Continental Glacier is in Bridger-Teton and Shoshone National Forests, in the U.S. state of Wyoming and straddles the Continental Divide in the northern Wind River Range. Continental Glacier is in both the Bridger and Fitzpatrick Wildernesses, and is part of the largest grouping of glaciers in the American Rocky Mountains. Continental Glacier is situated at an elevation range of 13,100 to 11,200 feet and forms a nearly unbroken icefield over 3 miles (4.8 km) in length along a high altitude plateau to the north of Downs Mountain. Immediately east of Continental Glacier lies East Torrey Glacier.
The Ellen Glacier is a glacier in the central Sentinel Range of the Ellsworth Mountains of Antarctica. It drains the eastern slopes of Mount Anderson and Long Gables and flows generally southeast for 22 nautical miles to Barnes Ridge, where it leaves the range and enters the south flowing Rutford Ice Stream.
The Usarp Mountains is a major Antarctic mountain range, lying westward of the Rennick Glacier and trending N-S for about 190 kilometres (118 mi). The feature is bounded to the north by Pryor Glacier and the Wilson Hills. Its important constituent parts include Welcome Mountain, Mount Van der Hoeven, Mount Weihaupt, Mount Stuart, Mount Lorius, Smith Bench, Mount Roberts, Pomerantz Tableland, Daniels Range, Emlen Peaks, Helliwell Hills and Morozumi Range.
Downs Glacier is located in Shoshone National Forest, in the U.S. state of Wyoming on the east of the Continental Divide in the Wind River Range. The glacier is 1 mi (1.6 km) south of Downs Mountain and sits at an elevation of between 12,600 and 11,200 ft. Downs Glacier is one of many glaciers found in the Fitzpatrick Wilderness, and is part of the largest grouping of glaciers in the American Rocky Mountains.
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.
J Glacier is located in Bridger-Teton National Forest, in the US state of Wyoming on the west of the Continental Divide in the Wind River Range. J Glacier is in the Bridger Wilderness, and is part of the largest grouping of glaciers in the American Rocky Mountains. J Glacier flows down from the northwest slope of Klondike Peak and a proglacial lake has formed at the toe of the glacier.
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.
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.
Baby Glacier is in the Bridger Wilderness of Bridger-Teton National Forest, in the U.S. state of Wyoming. The glacier is immediately west of the much larger Mammoth Glacier, both of which are on the west side of the Continental Divide in the northern Wind River Range. The glacier occupies a north facing cirque and flows northward from the slopes of Mount Whitecap. Baby Glacier is in the Bridger Wilderness and is part of the largest grouping of glaciers in the American Rocky Mountains.
Stroud Glacier is west of the Continental Divide in the northern Wind River Range in the U.S. state of Wyoming. The glacier is located in the Bridger Wilderness of Bridger-Teton National Forest, and is among the largest grouping of glaciers in the American Rocky Mountains. The glacier is situated in a north facing cirque, below the summit of Bow Mountain.
Twins Glacier is west of the Continental Divide in the northern Wind River Range in the U.S. state of Wyoming. The glacier is located in the Bridger Wilderness of Bridger-Teton National Forest, and is among the largest grouping of glaciers in the American Rocky Mountains. The glacier is situated in a northeast facing cirque, below the summit of Winifred Peak.
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.
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.
Shipley Glacier is a glacier, 25 miles (40 km) long, in the north-central Admiralty Mountains of Antarctica. The glacier drains the northern slopes of Mount Adam and flows along the east wall of DuBridge Range to Pressure Bay on the north coast of Victoria Land. Some of the glacier bypasses Pressure Bay and reaches the sea west of Flat Island. The seaward end of the glacier was first mapped by the Northern Party, led by Victor Campbell, of the British Antarctic Expedition, 1910-13. Named by Campbell for Sir Arthur Shipley, master of Christ's College, Cambridge, England, at the suggestion of Priestley. The entire glacier was mapped by United States Geological Survey (USGS), 1960-63.
Irwin Glacier is a steep tributary glacier in the Bowers Mountains of Antarctica, draining northeast from Edlin Névé and at the terminus coalescing with Montigny Glacier, with which it enters the larger Graveson Glacier. The glacier was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for Carlisle S. Irwin, a former glaciologist who participated in the study of Meserve Glacier in 1966–67. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
Jaburg Glacier is a broad glacier draining westward between the Dufek Massif and the Cordiner Peaks in the Pensacola Mountains of Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1956–66. The glacier was named by the Advisory Committee on Antarctic Names after Lieutenant Conrad J. Jaburg, U.S. Navy, a helicopter pilot with the Ellsworth Station winter party, 1957.
Piegan Glacier is in Glacier National Park in the U.S. state of Montana. The glacier is situated in a cirque on the southeast slope of Piegan Mountain and just below the summit at an elevation between 8,800 and 8,200 ft above sea level. The glacier covered an area of approximately 62 acres (0.25 km2) in 2005, a 10 percent reduction in its surface area since 1966. Comparing images of the glacier taken in 1930 with those from 1998, indicates that the glacier experienced relatively little change during that period.
Grimes Glacier is a steep glacier descending from the east side of Anderson Massif, in the Heritage Range of the Ellsworth Mountains of Antarctica. 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 Master Chief Equipmentman Paul D. Grimes, U.S. Navy, who supervised the construction crews during relocation of Williams Air Field at McMurdo Sound in the closing month of U.S. Navy Operation Deep Freeze 1965.
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.
