Franklin Butte is a 5,179-foot-elevation (1,579-meter) summit in San Juan County, Utah, United States.
| Franklin Butte | |
|---|---|
 Northwest aspect | |
| Highest point | |
| Elevation | 5,179 ft (1,579 m)[1] |
| Prominence | 359 ft (109 m)[1] |
| Parent peak | Battleship Rock (5,422 ft)[1] |
| Isolation | 0.71 mi (1.14 km)[1] |
| Coordinates | 37°17′12″N 109°49′37″W / 37.2865935°N 109.8269084°W[2] |
| Geography | |
  Franklin Butte Location in Utah  Franklin Butte Franklin Butte (the United States) | |
| Location | Valley of the Gods San Juan County, Utah, U.S. |
| Parent range | Colorado Plateau |
| Topo map | USGS Cigarette Spring Cave |
| Geology | |
| Rock age | Permian |
| Mountain type | Butte |
| Rock type | Sandstone |
| Climbing | |
| First ascent | 1990 |
| Easiest route | class 5.9 climbing[1] |
Description
editFranklin Butte is situated 15 miles (24 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 near this butte. Topographic relief is significant as the summit rises nearly 400 feet (122 meters) above the surrounding terrain in 0.1 mile (0.16 km). This landform's toponym has been officially adopted as Franklin Butte by the United States Board on Geographic Names.[2] It is also known as "Sitting Hen" by some rock climbers, however this should not be confused with nearby Setting Hen Butte.[1] The first ascent of the summit was made in 1990 by John Middendorf and Melissa Wruck.[4]
Geology
editFranklin 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.[5] Cedar Mesa Sandstone is the remains of coastal sand dunes deposited about 270 to 300 million years ago, during the Wolfcampian (early Permian).[6] 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.[7]
Climate
editSpring and fall are the most favorable seasons to visit Franklin Butte. According to the Köppen climate classification system, it is located in a cold semi-arid climate zone with cold winters and hot summers.[8] 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.
See also
editReferences
edit- ^ a b c d e f "Franklin Butte - 5,179' UT". listsofjohn.com. Retrieved 2024-08-31.
- ^ a b "Franklin Butte". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2024-08-31.
- ^ Valley of the Gods, Bureau of Land Management, Retrieved 2024-08-31.
- ^ First Ascent Timeline, deserttowersbook.com, Retrieved 2024-08-31.
- ^ Robert Brett O'Sullivan, Geology of the Cedar Mesa-Boundary Butte Area, San Juan County, Utah, U.S. Government Printing Office, 1965, p. 34.
- ^ Baars, D.L. (1962). "Permian System of Colorado Plateau". AAPG Bulletin. 46 (2): 149–218. doi:10.1306/BC74376F-16BE-11D7-8645000102C1865D.
- ^ Dan S. Chaney, The Carboniferous-Permian Transition, New Mexico Museum of Natural History and Science, 2013, p. 64.
- ^ 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.
External links
edit- Weather: Franklin Butte
