Upper Mesa Falls

{{Infobox waterfall

| name = Upper Mesa Falls

| photo = Mesa_Falls_4.JPG

| photo_width = 200

| photo_caption = Upper Mesa Falls in June 2008

| location = Fremont County, Idaho

| coords = {{coord|44|11|16|N|111|19|48|W}}

| elevation = {{convert|5600|ft|m|0}}

| type = Block

| height = {{convert|114|ft|m|0}}{{cite web

| title = Upper Mesa Falls, Idaho

| publisher = Public Lands Information Center

| year = 2008

| url = http://www.publiclands.org/explore/site.php?search=YES&back=Search%20Results&id=7121

| access-date = 2008-08-13}}

| width =

| height_longest =

| average_width =

| number_drops =

| average_flow =

| watercourse = Henrys Fork (Snake River)

| world_rank =

}}

Upper Mesa Falls is a waterfall on the Henrys Fork in the Caribou-Targhee National Forest. Upstream from Lower Mesa Falls, it is roughly {{convert|16|mi|km}} away from Ashton, Idaho.{{cite gnis|392638|Upper Mesa Falls|January 15, 2015}}

Upper Mesa Falls is roughly {{convert|114|ft|m}} high and {{convert|200|ft|m}} wide.{{cite web |url=http://www.westyellowstonenet.com/attractions/mesa_falls.php |title=Mesa Falls Near Ashton Idaho}}

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.{{cite book

| last = Shallat

| first = Todd A

|author2=Bentley, E B

| title = Snake: the plain and its people

| publisher = Boise State University

| year = 1994

| location = Boise, ID

| pages = 53

| oclc = 31689273

| isbn = 978-0-932129-12-3}}

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.

See also

References

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