The Kappen Cliffs ( 76°56′S162°22′E / 76.933°S 162.367°E ) are steep rock cliffs that form the south edge of Kar Plateau on Scott Coast, Victoria Land, Antarctica. The cliffs are 5.5 nautical miles (10 km) long and rise to 600 metres (2,000 ft). They were named by the New Zealand Geographic Board (1999) after Professor Ludger Kappen of Kiel University, Germany, who conducted extensive lichen ecophysiology in the Cape Geology area. [1]
James Ross Island is a large island off the southeast side and near the northeastern extremity of the Antarctic Peninsula, from which it is separated by Prince Gustav Channel. Rising to 1,630 metres (5,350 ft), it is irregularly shaped and extends 40 nautical miles in a north–south direction.
Koettlitz Glacier is a large Antarctic glacier lying west of Mount Morning and Mount Discovery in the Royal Society Range, flowing from the vicinity of Mount Cocks northeastward between Brown Peninsula and the mainland into the ice shelf of McMurdo Sound.
Mount Bird is a 1,765 metres (5,791 ft) high shield volcano standing about 7 nautical miles south of Cape Bird, the northern extremity of Ross Island. It was mapped by the British National Antarctic Expedition, 1901–04, under Robert Falcon Scott, and apparently named by them after Cape Bird.
Mount Lister is a massive mountain, 4,025 metres (13,205 ft) high, forming the highest point in the Royal Society Range of Victoria Land, Antarctica. It was discovered by the British National Antarctic Expedition (1901–1904) which named it for Lord Joseph Lister, President of the Royal Society, 1895–1900.
The Newall Glacier is a glacier in the east part of the Asgard Range of Victoria Land, It flows east between Mount Newall and Mount Weyant into the Wilson Piedmont Glacier. The Newall Glacier was mapped by the N.Z. Northern Survey Party of the CTAE, 1956-58, who named it after nearby Mount Newall.
The Worcester Range is a high coastal range, about 30 nautical miles long, in Antarctica. It stands between Skelton Glacier and Mulock Glacier on the western side of the Ross Ice Shelf. It is southwest of the Royal Society Range and north of the Conway Range of the Cook Mountains.
The Olympus Range is a primarily ice-free mountain range of Victoria Land, Antarctica, with peaks over 2,000 metres (6,600 ft) high, between Victoria Valley and McKelvey Valley on the north and Wright Valley on the south. It is south of the Clare Range and north of the Asgard Range.
The Nash Range is a mainly ice-covered coastal range in the Churchill Mountains of Antarctica.
Flint Ridge is a north-south trending ridge with a summit elevation of 995 metres (3,264 ft) in the Asgard Range of Victoria Land, Antarctica. Flint Ridge was named by US-ACAN for Lawrence A. Flint, manager of the USARP Berg Field Center at McMurdo Station in 1972. A standard USGS survey tablet stamped "Flint ET 1971-72" was fixed in a rock slab atop this ridge by the USGS Electronic Traverse, 1971-72.
Foreman Glacier is a glacier flowing south-southeast from the Havre Mountains in the northern portion of Alexander Island, Antarctica. It drains the southwest slopes of Dimitrova Peak and the west slopes of Breze Peak and flows into Palestrina Glacier north of Balan Ridge in Sofia University Mountains. The glacier was surveyed by the British Antarctic Survey (BAS), 1975–76, and was named by the UK Antarctic Place-Names Committee in 1980 after David Alexander Foreman, a BAS aircraft mechanic at Adelaide Station, 1973–76.
Gobamme Rock is an exposed rock standing on the coast between Kozō Rock and Byōbu Rock in Queen Maud Land, Antarctica. It was mapped from surveys and air photos by the Japanese Antarctic Research Expedition, 1957–62, and named Gobanme-iwa.
Granite Harbour is a bay in the coast of Victoria Land, Antarctica, about 14 nautical miles long, entered between Cape Archer and Cape Roberts. It was discovered and named by the British National Antarctic Expedition (BrNAE) of 1901–04 in the Discovery in January 1902, while searching for safe winter quarters for the ship. The name derives from the great granite boulders found on its shores.
The Lokehellene Cliffs are steep rock cliffs which form the west side of Nupsskarvet Mountain, in the Kurze Mountains of Queen Maud Land, Antarctica. They were mapped from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named Lokehellene after Loki, a god of Norse mythology.
Mount McLennan is a prominent mountain rising over 1,600 metres (5,250 ft) at the north side of Taylor Valley, surmounting the area at the heads of Canada Glacier, Commonwealth Glacier and Loftus Glacier, in Victoria Land, Antarctica. It was named by C.S. Wright of the British Antarctic Expedition (1910–13) for Professor McLennan, a physicist at Toronto University, Canada.
Harvey Summit is a peak 2,644 metres (8,675 ft) high at the head of McDermott Glacier in the Royal Society Range of Victoria Land, Antarctica. It was named by the United States Advisory Committee on Antarctic Names (US-ACAN) after John W. Harvey of the National Solar Observatory who, along with Thomas L. Duvall, Jr. and Martin A. Pomerantz, conducted research in helioseismology at the South Pole for some years from 1980 onwards.
The Kirkwood Range is a massive coastal mountain range in Antarctica, extending north–south between Fry Glacier and Mawson Glacier. A broad low-level platform on the seaward side of the range is occupied by the Oates Piedmont Glacier. It is south of the Prince Albert Mountains and northeast of the Convoy Range.
Mackay Glacier is a large glacier in Victoria Land, descending eastward from the Antarctic Plateau, between the Convoy Range and Clare Range, into the southern part of Granite Harbour. It was discovered by the South magnetic pole party of the British Antarctic Expedition, 1907–09, and named for Alistair Mackay, a member of the party. The glacier's tongue is called Mackay Glacier Tongue. First mapped by the British Antarctic Expedition, 1910–13 and named for Alistair F. Mackay, a member of the party. Its mouth is south of the Evans Piedmont Glacier and the Mawson Glacier. It is north of the Wilson Piedmont Glacier and the Ferrar Glacier.
The Horowitz Ridge is a rock ridge between David Valley and King Valley in the Asgard Range of Victoria Land, Antarctica.
The Larsen Cliffs are steep rock and ice cliffs which form a part of the east face of Jøkulkyrkja Mountain, in the Mühlig-Hofmann Mountains of Queen Maud Land, Antarctica. They were plotted from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named for Per Larsen, a steward with the expedition (1956–57).
The Colbert Hills are a line of hills and bluffs, including Coalsack Bluff, lying east of Lewis Cliffs, between Law Glacier and Walcott Névé in Antarctica. The hills trend southwest for 16 nautical miles from Mount Sirius.
This article incorporates public domain material from "Kappen Cliffs". Geographic Names Information System . United States Geological Survey.