| Scimitar Glacier | |
|---|---|
  Scimitar Glacier | |
| Type | Mountain glacier |
| Coordinates | 48°06′29″N121°07′49″W / 48.10806°N 121.13028°W Coordinates: 48°06′29″N121°07′49″W / 48.10806°N 121.13028°W [1] |
| Length | .9 mi (1.4 km) |
| Terminus | Barren rock |
| Status | Retreating |
Sitkum Glacier is located on the west slopes of Glacier Peak in the U.S. state of Washington. [2] As is true with all the glaciers found on Glacier Peak, Sitkum Glacier is retreating. [3] Sitkum Glacier is immediately south of Scimitar Glacier.
Glacier Peak or Dakobed is the most isolated of the five major stratovolcanoes of the Cascade Volcanic Arc in the U.S state of Washington. Located in the Glacier Peak Wilderness in Mount Baker–Snoqualmie National Forest, the volcano is visible from the west in Seattle, and from the north in the higher areas of eastern suburbs of Vancouver such as Coquitlam, New Westminster and Port Coquitlam. The volcano is the fourth tallest peak in Washington state, and not as much is known about it compared to other volcanoes in the area. Local Native Americans have recognized Glacier Peak and other Washington volcanoes in their histories and stories. When American explorers reached the region, they learned basic information about surrounding landforms, but did not initially understand that Glacier Peak was a volcano. Positioned in Snohomish County, the volcano is only 70 miles (110 km) northeast of downtown Seattle. From locations in northern Seattle and northward, Glacier Peak is closer than the more famous Mount Rainier, but as Glacier Peak is set farther into the Cascades and almost 4,000 feet (1,200 m) shorter, it is much less noticeable than Mount Rainier.
The Admiralty Mountains is a large group of high mountains and individually named ranges and ridges in northeastern Victoria Land, Antarctica. This mountain group is bounded by the Ross Sea, the Southern Ocean, and by the Dennistoun, Ebbe, and Tucker glaciers. The mountain range is situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.
The Usarp Mountains are a major Antarctic mountain range, lying west of the Rennick Glacier and trending north to south for about 190 kilometres (118 mi). The feature is bounded to the north by Pryor Glacier and the Wilson Hills.
The Sør Rondane Mountains are a group of mountains about 100 miles (160 km) long with main peaks rising to 3400 m, between the Queen Fabiola Mountains and Wohlthat Mountains in Queen Maud Land. They were discovered and photographed from the air by members of the Lars Christensen Expedition (LCE) on February 6, 1937, and named after Rondane, a mountain massif in southern Norway. The mountains and their constituent features were mapped in greater detail and named in 1957 by Norwegian cartographers working with air photos taken by U.S. Navy Operation Highjump, 1946–47.
Connie Glacier is in Bridger-Teton National Forest, in the U.S. state of Wyoming on the west of the Continental Divide in the Wind River Range. Connie Glacier is in the Bridger Wilderness, and is part of the largest grouping of glaciers in the American Rocky Mountains. The glacier is situated in a cirque on the north slope of Yukon Peak and terminates in a proglacial lake.
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.
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.
Agassiz Glacier is in Glacier National Park in the U.S. state of Montana. It is named after Louis Agassiz, a Swiss-American glaciologist. The glacier is situated in a cirque to the southeast of Kintla Peak west of the Continental Divide. Agassiz Glacier is one of several glaciers that have been selected for monitoring by the U.S. Geological Survey's Glacier Monitoring Research program, which is researching changes to the mass balance of glaciers in and surrounding Glacier National Park.
Boulder Glacier is located in the U.S. state of Montana in Glacier National Park (U.S.). The glacier is situated to the north of Boulder Peak and west of the Continental Divide. Between 1966 and 2005, Boulder Glacier lost more than 75 percent of its surface area. As of 2005 the glacier was measured to cover only 13 acres (0.053 km2), and no longer met the 25 acres (0.10 km2) threshold often cited as the minimal area to qualify as an active glacier.
Shepard Glacier is a glacier remnant (glacieret) In Glacier National Park in the U.S. state of Montana. The glacieret is immediately southeast of Cathedral Peak. Shepard Glacier was one of a number of glaciers that have been documented by the United States Geological Service (USGS) to have retreated significantly in Glacier National Park. Shepard Glacier was measured in 2009 to have decreased to less than 25 acres (0.10 km2), considered to be a minimal size to qualify as being considered an active glacier. Between 1966 and 2005, Shepard Glacier lost 56 percent of its surface area.
Two Ocean Glacier is in Glacier National Park in the U.S. state of Montana. The glacier is situated on the west side Continental Divide below Vulture Peak at an average elevation of 8,400 feet (2,600 m) above sea level. As of 2005, Two Ocean Glacier consisted of numerous ice patches covering a total of 67 acres (0.27 km2) and is more than 35 percent smaller than it was in 1966.
Hansen Glacier is a tributary glacier 10 nautical miles long, flowing northeast from Mount Tuck between Veregava Ridge and Doyran Heights to join Dater Glacier west of Dickey Peak, in the Sentinel Range of the Ellsworth Mountains in Antarctica. 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 Herbert L. Hansen, a meteorologist at South Pole Station in 1957.
Litz Glacier is a glacier flowing northeast from the vicinity of Smith Peak and Litz Bluff in north-central Thurston Island, Antarctica. The glacier enters the west part of Peale Inlet north of the Guy Peaks. It was named by the Advisory Committee on Antarctic Names after A.K. Litz, Chief Photographer's Mate in the Eastern Group of Operation Highjump, which obtained aerial photographs of this glacier and adjacent coastal areas, 1946–47.
Henderson Glacier is a glacier approximately 7 nautical miles long in the Enterprise Hills of the Heritage Range, Antarctica. It flows northeast from Schoeck Peak and Hoinkes Peak to enter Union Glacier just east of Mount Rossman. Henderson Glacier 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 Felix E. Henderson, a United States Antarctic Research Program meteorologist at Eights Station in 1965.
Sky Top Glacier is in the Beartooth Mountains in the U.S. state of Montana. The glacier is situated at an elevation of 11,600 feet (3,500 m) in a cirque to the west of Granite Peak, the tallest summit in Montana. The glacier covers approximately 25 acres (0.10 km2) and a small proglacial lake is near the glacier terminus.
Donnellan Glacier is a steep valley glacier fed by highland ice adjacent to Opalchenie Peak and Fukushima Peak on Vinson Plateau, the summit plateau of Vinson Massif, in the Sentinel Range of the Ellsworth Mountains, Antarctica. The glacier flows west-southwestward from Opalchenie Peak along the northwest side of Mount Slaughter into Nimitz Glacier.
Scimitar Glacier is located on the west and northwest slopes of Glacier Peak in the U.S. state of Washington. As is true with all the glaciers found on Glacier Peak, Scimitar Glacier is retreating. During the Little Ice Age Scimitar Glacier was connected to Kennedy Glacier to the north. From about 1850 to 1946, the glacier retreated 5,250 ft (1,600 m), but advanced 1,738 ft (530 m) during a colder and wetter period lasting until about 1980. Scimitar Glacier has retreated since, but due to the thickness of the ice at the terminus, had not lost much of its length through the year 2005.
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