Canyons of the Teton Range explained

The canyons of the Teton Range lie almost entirely within Grand Teton National Park in the U.S. state of Wyoming. Ranging from to less than in length and up to deep, the canyons were carved primarily by glaciers over the past 250,000 years.^[1] The canyons in the Teton Range descend in altitude generally west to east and many have lakes at their outlets. The lakes were created by terminal moraines left behind by the now retreated glaciers.^[2] A few of the canyons have small glaciers that were created mostly during the Little Ice Age (1550-1850). Fast retreating Schoolroom Glacier is a tiny glacier located at the head of the South Cascade Canyon. Most of the canyons have streams from which rain and snowmelt flow towards Jackson Hole valley, and due to the sometimes rapid altitude descent, waterfalls are common. The canyons offer the easiest hiking access into the Teton Range.^[3]

Teton Range canyons within Grand Teton National Park

• Webb Canyon^[4] is long and originates at several alpine lakes near the western boundary of Grand Teton National Park. Moose Creek flows through the canyon and empties into Jackson Lake.
• Colter Canyon^[5] is long and originates north of Ranger Peak.
• Waterfalls Canyon^[6] is long. Several cascades near the head of the canyon descend from an unnamed lake.
• Snowshoe Canyon^[7] has a north and south fork. This long canyon lies between Eagles Rest Peak and Rolling Thunder Mountain to the north and Raynolds Peak, Traverse Peak and Bivouac Peak to the south.
• Moran Canyon^[8] is long and is situated south of Raynolds Peak, Traverse Peak and Bivouac Peak and north of Mount Moran. The canyon outlet is at Moran Bay on Jackson Lake.
• Leigh Canyon^[9] is long and lies between Mount Moran to the north and Mount Woodring to the south. The canyon outlet is at Leigh Lake.
• Paintbrush Canyon^[10] is long and the canyon outlet is near Leigh Lake. The popular but very strenuous Paintbrush-Cascade Loop hike traverses through the canyon.^[3]
• Hanging Canyon^[11] is a long canyon which is immediately south of Mount Saint John.
• Cascade Canyon^[12] is long and splits into the North Cascade and South Cascade canyons from its outlet at Jenny Lake. The canyon is more than deep in places as the north slopes of Mount Owen and Grand Teton tower above the canyon. One of the most visited canyons in Grand Teton National Park, Cascade Canyon can be accessed by trail via a loop hike around Jenny Lake or a boat shuttle which provides easier access to Inspiration Point and the nearly cascade known as Hidden Falls. Schoolroom Glacier is located at the head of the South Cascade Canyon while Lake Solitude lies at the end of the North Cascade Canyon.^[3]
• Valhalla Canyon^[13] extends northward from the northwestern slopes of Grand Teton and ends within Cascade Canyon.

• Garnet Canyon^[14] is long and is the most commonly used canyon by mountaineers to access the upper slopes of Grand Teton, Middle Teton and other peaks of the Cathedral Group. The terminal moraine at the outlet of Garnet Canyon impounds Bradley Lake.
• Avalanche Canyon^[15] is long. Both Snowdrift Lake and Lake Taminah are within the canyon. South Teton and Cloudveil Dome are to the north and Mount Wister is to the south of the canyon. The terminal moraine at the outlet of Avalanche Canyon impounds Taggart Lake.
• Death Canyon^[16] is a popular hiking destination. More than long, the canyon provides access from Phelps Lake to the Teton backcountry region.
• Open Canyon^[17] is long and extends from Mount Hunt to Phelps Lake.
• Granite Canyon^[18] is the southernmost canyon in Grand Teton National Park. Granite Canyon is almost long and is flanked to the south by Rendezvous Mountain.

Teton Range canyons outside Grand Teton National Park

• Jensen Canyon^[19] is located to the south of Grand Teton National Park in Bridger-Teton National Forest.
• Phillips Canyon^[20] is located to the south of Grand Teton National Park in Bridger-Teton National Forest.
• Teton Canyon^[21] is on the west slopes of the Teton Range and within Caribou-Targhee National Forest.
• Darby Canyon^[22] is on the west slopes of the Teton Range and within Caribou-Targhee National Forest.

See also

• Geology of the Grand Teton area

Notes and References

1. Web site: Love . J.D. . John C. Reed, Jr. . Creation of the Teton Landscape: The Geologic Story of Grand Teton National Park . Quaternary-Time of Ice, More Lakes and Continued Crustal Disturbance . National Park Service . 2011-05-15 . dead . https://web.archive.org/web/20121108041202/http://www.nps.gov/history/history/online_books/grte/grte_geology/sec9.htm . 2012-11-08 .
2. Web site: Park Geology. Geology Fieldnotes. National Park Service. 2011-05-15. 2011-06-13. https://web.archive.org/web/20110613170423/http://www.nature.nps.gov/geology/parks/grte/index.cfm. dead.
3. Web site: Day Hikes. National Park Service. pdf. 2011-05-15.
4. 1604018. Webb Canyon. 2011-05-15.
5. 1598866. Colter Canyon. 2011-05-15.
6. 1604011. Waterfalls Canyon. 2011-05-15.
7. 1594521. Snowshoe Canyon. 2011-05-15.
8. 1601555. Moran Canyon. 2011-05-15.
9. 1600890. Leigh Canyon. 2011-05-15.
10. 1601993. Paintbrush Canyon. 2011-05-15.
11. 1600190. Hanging Canyon. 2011-05-15.
12. 1598649. Cascade Canyon. 2011-05-15.
13. 1603904. Valhalla Canyon. 2011-05-15.
14. 1599911. Garnet Canyon. 2011-05-15.
15. 1597845. Avalanche Canyon. 2011-05-15.
16. 1599168. Death Canyon. 2011-05-15.
17. 1601936. Open Canyon. 2011-05-15.
18. 1600020. Granite Canyon. 2011-05-15.
19. 1600605. Jensen Canyon. 2011-05-15.
20. 1602118. Phillips Canyon. 2011-05-15.
21. 1603579. Teton Canyon. 2011-05-15.
22. 1599114. Darby Canyon. 2011-05-15.