Upper Mesa Falls: Difference between revisions
m Standard headers and general fixes |
No edit summary |
||
Line 9: | Line 9: | ||
| coordinates = {{coord|44|11|16|N|111|19|48|W}} |
| coordinates = {{coord|44|11|16|N|111|19|48|W}} |
||
| elevation = {{convert|5600|ft|m|0}} |
| elevation = {{convert|5600|ft|m|0}} |
||
| type = |
| type = Block |
||
| height = {{convert|114|ft|m|0}}<ref>{{cite web |
| height = {{convert|114|ft|m|0}}<ref>{{cite web |
||
| title = Upper Mesa Falls, Idaho |
| title = Upper Mesa Falls, Idaho |
Revision as of 02:44, 23 April 2010
Upper Mesa Falls | |
---|---|
Location | Fremont County, Idaho |
Coordinates | 44°11′16″N 111°19′48″W / 44.18778°N 111.33000°W |
Type | Block |
Elevation | 5,600 feet (1,707 m) |
Total height | 114 feet (35 m)[1] |
Watercourse | Henrys Fork (Snake River) |
Upper Mesa Falls is a waterfall on the Henrys Fork in the Caribou-Targhee National Forest. Upstream from Lower Mesa Falls, it is roughly 16 miles away from Ashton, Idaho.
Upper Mesa Falls is roughly 114 feet high and 300 feet wide. [2]
Formation
Mesa Falls Tuff, which is the rock over which Upper Mesa Falls cascades, was formed 1.3 million years ago. A cycle of rhyolitic volcanism from the Henrys Fork caldera deposited a thick layer of rock and ash across the area.[3] This layer compressed and hardened over time.
Between 200,000 and 600,000 years ago, the river eroded a wide canyon which was subsequently partly filled with basalt lava flows. The Henrys Fork of the Snake River then carved the channel through the basalt; which is the inner canyon seen today.
External links
- Mesa Falls Recreation Area (USDA Forest Service - Caribou-Targhee National Forest)
References
- ^ "Upper Mesa Falls, Idaho". Public Lands Information Center. 2008. Retrieved 2008-08-13.
- ^ Mesa Falls Near Ashton Idaho
- ^ Shallat, Todd A (1994). Snake: the plain and its people. Boise, ID: Boise State University. p. 53. ISBN 9780932129123. OCLC 31689273.
{{cite book}}
: Unknown parameter|coauthors=
ignored (|author=
suggested) (help)