is also known as Eagle Plume Tower.[1] [2] The first ascent of the summit was made in 1976 by Bill Forrest and Frank Luptom via the South Face.[5]

Geology

Castle 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.[6] Cedar Mesa Sandstone is the remains of coastal sand dunes deposited about 270 to 300 million years ago, during the Wolfcampian (early Permian).[7] 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.[8]

Climate

Spring and fall are the most favorable seasons to visit Castle Butte. According to the Köppen climate classification system, it is located in a cold semi-arid climate zone with cold winters and hot summers.[9] Summers highs rarely exceed 100°F. 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 are uncommon, though possible. This desert climate receives less than 10abbr=offNaNabbr=off of annual rainfall, and snowfall is generally light during the winter.

See also

External links

Notes and References

  1. Web site: Castle Butte - 5,700' UT. listsofjohn.com. 2024-08-31.
  2. 107302. Eagle Plume Tower, Utah. 2024-08-31.
  3. 1426374. Castle Butte. 2024-08-31.
  4. https://www.blm.gov/visit/valley-gods Valley of the Gods
  5. https://www.deserttowersbook.com/first-ascent-timeline First Ascent Timeline
  6. Robert Brett O'Sullivan, Geology of the Cedar Mesa-Boundary Butte Area, San Juan County, Utah, U.S. Government Printing Office, 1965, p. 34.
  7. Baars . D.L. . Permian System of Colorado Plateau . AAPG Bulletin . 1962 . 46 . 2 . 149–218 . 10.1306/BC74376F-16BE-11D7-8645000102C1865D.
  8. https://books.google.com/books?id=5f4oCgAAQBAJ&pg=PA64&dq=honaker+trail+formation+valley+of+the+gods&hl=en&newbks=1&newbks_redir=0&sa=X&ved=2ahUKEwjljrKI556IAxWHJTQIHXDQLDAQuwV6BAgFEAY#v=onepage&q=honaker%20trail%20formation%20valley%20of%20the%20gods&f=false Dan S. Chaney, The Carboniferous-Permian Transition
  9. Peel, M. C. . Finlayson, B. L. . McMahon, T. A. . amp . 2007 . Updated world map of the Köppen−Geiger climate classification . Hydrol. Earth Syst. Sci. . 11 . 5 . 1633–1644 . 10.5194/hess-11-1633-2007 . 2007HESS...11.1633P . 9654551 . 1027-5606. free .