Waterfalls Canyon | |
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Waterfalls Canyon at far right with Eagles Rest Peak at center | |
Geography | |
Country | United States |
State | Wyoming |
County | Teton |
Coordinates | 43°46′37″N109°50′29″W / 43.77694°N 109.84139°W Coordinates: 43°46′37″N109°50′29″W / 43.77694°N 109.84139°W [1] |
Lake | Jackson Lake |
Waterfalls Canyon is located in Grand Teton National Park, in the U. S. state of Wyoming. [2] The canyon was formed by glaciers which retreated at the end of the last glacial maximum approximately 15,000 years ago, leaving behind a U-shaped valley. [3] Waterfalls Canyon is south of Ranger Peak and north of Eagles Rest Peak and the entrance to the canyon is along the western shore of Jackson Lake, directly across the lake from the Colter Bay Village. There are several cascades in the canyon, including Wilderness Falls and Columbine Cascade, which descend from an unnamed lake below Ranger Peak.
Grand Teton National Park is an American national park in northwestern Wyoming. At approximately 310,000 acres, the park includes the major peaks of the 40-mile-long (64 km) Teton Range as well as most of the northern sections of the valley known as Jackson Hole. Grand Teton National Park is only 10 miles (16 km) south of Yellowstone National Park, to which it is connected by the National Park Service-managed John D. Rockefeller, Jr. Memorial Parkway. Along with surrounding national forests, these three protected areas constitute the almost 18,000,000-acre (7,300,000 ha) Greater Yellowstone Ecosystem, one of the world's largest intact mid-latitude temperate ecosystems.
Jenny Lake is located in Grand Teton National Park in the U.S. state of Wyoming. The lake was formed approximately 12,000 years ago by glaciers pushing rock debris which carved Cascade Canyon during the last glacial maximum, forming a terminal moraine which now impounds the lake. The lake is estimated to be 256 feet (78 m) deep and encompasses 1,191 acres (482 ha). Jenny Lake is considered to be a major focal point in Grand Teton National Park, with many hiking trails, scenic boat rides, and quick access to the major climbing routes onto the tallest peaks of the Teton Range.
Cascade Canyon is located in Grand Teton National Park, in the U.S. state of Wyoming. The canyon was formed by glaciers which retreated at the end of the last glacial maximum approximately 15,000 years ago. Today, Cascade Canyon has numerous polished glacial erratics, hanging cirques and a U-shape as evidences that demonstrate that glaciers once filled the canyon to a depth of at least 2,000 feet (610 m). Rock debris that was transported out of the canyon by glacial motion formed moraines which now impound the waters of Jenny Lake which is located at the base of the canyon. Cascade Creek now flows where the glaciers once did and the numerous waterfalls, such as the 100-foot (30 m) tall Hidden Falls, found within the gorge are popular destinations with tourists.
Rolling Thunder Mountain is in the northern Teton Range, Grand Teton National Park, Wyoming. The peak is located northwest of Moran Bay on Jackson Lake and access to the peak involves navigating through several miles of backcountry areas of Snowshoe Canyon where there are no maintained trails.
Ranger Peak is in the northern Teton Range, Grand Teton National Park, Wyoming. The peak is located slightly northwest of and across Jackson Lake from Colter Bay Village. Colter Canyon is to the north while Waterfalls Canyon is immediately southeast of the peak, but there are no maintained trails in the area. Access to the summit involves off trail hiking and scrambling. The top of the mountain is more than 4,500 feet (1,400 m) above Jackson Lake.
Doane Peak is in the northern Teton Range, Grand Teton National Park, Wyoming. The peak is located west of and across Jackson Lake from Colter Bay Village. The scenic Waterfalls Canyon is immediately northeast of the peak, but there are no maintained trails in the area. Access to the summit involves off trail hiking and scrambling as the top of the mountain is more than 4,500 feet (1,400 m) above Jackson Lake. The peak is named for Lt. Gustavus Cheyney Doane.
Eagles Rest Peak is in the northern Teton Range, Grand Teton National Park, Wyoming. The peak is located west of and across Jackson Lake from Colter Bay Village. The peak rises dramatically almost 4,500 feet (1,400 m) above Jackson Lake in less than 1 mile (1.6 km). Waterfalls Canyon is to the north of the peak and Snowshoe Canyon lies to the south.
Mount Saint John, height 11,435 feet (3,485 m), is located in the Teton Range, Grand Teton National Park, Wyoming, northwest of Jenny Lake. The mountain towers above the northwest shore of Jenny Lake, and along with Symmetry Spire and Rockchuck Peak, form a massif which looms to the north above Cascade Canyon. The scenic Lake of the Crags, a cirque lake or tarn, is located immediately south of the summit and is accessed by way of Hanging Canyon.
Garnet Canyon is located in Grand Teton National Park in the U.S. state of Wyoming. The canyon was formed by retreating glaciers which reached their last glacial maximum around 15,000 years ago. While Garnet Canyon is a less popular destination for recreational hikers than nearby Cascade Canyon or Death Canyon, it is an important approach to many significant and popular mountaineering climbs including routes found on Grand Teton, Middle Teton, South Teton and Disappointment Peak.
Moran Canyon is located in Grand Teton National Park, in the U. S. state of Wyoming. The canyon lies between Mount Moran to the south and Traverse Peak and Bivouac Peak to the north. Moran Bay, part of Jackson Lake, is at the mouth of the canyon to the east. The canyon was formed by glaciers which retreated at the end of the last glacial maximum approximately 15,000 years ago.
The canyons of the Teton Range lie almost entirely within Grand Teton National Park in the U.S. state of Wyoming. Ranging from 9 miles (14 km) to less than 1 mile (1.6 km) in length and up to 6,000 feet (1,800 m) deep, the canyons were carved primarily by glaciers over the past 250,000 years. 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. 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.
Webb Canyon is located in Grand Teton National Park, in the U. S. state of Wyoming. The canyon was formed by glaciers which retreated at the end of the last glacial maximum approximately 15,000 years ago, leaving behind a U-shaped valley. Webb Canyon is south of Owl Peak and the entrance to the canyon is near the northern reaches of Jackson Lake. Moose Creek flows through much of the 9 miles (14 km) long canyon and the Webb Canyon Trail traverses the length of the canyon to Moose Basin Divide.
Colter Canyon is located in Grand Teton National Park, in the U. S. state of Wyoming. The canyon was formed by glaciers which retreated at the end of the last glacial maximum approximately 15,000 years ago, leaving behind a U-shaped valley. Colter Canyon is north of Ranger Peak and the entrance to the canyon is along the northwestern shore of Jackson Lake.
Snowshoe Canyon is located in Grand Teton National Park, in the U. S. state of Wyoming. The canyon was formed by glaciers which retreated at the end of the last glacial maximum approximately 15,000 years ago, leaving behind a U-shaped valley. Snowshoe Canyon splits into an upper and lower canyon. The source of the upper canyon is near Talus Lake while the south canyon is situated between Rolling Thunder Mountain to the north and Raynolds, Traverse and Bivouac Peaks to the south. Near the fork of north and south Snowshoe Canyon lies Dudley lake. The canyon terminus is at Moran Bay on the southwest side of Jackson Lake, below Eagles Rest Peak.
Avalanche Canyon is located in Grand Teton National Park, in the U. S. state of Wyoming. The canyon was formed by glaciers which retreated at the end of the last glacial maximum approximately 15,000 years ago, leaving behind a U-shaped valley. To the north of Avalanche Canyon lies South Teton, Cloudveil Dome and Nez Perce Peak while to the southwest lie Mount Wister and Veiled Peak. Snowdrift Lake and Lake Taminah are situated at the head of the canyon.
Table Mountain is located in the Teton Range in the U.S. state of Wyoming. The peak is on the border of Grand Teton National Park and the Jedediah Smith Wilderness of Caribou-Targhee National Forest. Table Mountain is west of the south fork of Cascade Canyon and a little more than 1 mile (1.6 km) north of Hurricane Pass.
Wilderness Falls is located in Waterfalls Canyon, Grand Teton National Park in the U.S. state of Wyoming. The cascade drops approximately 250 feet (76 m) in Waterfalls Canyon, fed by unnamed intermittent stream off a glacial lake. The waterfall also receives snowmelt from Ranger Peak to the north and Doane Peak to the southwest. Less than .5 miles (0.80 km) downstream, the same unnamed creek flows over another steep section known as Columbine Cascade The peak time for waterflow is during spring snowmelt and the falls are visible across Jackson Lake from the Colter Bay Village area.
Columbine Cascade is a waterfall in Waterfalls Canyon, a part of the Grand Teton National Park in the U.S. state of Wyoming. The cascade drops approximately 250 feet (76 m) in Hanging Canyon, fed by an unnamed intermittent stream off a glacial lake. The waterfall also receives snowmelt from Ranger Peak to the north Doane Peak to the southwest and Eagles Rest Peak to the south. Less than .5 miles (0.80 km) upstream, the same unnamed creek flows over another steep section known as Wilderness Falls The peak time for waterflow is during spring snowmelt and the falls are visible across Jackson Lake from the Colter Bay Village area.
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