Echo Tower

Last updated
Echo Tower
Fisher Towers - Echo Tower.jpg
Northwest aspect
Highest point
Elevation 5,784 ft (1,763 m) [1]
Prominence 396 ft (121 m) [1]
Parent peak Kingfisher Tower [2]
Isolation 0.18 mi (0.29 km) [2]
Coordinates 38°43′13″N109°18′03″W / 38.72027°N 109.30084°W / 38.72027; -109.30084 [1]
Geography
USA Utah relief location map.svg
Red triangle with thick white border.svg
Echo Tower
Location in Utah
Usa edcp relief location map.png
Red triangle with thick white border.svg
Echo Tower
Echo Tower (the United States)
CountryUnited States
State Utah
County Grand
Parent range Colorado Plateau [1]
Topo map USGS Fisher Towers
Geology
Age of rock Permian
Mountain type Pillar
Type of rock Sandstone
Climbing
First ascent 1966

Echo Tower is a 5,784-foot-elevation (1,763-meter) pillar in Grand County, Utah, United States.

Contents

Description

Echo Tower is located 17 miles (27 km) northeast of Moab, Utah, in the Fisher Towers, on land administered by the Bureau of Land Management. Echo ranks as the third-steepest peak in the United States. [3] Topographic relief is significant as the summit rises 800 feet (244 meters) above the tower's base. Precipitation runoff from the tower drains to Onion Creek which empties into the Colorado River, approximately three miles to the west. Access is via Fisher Towers Road from Route 128, and hiking the Fisher Towers Trail. Echo Tower is briefly shown (as a parachute flies by) in the opening scene of the film Austin Powers in Goldmember . [4]

Climbing

The first ascent of the summit was made on October 19, 1966, by Harvey T. Carter, Fred Beckey, and Eric Bjørnstad via the class 5.8 North Chimney route. [5] [6] [7]

Other rock-climbing routes on Echo Tower:

Geology

Echo Tower is set on a fin and is composed of sandstone and mudstone of the Permian Cutler Formation. [15] The reddish coloration of the rock is a result of varying amounts of hematite. [16]

Climate

Spring and fall are the most favorable seasons to visit Echo Tower. According to the Köppen climate classification system, it is located in a cold semi-arid climate zone with cold winters and hot summers. [17] 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

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References

  1. 1 2 3 4 "Echo Tower, Utah". Peakbagger.com.
  2. 1 2 "Echo Tower - 5,980' UT". listsofjohn.com. Retrieved 2024-09-13.
  3. ↑ Contiguous US Steepness List, listsofjohn.com, Retrieved 2024-09-13.
  4. ↑ Fisher Towers - Hittle Bottom Campground, sceen-it.com, Retrieved 2024-09-13.
  5. ↑ First Ascent Timeline, deserttowersbook.com, Retrieved 2024-09-13.
  6. ↑ North America, United States, Utah, Echo Tower, Fisher Towers, Fred Beckey, 1967, American Alpine Journal, americanalpineclub.org
  7. ↑ Stewart M. Green, Rock Climbing Utah, Rowman & Littlefield, 2012, ISBN   9780762792849, p. 165.
  8. ↑ Run Amok, Mountain Project, Retrieved 2024-09-13.
  9. ↑ Cameron Burns, Selected Climbs in the Desert Southwest: Colorado and Utah, The Mountaineers Books, 1999, ISBN   9780898866575, p. 71.
  10. ↑ Phantom Sprint, Mountain Project, Retrieved 2024-09-13.
  11. 1 2 1995 American Alpine Journal, 1995, p. 158.
  12. ↑ The Iron Chef, Mountain Project, Retrieved 2024-09-13.
  13. ↑ Sidewinder, Mountain Project, Retrieved 2024-09-13.
  14. ↑ Bad Religons, Mountain Project, Retrieved 2024-09-13.
  15. ↑ Castle Valley Overview United States of America, Virtual 3D Geoscience, v3geo.com, Retrieved 2024-09-05.
  16. ↑ GeoSights: Fisher Towers – The towering red rock sculptures of Grand County, Utah, Carl Ege, Utah Geological Survey, Retrieved 2024-09-12.
  17. ↑ 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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