Show Navigation
back to search results

Upper Mesa Falls, Henrys Fork of Snake River, Caribou-Targhee National Forest, Idaho, USA.

Upper Mesa Falls plunges 114 feet over a 300 foot wide cliff face along Henrys Fork (also known as North Fork, a tributary of the Snake River) in Caribou-Targhee National Forest in southeastern Idaho, USA. Turn off Highway 47 on the Mesa Falls Scenic Byway about 15 miles north of the city of Ashton. On sunny days from about 9 am until 1 pm, the mist from powerful Upper Mesa Falls creates a beautiful rainbow. The falls flow over Mesa Falls Tuff, which formed 1.3 million years ago. A cycle of rhyolitic volcanism from the Henrys Fork caldera depositing a thick layer of rock and ash which 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 carved a channel through the basalt to create todays inner canyon.

Add to Cart Add to Lightbox Download
Filename
04ID-0051_viewing-platform-Upper-Mesa-Falls.jpg
Copyright
© Tom Dempsey / PhotoSeek.com
Image Size
4000x3000 / 4.0MB
http://www.photoseek.com/
Contained in galleries
Idaho: Mesa Falls, Henrys Fork, Snake River
Upper Mesa Falls plunges 114 feet over a 300 foot wide cliff face along Henrys Fork (also known as North Fork, a tributary of the Snake River) in Caribou-Targhee National Forest in southeastern Idaho, USA. Turn off Highway 47 on the Mesa Falls Scenic Byway about 15 miles north of the city of Ashton. On sunny days from about 9 am until 1 pm, the mist from powerful Upper Mesa Falls creates a beautiful rainbow. The falls flow over Mesa Falls Tuff, which formed 1.3 million years ago. A cycle of rhyolitic volcanism from the Henrys Fork caldera depositing a thick layer of rock and ash which 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 carved a channel through the basalt to create todays inner canyon.
Info