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 (Tahoma), 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 Sentinel Range is a major mountain range situated northward of Minnesota Glacier and forming the northern half of the Ellsworth Mountains in Antarctica. The range trends NNW-SSE for about 185 km (115 mi) and is 24 to 48 km wide. Many peaks rise over 4,000 m (13,100 ft) and Vinson Massif (4892 m) in the southern part of the range is the highest elevation on the continent.
The Leverett Glacier is about 50 nautical miles (90 km) long and 3 to 4 nautical miles wide, flowing from the Antarctic Plateau to the south end of the Ross Ice Shelf through the Queen Maud Mountains. It is an important part of the South Pole Traverse from McMurdo Station to the Admundson–Scott South Pole Station, providing a route for tractors to climb from the ice shelf through the Transantarctic Mountains to the polar plateau.
The Amundsen Glacier is a major Antarctic glacier, about 7 to 11 km wide and 150 km (80 nmi) long. It originates on the Antarctic Plateau where it drains the area to the south and west of Nilsen Plateau, then descends through the Queen Maud Mountains to enter the Ross Ice Shelf just west of the MacDonald Nunataks.
The UK Antarctic Place-Names Committee is a United Kingdom government committee, part of the Foreign and Commonwealth Office, responsible for recommending names of geographical locations within the British Antarctic Territory (BAT) and the South Georgia and the South Sandwich Islands (SGSSI). Such names are formally approved by the Commissioners of the BAT and SGSSI respectively and published in the BAT Gazetteer and the SGSSI Gazetteer maintained by the Committee. The BAT names are also published in the international Composite Gazetteer of Antarctica maintained by SCAR.
Mount Gould is a peak on the Continental Divide in Glacier National Park, Montana, United States. It is the highest point of the Garden Wall, a distinctive ridge of the Lewis Range. It is most notable for its huge, steep east face, which drops 4,000 ft (1,220 m) in only one-half mile (0.8 km). This face provides a backdrop to Grinnell Lake, and is often photographed.
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.
Andrews Glacier is an alpine glacier in a cirque below Otis Peak in Rocky Mountain National Park in the U.S. state of Colorado. The glacier extends from Andrews Pass at nearly 12,000 to 11,700 feet with some perennial snow extending to Andrews Tarn, a small proglacial lake. When images of the glacier taken in the early 1900s are compared with those of the early 2000s, Andrews Glacier is showing a negative glacier mass balance which indicates the glacier is retreating.
The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s.
The Land Glacier is a broad, heavily crevassed glacier, about 35 nautical miles long, descending into Land Bay in Marie Byrd Land, Antarctica. It was discovered by the United States Antarctic Service (1939–41) and named for Rear Admiral Emory S. Land, Chairman of the United States Maritime Commission.
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.
Pollock Mountain is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Pollock Mountain is situated along the Continental Divide and is one of the peaks along the Garden Wall and is approximately .6 miles (0.97 km) south of Bishops Cap. The mountain was named by Ross Carter for William C. Pollock, a member of the Indian Commission who along with Walter M. Clements and George Bird Grinnell negotiated with the Blackfeet to consummate the treaty that enabled the Federal Government to purchase the "Ceded Strip" of land, which included all of what is now Glacier National Park to the east of the Continental Divide.
Ahern Glacier is in Glacier National Park in the U.S. state of Montana. The glacier was named after George Patrick Ahern. Ahern Glacier is situated on a ridge between Ipasha Peak to the north and Ahern Peak to the south at an elevation between 8,800 feet (2,700 m) and 8,000 feet (2,400 m) above sea level, immediately east of the Continental Divide. Meltwater from the glacier feeds Ahern Glacier Falls, a waterfall which descends an estimated 1,680 feet (510 m) in one sheer drop to a talus slope below en route to Helen Lake. Between 1966 and 2005, Ahern Glacier lost 13 percent of its surface area.
The Flowers Hills are a triangular shaped group of hills, 34.6 kilometres (21.5 mi) long and 11.5 kilometres (7.1 mi) wide, with peaks of 1,240 metres (4,070 ft) and 1,504 metres (4,934 ft), extending along the eastern edge of the Sentinel Range, Ellsworth Mountains, Antarctica. The hills are bounded by Hansen Glacier and Dater Glacier to the west and north, Rutford Ice Stream to the east and Sikera Valley to the southwest, and separated from Doyran Heights to the west-southwest by Kostinbrod Pass. Their interior is drained by Lardeya Ice Piedmont and Valoga Glacier.
Overcoat Glacier is in the U.S. state of Washington. Overcoat Glacier is in both Wenatchee and Snoqualmie National Forests and flows north from Overcoat Peak and Chimney Rock. Overcoat Glacier descends from 7,200 to 6,000 ft.
Chickamin Glacier is in the U.S. state of Washington. Chickamin Glacier is in Wenatchee National Forest and flows north from Dome Peak and Sinister Peak, descending from nearly 8,600 to 5,600 ft. Chickamin Glacier is separated from Dome Glacier to the south and Dana Glacier to the west by arêtes. The relatively narrow tongue of the 2-mile (3.2 km) wide glacier retreated 800 ft (240 m) between 1998 and 2006.
Sinister Peak is in Mount Baker-Snoqualmie and Wenatchee National Forests in the U.S. state of Washington. It is situated in Glacier Peak Wilderness and the North Cascades. Not quite 1 mi (1.6 km) east of Dome Peak, Sinister Peak is along a high ridge connecting the two peaks. The Chickamin Glacier is on the north slopes of Sinister Peak while the Garden Glacier is just southeast. Though some of the routes to the summit are technical, it can be reached by a moderate scramble.
Diobsud Creek Glacier is in North Cascades National Park in the U.S. state of Washington and is on the east slopes of Bacon Peak. Diobsud Creek Glacier has a shallow gradient, descending to the east from 7,000 to 6,000 ft for a distance of nearly 1 mi (1.6 km). The ridge is an arête which separates Diobsud Creek Glacier from Green Lake Glacier to the north.
Green Lake Glacier is in North Cascades National Park in the U.S. state of Washington and is immediately northeast of Bacon Peak. Green Lake Glacier descends from a ridge extending from the east of Bacon Peak. The glacier forms two tongues descending to the north of the ridge from 6,600 to 5,500 ft. The ridge is an arête which separates Green Lake Glacier from Diobsud Creek Glacier to the south. Meltwater from the glacier spills over Bacon Lake Falls en route to Green Lake.
Richardson Glacier is in Wenatchee National Forest in the U.S. state of Washington and is on the south slopes Luahna Peak and north slopes of Clark Mountain. Richardson Glacier descends from 7,800 to 6,600 ft. Richardson Glacier is connected to Clark Glacier to the east at its upper margins. Richardson Glacier is named after J.B. Richardson, an early settler to the region.
