Schoolroom Glacier is a small glacier in Grand Teton National Park in the U.S. state of Wyoming. This Teton Range glacier lies adjacent to the south Cascade Canyon trail at an altitude of 10,400 ft (3,200 m), approximately 12 mi (19 km) from the trailhead at Jenny Lake. The glacier has many of the classic textbook details of a glacier, namely, well defined terminal and lateral moraines, crevasses, a proglacial lake and related features which led to the naming schoolroom.
Middle Teton is the third highest peak in the Teton Range, Grand Teton National Park, Wyoming. The peak is immediately southwest of Grand Teton and the two are separated from one another by the lower saddle, a broad high ridge at 11,600 feet (3,540 m). The Middle Teton Glacier is located on the eastern slopes of the peak. Middle Teton is a classic pyramidal shaped alpine peak and is sometimes included as part of the Cathedral Group of high Teton peaks. The 40-mile (64 km) long Teton Range is the youngest mountain chain in the Rocky Mountains, and began their uplift 9 million years ago, during the Miocene. Several periods of glaciation have carved Middle Teton and the other peaks of the range into their current shapes. From the lower saddle, a distinctive feature known as the black dike appears as a straight line running from near the top of the mountain down 800 feet (240 m). The black dike is a basaltic intrusion that occurred long after the surrounding rock was formed.
Teewinot Mountain is the sixth highest peak in the Teton Range, Grand Teton National Park, Wyoming. The name of the mountain is derived from the Shoshone Native American word meaning "many pinnacles". The peak is northeast of the Grand Teton, and the two are separated from one another by the Teton Glacier and Mount Owen. Teewinot Mountain rises more than 5,500 feet (1,700 m) above Jenny Lake. The 40 miles (64 km) long Teton Range is the youngest mountain chain in the Rocky Mountains, and began their uplift 9 million years ago, during the Miocene. Several periods of glaciation have carved Teewinot Mountain and the other peaks of the range into their current shapes. Broken Falls is one of the tallest cascades in Grand Teton National Park and descends 300 feet (91 m) down the eastern slopes of Teewinot Mountain.
The Cathedral Group is the group of the tallest mountains of the Teton Range, all of which are located in Grand Teton National Park in the U.S. state of Wyoming. The Cathedral Group are classic alpine peaks, with pyramidal shapes caused by glacial motion. The highest peak in the group is Grand Teton, which rises more than 7,000 feet (2,100 m) above Jackson Hole valley, and is the second tallest mountain in Wyoming, after Gannett Peak. The Cathedral Group is separated by other tall peaks of the range by the Cascade Canyon to the north and Avalanche Canyon to the south.
Thor Peak is in the northern Teton Range, Grand Teton National Park, in the U.S. state of Wyoming. Mount Moran is 1 mile (1.6 km) to the east. The summit is the eighth-highest in the Teton Range. Several semi-permanent snowfields as well as the Triple Glaciers are located on the east and northern slopes of the mountain. While the easiest route up the mountain, the south slope, is only rated a class 4, the mountain's remoteness and difficulty of approach make it a challenging mountain to summit.
Teepe Pillar is located in the Teton Range, Grand Teton National Park, Wyoming, immediately south of Grand Teton. The peak is the seventh highest in the Teton Range. Teepe Pillar is separated from Grand Teton by a col which drops sharply to the east and west. Northeast of and well below the summit, the Teepe Glacier is situated in a cirque. From Jackson Hole, Teepe Pillar is difficult to observe except from the northeast as it is hidden from view by Disappointment Peak.
Static Peak is located in the Teton Range, Grand Teton National Park, in the U.S. state of Wyoming. Located .48 miles (0.77 km) southeast of Buck Mountain, the summit is also east of the Alaska Basin Trail, from a point known as Static Peak Divide, the summit can be climbed in a scramble. Below the summit on the north face, a small remnant glacier persists, sheltered from direct sunlight by steep cliffs. Timberline Lake lies to the north of the peak.
Middle Teton Glacier is on the northeast flank of Middle Teton in Grand Teton National Park, Wyoming. The alpine glacier is a popular mountaineering route for ice climbing and for access to the summit of Middle Teton and other peaks to the south. The glacier is at the west end of Garnet Canyon, which is the most popular route used by climbers ascending Grand Teton. The glacier melt feeds streams below including Spalding Falls, an 80 ft (24 m) high cascade. Between 1967 and 2006, Middle Teton Glacier lost approximately 25 percent of its surface area, shrinking from 52 to 39 acres.
Teton Glacier is a mountain glacier located below the north face of Grand Teton in Grand Teton National Park, Wyoming, United States. Its neighbors are Mount Owen to the west and Teewinot Mountain to the north. Teton Glacier is the largest of the twelve named glaciers in the park. In 1971, the glacier was approximately 3,500 ft (1,100 m) long and 1,100 ft (340 m) wide. Between 1967 and 2006, Teton Glacier lost approximately 14 to 20 percent of its surface area, a reduction from 64 to 53 acres.
Skillet Glacier is in Grand Teton National Park, Wyoming, United States. The glacier is situated on the eastern cliffs of Mount Moran and is easily seen from Jackson Hole. The shape of the glacier led to the naming as the uppermost section of the glacier is long and narrow and then broadens abruptly more than halfway down the mountain into a larger area, giving it the shape of a skillet or frying pan. The glacier is one of twelve that remain in Grand Teton National Park and one of five glaciers located on Mount Moran. Mountain climbers consider the Skillet Glacier route to be the fastest and one of the easiest ways to climb Mount Moran, and was the route taken when the peak was first climbed in 1922, though it is rarely used in late summer due to poor footing. On November 21, 1950, A DC-3 crashed into Mount Moran, adjacent to Skillet Glacier, killing all 21 passengers aboard. The remains of the passengers and the plane are still on the mountain.
Falling Ice Glacier is located in the Grand Teton National Park, Wyoming, United States. The glacier is situated on the southeastern cliffs of Mount Moran and can be seen from Jackson Hole. Runoff from the glacier flows into Leigh Lake. The glacier is located in a high altitude cirque and is along one of the major climbing routes to the summit of Mount Moran. All of the existing glaciers in Grand Teton National Park were created during the Little Ice Age (1350–1850 A.D.) and have been in a general state of retreat since the mid-19th century.
Triple Glaciers are in Grand Teton National Park, Wyoming, United States. The glaciers are disconnected from each other and occupy three separate cirques on the northwest face of Mount Moran and northeast of Thor Peak. The glaciers are unofficially referred to as East, Middle and West Triple Glacier.
Petersen Glacier is in Grand Teton National Park, Wyoming, United States. The glacier is in a cirque to the west and above north Cascade Canyon at an altitude of approximately 10,000 feet (3,000 m). The glacier is named after Frank Petersen, one of the first mountaineers to climb Grand Teton in 1898. Runoff from the glacier is heavy in rock flour which turns the waters of Mica Lake turquoise in appearance. The glacier is no longer visible in satellite imagery, indicating it may have disappeared. All of the existing glaciers in Grand Teton National Park were created during the Little Ice Age (1350-1850) and have been in a general state of retreat since the mid-19th century.
Sourdough Glacier is in the Wind River Range, Bridger-Teton National Forest in the U.S. state of Wyoming. Sourdough Glacier is in the Bridger Wilderness, and is part of the largest grouping of glaciers in the American Rocky Mountains. The glacier extends from the north slope of Klondike Peak at an elevation range of 12,800 to 11,800 ft and flows into a proglacial lake.
Minor Glacier is in Bridger-Teton National Forest, in the U.S. state of Wyoming on the west side of the Continental Divide in the northern Wind River Range. Minor Glacier is in the Bridger Wilderness and is part of the largest grouping of glaciers in the American Rocky Mountains. The glacier is situated below the west flank of Gannett Peak, the tallest mountain in Wyoming.
Mammoth Glacier is in the Bridger Wilderness of Bridger-Teton National Forest, in the U.S. state of Wyoming. The glacier is on the west side of the Continental Divide which separates it from Dinwoody Glacier to the east. Mammoth Glacier is the largest glacier on the west side of the Continental Divide of the Wind River Range and occupies a large, north facing cirque on the north slopes of Twin Peaks and just west of Mount Woodrow Wilson. Mammoth Glacier is part of the largest grouping of glaciers in the American Rocky Mountains.
Harrower Glacier is located on the west side of the Continental Divide in the northern Wind River Range in the US state of Wyoming. The glacier is in the Bridger Wilderness of Bridger-Teton National Forest, and is among the largest grouping of glaciers in the American Rocky Mountains. Harrower Glacier flows to the north and is situated in a cirque, below the summit of Knife Point Mountain.
Tiny Glacier is in the Wind River Range, Bridger-Teton National Forest, in the U.S. state of Wyoming. The glacier is situated in a north-facing cirque immediately west of the Continental Divide.
