Earth:Smithsonian Butte
| Smithsonian Butte | |
|---|---|
 Smithsonian Butte, north aspect | |
| Highest point | |
| Elevation | 6,780 ft (2,070 m) [1] |
| Prominence | 1,400 ft (430 m) [1] |
| Parent peak | Canaan Mountain (7,363 ft)[1] |
| Isolation | 3.21 mi (5.17 km) [1] |
| Coordinates | [ ⚑ ] : 37°06′50″N 113°04′47″W / 37.1138722°N 113.0796642°W [2] |
| Geography | |
  Smithsonian Butte Location in Utah  Smithsonian Butte Smithsonian Butte (the United States) | |
| Location | Canaan Mountain Wilderness Washington County, Utah, United States |
| Parent range | Colorado Plateau |
| Topo map | USGS Smithsonian Butte |
| Geology | |
| Age of rock | Jurassic |
| Type of rock | Navajo sandstone |
| Climbing | |
| Easiest route | class 5.3 climbing[1] |
Smithsonian Butte is a 6,780-foot (2,070 m) elevation summit located in the Canaan Mountain Wilderness of Washington County in southwest Utah, United States.[2]
Description
Smithsonian Butte is situated four miles (6.4 km) southwest of Rockville and four miles south of Zion National Park, and can be seen from Utah State Route 9. Topographic relief is significant as it rises 2,000-feet (610-meters) in one mile on its south side, and 3,000 feet in three miles above the Virgin River on its north aspect which drains precipitation runoff from this mountain. Its nearest higher neighbor is Zion Butte, 3.2 mi (5.1 km) to the southeast, and Eagle Crags are four miles to the east-northeast.[3] The uppermost part of this mountain is composed of light-colored Jurassic Navajo Sandstone which overlays the deep-red sandstone of the Kayenta Formation. This geographical feature was named by geologist Clarence Edward Dutton (1841–1912) for the Smithsonian Institution which had sponsored an exploration of the region, and the toponym was officially adopted in 1934 by the U.S. Board on Geographic Names.[2] From 1875 to 1877, Dutton's field party mapped 12,000 square miles (31,000 km2) of the high plateaus of southern Utah.[4] The saddle between Smithsonian Butte and its parent Caanan Mountain is named Dutton Pass, after him.[5] Access to this mountain is via the Smithsonian Butte National Back Country Byway.[6]
Gallery
South aspect
Smithsonian Butte depicted in a colored frontispiece chromolith by William Henry Holmes, published in "Tertiary History of the Grand Canon District with Atlas", an 1882 monograph by Clarence E. Dutton
Climate
Spring and fall are the most favorable seasons to visit Smithsonian Butte. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total annual precipitation being received during the spring and summer. This desert climate receives less than 10 inches (250 millimeters) of annual rainfall, and snowfall is generally light during the winter.[7]
See also
- Geology of the Zion and Kolob canyons area
- Colorado Plateau
References
- ↑ 1.0 1.1 1.2 1.3 1.4 "Smithsonian Butte - 6,780' UT". https://listsofjohn.com/peak/21575. Retrieved 2020-12-08.
- ↑ 2.0 2.1 2.2 "Smithsonian Butte". United States Geological Survey. https://geonames.usgs.gov/apex/f?p=gnispq:3:::NO::P3_FID:1432576.
- ↑ "Smithsonian Butte, Utah". http://www.peakbagger.com/peak.aspx?pid=56457.
- ↑ Clarence Dutton: Poet of the Grand Canyon, National Geographic
- ↑ "Dutton Pass". United States Geological Survey. https://geonames.usgs.gov/apex/f?p=gnispq:3:::NO::P3_FID:1450343.
- ↑ Peter Massey and Jeanne Wilson, 4WD Trails Southwest Utah, Swagman Publishing Company, 2001, page 49.
- ↑ "Zion National Park, Utah, USA - Monthly weather forecast and Climate data". Weather Atlas. https://www.weather-us.com/en/utah-usa/zion-national-park-climate.
External links
- Weather: Smithsonian Butte
 |  |
