Mount Pennell

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Mount Pennell
Mount Pennell.jpg
Mount Pennell, south aspect
Highest point
Elevation 11,413 ft (3,479 m) [1]
Prominence 3,568 ft (1,088 m) [1]
Parent peak Mount Ellen (11,527 ft) [2]
Isolation 10.62 mi (17.09 km) [2]
Coordinates 37°57′24″N110°47′27″W / 37.9566537°N 110.7907081°W / 37.9566537; -110.7907081 [3]
Naming
Etymology Joseph Pennell
Geography
USA Utah relief location map.svg
Red triangle with thick white border.svg
Mount Pennell
Location in Utah
Usa edcp relief location map.png
Red triangle with thick white border.svg
Mount Pennell
Mount Pennell (the United States)
CountryUnited States
State Utah
County Garfield
Parent range Henry Mountains
Topo map USGS Mount Pennell
Geology
Rock age Oligocene
Mountain type Laccolith
Rock type Igneous
Climbing
Easiest route class 2 scrambling [2]

Mount Pennell is a prominent 11,413-foot (3,478 m) elevation summit located in eastern Garfield County, Utah, United States. [3] Mount Pennell is the second-highest mountain in the Henry Mountains, following Mount Ellen, 10.6 miles to the north. It is situated in a dry, rugged, and sparsely settled region east of Capitol Reef National Park, on primitive land administered by the Bureau of Land Management. Several deep canyons cut the sides of the mountain, which on the higher slopes supports oak, Ponderosa pine, subalpine fir, spruce, Douglas fir, and aspen. [4] Precipitation runoff from this mountain drains into tributaries of the nearby Colorado River.

Contents

History

This mountain was first called Un-chu'-ka-ret by the native Paiute. [5]

Almon Harris Thompson served as chief topographer and geographer of John Wesley Powell's Second Geographical Expedition (1871–1875) when he named Mount Ellen after his wife, Ellen Powell Thompson, and Mount Pennell was later named for his friend Joseph Pennell (1857–1926), an American artist and author. [6] [7]

The American geologist Grove Karl Gilbert surveyed this area in 1875 and 1876, and published his findings in 1879 as a monograph, The Geology of the Henry Mountains. The term laccolith was first applied as laccolite by Gilbert after his study of intrusions of diorite in the Henry Mountains. [8]

Climate

Spring and fall are the most favorable seasons to visit Mount Pennell. 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.

See also

Mount Pennell from Lake Powell at Bullfrog-Halls Crossing Mount Pennell, Henry Mountains.jpg
Mount Pennell from Lake Powell at Bullfrog-Halls Crossing

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References

  1. 1 2 "Mount Pennell". Peakbagger.com. Retrieved 2020-09-12.
  2. 1 2 3 "Pennell, Mount - 11,420' UT". listsofjohn.com. Retrieved 2020-09-12.
  3. 1 2 "Mount Pennell". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2020-09-12.
  4. "Mt. Pennell | Bureau of Land Management".
  5. Don D. Fowler and Catherine S. Fowler, Anthropology of the Numa, Smithsonian Institution Press, 1971, page 141.
  6. Don D. Fowler and Catherine S. Fowler, Anthropology of the Numa, Smithsonian Institution Press, 1971, page 141.
  7. Pete Klocki and Tiffany Mapel, A Wild Redhead Tamed: A Brief History of the Colorado River and Lake Powell, 2009, page 85.
  8. Aber, James S. "Grove Karl Gilbert". academic.emporia.edu. Retrieved 29 December 2018.