Kangchenjunga, also spelled Kanchenjunga, Kanchanjanghā and Khangchendzonga, is the third-highest mountain in the world. Its summit lies at 8,586 m (28,169 ft) in a section of the Himalayas, the Kangchenjunga Himal, which is bounded in the west by the Tamur River, in the north by the Lhonak River and Jongsang La, and in the east by the Teesta River. It lies in the border region between Nepal and Sikkim state of India, with three of the five peaks, namely Main, Central and South, directly on the border, and the peaks West and Kangbachen in Nepal's Taplejung District.
A moraine is any accumulation of unconsolidated debris, sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines and medial moraines.
The Karakoram is a mountain range in the Kashmir region spanning the border of Pakistan, China, and India, with the northwestern extremity of the range extending to Afghanistan and Tajikistan. Most of the Karakoram mountain range falls under the jurisdiction of Gilgit-Baltistan, which is controlled by Pakistan. Its highest peak, K2, is located in Gilgit-Baltistan. It begins in the Wakhan Corridor (Afghanistan) in the west, encompasses the majority of Gilgit-Baltistan, and extends into Ladakh and Aksai Chin.
Glaciology is the scientific study of glaciers, or, more generally, ice and natural phenomena that involve ice.
Mount Athabasca is in the Columbia Icefield of Jasper National Park in Canada. The mountain was named in 1898 by J. Norman Collie, who made the first ascent on August 18 of that year. Athabasca is the Cree language name for "where there are reeds", which originally referred to Lake Athabasca. Mount Athabasca is unusual, in that water flows to the Pacific Ocean from the western slope, the Arctic Ocean from the northeastern slope, and to Hudson Bay from the southeastern slope.
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 Darwin Glacier is a large glacier in Antarctica. It flows from the polar plateau eastward between the Darwin Mountains and the Cook Mountains to the Ross Ice Shelf. The Darwin and its major tributary the Hatherton are often treated as one system, the Darwin–Hatherton.
The Royal Society Range is a majestic range of mountains in Victoria Land, Antarctica, rising to 4,025 metres (13,205 ft) along the west shore of McMurdo Sound between the Koettlitz, Skelton and Ferrar Glaciers. They are south of the Kukri Hills, southeast of the Quartermain Mountains, and northeast of the Worcester Range.
Kaliakra Glacier is a glacier in northeastern Livingston Island, Antarctica extending 3.8 nautical miles in east-west direction and 4.3 nautical miles in north-south direction, and situated southeast of Saedinenie Snowfield, southwest of Panega Glacier, north of Struma Glacier and upper Huron Glacier, and northeast of Perunika Glacier. It is bounded by Melnik Ridge and Bowles Ridge to the south, by Hemus Peak, Gurev Gap, Gleaner Heights, Elhovo Gap, Leslie Hill, Leslie Gap and Radnevo Peak to the west, and Miziya Peak and Samuel Peak to the north. The glacier drains eastwards into Moon Bay south of Perperek Knoll and north of Sindel Point.
Lennox-King Glacier is a large valley glacier, about 40 nautical miles (70 km) long that flows east into the Ross Ice Shelf.
Drygalski Glacier is a broad glacier, 18 nautical miles long and 15 miles (24 km) wide at its head, which flows from Herbert Plateau southeast between Ruth Ridge and Kyustendil Ridge, and enters Solari Bay immediately north of Sentinel Nunatak on Nordenskjöld Coast, the east coast of Graham Land, Antarctica. It was discovered in 1902 by the Swedish Antarctic Expedition, under Otto Nordenskiöld, and named "Drygalski Bay" after Professor Erich von Drygalski. The feature was determined to be a glacier by the Falkland Islands Dependencies Survey in 1947.
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.
Kirkby Glacier is a glacier, 20 nautical miles in length, that drains the central Anare Mountains of Antarctica and flows northwest to the sea just north of Arthurson Bluff, northern Victoria Land.
William Glacier is a glacier flowing south from the interior highlands of Anvers Island to the head of Börgen Bay on the southeast coast of the island, in the Palmer Archipelago. Discovered by the Belgian Antarctic Expedition, 1897–99, under Gerlache, and charted by them simply as a "grand glacier." The name William Glacier first appears on a chart based upon a 1927 survey by DI personnel on the Discovery. Gateway Ridge separates William Glacier from Hooper Glacier.
Ambergris Glacier is a glacier flowing south-southeast from Mount Sara Teodora between Chintulov Ridge and Valkosel Ridge to join Flask Glacier just west of Fluke Ridge in Aristotle Mountains on the east coast of Graham Land, Antarctica. One of several names in the area that reflect a whaling theme, it was named in 1987 by the United Kingdom Antarctic Place-Names Committee from the substance secreted by the sperm whale and used in perfumery.
Arena Glacier is a glacier on Trinity Peninsula, the northernmost region of the Antarctic Peninsula. The glacier is 3 miles (5 km) long and flows northeast from Mount Taylor into Hope Bay, 2 miles (3 km) southwest of Sheppard Point. The Falkland Islands Dependencies Survey mapped the area in 1948 and again in 1955. Due to its flat ice floor on the upper half, they named it Arena Glacie, which was surrounded by the steep slopes of the Twin Peaks, Mount Taylor and Blade Ridge, resembling an arena.
Pequod Glacier is a glacier over 15 nautical miles (28 km) long, draining eastwards between Parlichev Ridge to the north, and Taridin Ridge and Krupen Ridge to the south, and flowing into Exasperation Inlet on the east coast of Graham Land. It lies parallel and just south of Melville Glacier. The lower part of the glacier was surveyed by Falkland Islands Dependencies Survey (FIDS) in 1947 and the upper reaches were surveyed in 1955. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) after the whaling ship Pequod in Herman Melville's Moby-Dick.
Melville Glacier is a glacier, 12 nautical miles (22 km) long, between Mapple Glacier and Pequod Glacier on the east coast of Graham Land, Antarctica. It flows eastwards between Stevrek Ridge and Parlichev Ridge in the Aristotle Mountains, to enter Domlyan Bay in the Weddell Sea. It was surveyed by the Falkland Islands Dependencies Survey in 1947 and 1955, and was named by the UK Antarctic Place-Names Committee after Herman Melville, the author of the 1851 novel Moby-Dick. Several other features in the area, such as Mount Ahab, are named after characters in the story.
Cervellati Glacier is the 5 nmi long glacier situated southeast of Patton Glacier and northwest of Ramorino Glacier on the east slope of Sentinel Range in the Ellsworth Mountains, Antarctica. It flows northeastwards between Tyree Ridge and Epperly Ridge, and enters Crosswell Glacier southeast of Mount Bearskin. The feature was named by US-ACAN in 2006 after Roberto Cervellati, Italian representative to the SCAR Expert Group on Geographic Information, 1992–2006, and director of the SCAR Composite Gazetteer of Antarctica in the same period.
Ramorino Glacier is the 4.5 nautical miles long glacier situated northwest of upper Crosswell Glacier and southeast of Cervellati Glacier on the east slope of Sentinel Range in the Ellsworth Mountains, Antarctica. It flows northeastwards between Epperly Ridge and Shinn Ridge, and enters Crosswell Glacier northwest of Mount Segers. The feature was named by US-ACAN in 2006 after Maria Chiara Ramorino, manager of the Italian team that compiled and promulgated the SCAR Composite Gazetteer of Antarctica, 1998–2006.
