Tule Valley

Coordinates: 38°57′25″N 113°22′34″W / 38.9568985°N 113.376079°W / 38.9568985; -113.376079
Source: Wikipedia, the free encyclopedia.
Tule Valley
1859: White Valley
Shadow on the eponymic white rocks of the
Tule Valley, November 2009
Tule Valley is located in Utah
Tule Valley
Tule Valley
Millard County, Utah
United States
Tule Valley is located in the United States
Tule Valley
Tule Valley
Tule Valley (the United States)
Floor elevation4,780 ft (1,460 m)
Area248 sq mi (640 km2)
Geography
Coordinates38°57′25″N 113°22′34″W / 38.9568985°N 113.376079°W / 38.9568985; -113.376079

Tule Valley (also known as White Valley) is a valley in Millard County, Utah, United States.[1]

Description

The valley is a north-south trending

Middle Range and the Great Salt Lake Desert, and the south by Wah Wah Valley and the Wah Wah Mountains. The central part of the valley has several knolls, the largest of which is Coyote Knolls. The White Valley name comes from the abundance of white rocks noted by James H. Simpson in 1859.[3] These rocks are mostly Lake Bonneville marls
in the valley floor.

Geographic features

(view west, beyond Sevier Lake)-Arc-shaped south Tule Valley section, (Confusion Range to west, House Range to east); north Tule Valley, at horizon, photo right, February 2011

Tule Valley's most prominent feature may be Coyote Springs, an important spring system for local wildlife and

Tule" is a reference to a swamp plant that probably was found at Coyote Springs during the early exploration of the valley.[3]

The valley itself is very isolated and only has one paved road through its southern end,

playa, the place where all precipitation from the drainage basin collects, since it is an isolated basin and watershed.[4] This is the location of the lowest point in Millard County, Utah.[5]

The Ibex Crags offer "world class" bouldering to climbers. They are located on the eastern edge of the Great Basin.[6]

Geology

The geology of Tule Valley consists of

normal faults on both sides of the valley. The knolls in the valley are horsts of Silurian to Devonian carbonates.[7]

Tule Valley watershed

The Tule Valley

endorheic watershed's volume of surface water averages 4,000 acre-feet (4,900,000 m3).[9]

See also

References

  1. ^ U.S. Geological Survey Geographic Names Information System: Tule Valley
  2. ^
  3. ^ "Surf Your Watershed". EPA.
  4. .
  5. ^ "Ibex Crags". BLM.
  6. .
  7. ^ Davis, Fitzhugh D (2005). "Water Resources of Millard County, Utah" (PDF). Utah Geological Survey. p. 12. Retrieved 2010-05-09.
  8. ^ "West Desert Basin" (PDF). Utah State Water Plan. Retrieved 2010-05-06.


External links

Media related to Tule Valley at Wikimedia Commons