Gem Glacier is the smallest named glacier in Glacier National Park (U.S.). Located on the east side of the Continental Divide arête known as the Garden Wall, the glacier is situated on the cliff face above the better known Grinnell Glacier. Gem Glacier is a hanging glacier, and drapes down from the north face of the steep arete to which it is attached. Gem Glacier is only 5 acres (0.020 km2) in area and is far below the 25 acres (0.10 km2) threshold often cited as qualifying as an active glacier. Between 1966 and 2005, Gem Glacier lost 30 percent of its acreage and Grinnell Glacier lost 40 percent.
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.
Mount Sacagawea is the eighth-highest peak in the U.S. state of Wyoming and the seventh-highest in the Wind River Range. It was named after Sacagawea, the young Lemhi Shoshone woman who accompanied the Lewis and Clark Expedition as an interpreter and guide. The Upper Fremont Glacier is located southeast and the Sacagawea Glacier is northeast of the mountain. Straddling the Continental Divide, Mount Sacagawea is one mile (1.6 km) northwest of Fremont Peak.
Gooseneck Glacier is located in the Fitzpatrick Wilderness, Shoshone National Forest, in the US state of Wyoming. The glacier is east of the Continental Divide in the northern Wind River Range and on the southeast flank of Gannett Peak, the tallest mountain in Wyoming. Gooseneck Glacier is separated from Dinwoody Glacier by a rocky outcropping and they are part of the largest grouping of glaciers in the American Rocky Mountains.
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.
Heap Steep Glacier is located east of the Continental Divide in the northern Wind River Range in the US state of Wyoming. The glacier is situated in the Fitzpatrick Wilderness of Shoshone National Forest, and is among the largest grouping of glaciers in the American Rocky Mountains. Heap Steep Glacier is in a north facing cirque, below the summit of Sunbeam Peak. A large terminal moraine and small proglacial lake are located below the glacier.
Helen Glacier is located east of the Continental Divide in the northern Wind River Range in the US state of Wyoming. The glacier is located in the Fitzpatrick Wilderness of Shoshone National Forest, and is among the largest grouping of glaciers in the American Rocky Mountains. Helen Glacier flows to the east from a cirque to the northeast of Mount Helen.
Lower Fremont Glacier is east of the Continental Divide in the northern Wind River Range in the U.S. state of Wyoming. The glacier is in the Fitzpatrick Wilderness of Shoshone National Forest, and is among the largest grouping of glaciers in the American Rocky Mountains. Lower Fremont Glacier flows to the southeast and the rapid retreat of this glacier has left behind lateral moraines and a proglacial lake. Lower Fremont Glacier is separated from the Bull Lake Glacier by a moraine and from the Upper Fremont Glacier by cliffs.
Bull Lake Glacier is located immediately east of the Continental Divide in the northern Wind River Range in the U.S. state of Wyoming. The glacier is in the Fitzpatrick Wilderness of Shoshone National Forest, and is among the largest grouping of glaciers in the American Rocky Mountains. Bull Lake Glacier flows to the east and starts below the summit of Jackson Peak. It is adjacent to Lower Fremont Glacier though the two are separated by a moraine.
Knife Point Glacier is on the east side Continental Divide in the northern Wind River Range in the U.S. state of Wyoming. The glacier is in the Fitzpatrick Wilderness of Shoshone National Forest, and is among the largest grouping of glaciers in the American Rocky Mountains. Knife Point Glacier flows to the north and starts below the summit of Knife Point Mountain.
Washakie Glacier is on the east side of the Continental Divide in the southern Wind River Range in the U.S. state of Wyoming. The glacier is in the Popo Agie Wilderness of Shoshone National Forest. Washakie Glacier is situated in a north facing cirque between Mount Washakie and Bair Peak.
Swiftcurrent Glacier is in Glacier National Park in the U.S. state of Montana.The glacier is on the east side of the Continental Divide arête known as the Garden Wall. Swiftcurrent Glacier is one of several glaciers that are being monitored to determine stream flow alterations that occur due to glacial retreat. Compared to other glaciers in Glacier National Park, Swiftcurrent Glacier has experienced relatively slow retreat. As of 2005, the glacier had an area of 55 acres (0.22 km2), a 14 percent reduction since 1966.
Tyndall Glacier is a small cirque glacier in Rocky Mountain National Park in the U.S. state of Colorado. Tyndall Glacier is on the east side of the Continental Divide and in a cirque to the north of Hallett Peak. Tyndall Glacier is both an ice and a rock glacier, with the lower portions of the glacier being composed primarily of rock debris and a small portion of ice.
Grant Glacier is located in the US state of Montana in Flathead National Forest. The glacier is situated in a cirque and lies below the east slopes of Mount Grant. Grant Glacier is 1 mile (1.6 km) southeast of Stanton Glacier and both 5 miles (8.0 km) west of Glacier National Park (U.S.). Images taken of the glacier in 1902 and from the same vantage point in 1998 indicate that the glacier retreated substantially during the 20th Century.
Flanagan Glacier is a glacier in the Pioneer Heights of the Heritage Range, Antarctica, draining east from Thompson Escarpment between the Gross Hills and the Nimbus Hills to the confluent ice at the lower end of Union Glacier. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1961–66, and was named by the Advisory Committee on Antarctic Names for Lieutenant Walter B. Flanagan, an assistant maintenance officer with U.S. Navy Squadron VX-6 at McMurdo Station during Operation Deep Freeze 1963 and 1964.
Hough Glacier is a glacier in central Doyran Heights in the Sentinel Range of Ellsworth Mountains, Antarctica, rising just south of Mount Tuck and flowing east-southeast for 10 nautical miles between Guerrero Glacier and Remington Glacier. It was first mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1957–59, and was named by the Advisory Committee on Antarctic Names for William S. Hough, who made ionosphere studies at South Pole Station in 1957.
Mills Glacier is an alpine glacier near the base of the east mountain face of Longs Peak, in Rocky Mountain National Park in the U.S. state of Colorado.
The Saint Vrain Glaciers are small alpine glaciers located in Roosevelt National Forest in the U.S. state of Colorado. The glaciers are just south of Rocky Mountain National Park and east of the Continental Divide in northeast facing cirques.
Taylor Glacier is a small cirque glacier in Rocky Mountain National Park in the U.S. state of Colorado. Taylor Glacier is on the east side of the Continental Divide and adjacent to Taylor Peak. Taylor Glacier is both an ice and a rock glacier, with the lower portions of the glacier being composed primarily of rock debris and a small portion of ice.
Sphinx Glacier is in the Wind River Range, Bridger-Teton National Forest, in the U.S. state of Wyoming. The glacier is situated on the southern slope of Mount Woodrow Wilson and immediately west of the Continental Divide. The glacier is flanked on the east by a mountain known as The Sphinx. Sphinx Glacier is on the opposite side of the Continental Divide from Dinwoody Glacier.
