The Hauberg Mountains ( 75°52′S 069°15′W / 75.867°S 69.250°W / -75.867; -69.250 ( Hauberg Mountains ) ) are a group of mountains of about 35 nautical miles (65 km; 40 mi) extent, located 12 nautical miles (22 km; 14 mi) north of Cape Zumberge and 30 nautical miles (56 km; 35 mi) south of the Sweeney Mountains in eastern Ellsworth Land , Antarctica.
30-662: Download coordinates as: The Hauberg Mountains are in the southeast of Ellsworth Land just north of the Orville Coast . They are southeast of the Behrendt Mountains and south of the Sweeney Mountains . Eastern features, from north to south, include Shelton Nunataks, Janke Nunatak, Bean Peaks, Carlson Peak, Novocin Peak and Cape Zumberge. Western features include Mount Leek and Mount Dewe, separated by
60-673: A USGS field party. Named by US-ACAN in 1985 after Commander Dwight D. Fisher, United States Navy, command pilot on the first landing by LC-130 Hercules aircraft on English Coast in December 1984; Commanding Officer, United States Navy Antarctic Development Squadron Six (VXE-6), from May 1984 to May 1985; Commanding Officer, NSFA, 1987-89; Naval Officer on detail to NSF, 1989-92; Deputy Manager, Polar Operations Section, Office of Polar Programs, NSF, from 1992. 75°49′S 68°31′W / 75.817°S 68.517°W / -75.817; -68.517 . A mountain standing west of Spear Glacier in
90-623: A USGS geological party to this area, 1977-78; Commanding Officer, Antarctic Development Squadron Six (VXE-6), May 1978 to May 1979. 76°14′S 69°40′W / 76.233°S 69.667°W / -76.233; -69.667 . A steep rock cape on the west side of the Ronne Ice Shelf , marking the southwest end of the Orville Coast. The name "Zumberge Nunatak" was given by the US-IGY party from Ellsworth Station , 1957-58, to
120-581: A USGS geological party, led by P.D. Rowley, and named after Lieutenant Commander John R. Hutchins, United States Navy, command pilot of an LC-130 aircraft in support of the party. 75°29′S 69°22′W / 75.483°S 69.367°W / -75.483; -69.367 . Isolated nunataks about midway between the Sweeney Mountains and Hauberg Mountains. Mapped by USGS from ground surveys and United States Navy air photos, 1961-67. Named by US-ACAN for Paul F. Witte, construction mechanic with
150-542: A depth of 1,233 m (872 of which were ice), 260 km from open water. In October 1998, the iceberg A-38 broke off the Filchner–Ronne ice shelf. It had an extent of roughly 150 by 50 km and was thus larger than Delaware . It later broke up again into three parts. A similar-sized calving in May 2000 created an iceberg 167 by 32 km in extent, dubbed A-43 – the disintegration of this is thought to have been responsible for
180-534: A rock feature reported to lie 30 nautical miles (56 km; 35 mi) north of the westernmost traverse station occupied by the party. The cape described, though somewhat farther north, is apparently the only rock feature lying in that direction. Named for James H. Zumberge, American glaciologist who has made studies of the Ross Ice Shelf. 75°55′S 68°15′W / 75.917°S 68.250°W / -75.917; -68.250 . A glacier between
210-565: Is a stub . You can help Misplaced Pages by expanding it . Ronne Ice Shelf 77°51′33″S 61°17′57″W / 77.85917°S 61.29917°W / -77.85917; -61.29917 The Filchner–Ronne Ice Shelf or Ronne–Filchner Ice Shelf is an Antarctic ice shelf bordering the Weddell Sea . The seaward side of the Filchner–Ronne ice shelf is divided into Eastern (Filchner) 79°00′S 40°00′W / 79.000°S 40.000°W / -79.000; -40.000 and
240-566: Is therefore named for Edith Ronne , the wife of Finn Ronne and RARE Expedition member. The Filchner ice shelf is the eastern part of the Filchner–Ronne ice shelf. It is bounded on the west by Berkner Island and on the east by Coats Land . The east part of this shelf was discovered in January–February 1912 by the German Antarctic Expedition under Wilhelm Filchner . Filchner named the feature for Kaiser Wilhelm , but
270-668: The Ronne Antarctic Research Expedition (RARE) in 1947–48, discovered and photographed a strip along the entire northern portion of this ice shelf in two aircraft flights in November and December 1947. He named it the "Lassiter Shelf Ice" and gave the name "Edith Ronne Land" to the land presumed to lie south of it. In 1957–58, the US- IGY party at Ellsworth Station , under now Captain Ronne, determined that
300-712: The United States Geological Survey (USGS) from surveys and United States Navy air photos, 1961-67. Named by the United States Advisory Committee on Antarctic Names (US-ACAN) for John W. Janke, radioman with the Eights Station winter party in 1964. 76°00′S 69°00′W / 76.000°S 69.000°W / -76.000; -69.000 . A glacier over 20 nautical miles (37 km; 23 mi) long, flowing east and southeast from Janke Nunatak to
330-533: The United States Geological Survey . Ellsworth Land Ellsworth Land is a portion of the Antarctic continent bounded on the west by Marie Byrd Land , on the north by Bellingshausen Sea , on the northeast by the base of Antarctic Peninsula , and on the east by the western margin of the Filchner–Ronne Ice Shelf . It extends between 103°24'W and 79°45'W. The area west of 90°W is unclaimed,
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#1732801401210360-525: The Bean Peaks, located near the southeast end of this group. First observed from aircraft by the RARE, 1947-48. Mapped by USGS from surveys and United States Navy air photos, 1961-67. Named by US-ACAN for Norbert W. Novocin, meteorologist at Byrd Station, summer 1965-66. 75°58′S 68°39′W / 75.967°S 68.650°W / -75.967; -68.650 . Mountain in the southeast part of
390-573: The Eights Station winter party in 1964. 75°43′S 70°35′W / 75.717°S 70.583°W / -75.717; -70.583 . Two isolated nunataks located 10 nautical miles (19 km; 12 mi) southeast of Thomas Mountains. Mapped by USGS from surveys and United States Navy air photos, 1961-67. Named by US-ACAN for Willard S. Shelton, electrician at Eights Station in 1964. [REDACTED] This article incorporates public domain material from websites or documents of
420-715: The Emperor requested it be named for its discoverer. The shelf is nourished primarily by the Slessor Glacier , the Recovery Glacier , and the Support Force Glacier , all located east of Berkner Island. In 2021, sponges and other unidentified suspension feeders were reported to have been found growing on a boulder under the western margin of the Filchner ice shelf, close to Berkner Island, at
450-896: The Hauberg Mountains and Peterson Hills. Mapped by USGS from surveys and United States Navy air photos, 1961-67. Named by US-ACAN for Milton B. Spear, construction electrician at Eights Station in 1965. 75°50′S 67°55′W / 75.833°S 67.917°W / -75.833; -67.917 . A group of hills just east of Spear Glacier, between the Hauberg Mountains and Wilkins Mountains. Mapped by USGS from surveys and United States Navy air photos, 1961-67. Named by US-ACAN for D.G. Peterson, electronics technician at South Pole Station in 1963. 75°32′S 66°30′W / 75.533°S 66.500°W / -75.533; -66.500 . A group of low mountains of about 20 nautical miles (37 km; 23 mi) extent, located 25 nautical miles (46 km; 29 mi) southeast of
480-541: The Hauberg Mountains. Mapped by USGS from ground surveys and United States Navy air photos, 1961-67. Named by US-ACAN for Michael B. Dewe, glaciologist at Byrd Station, summer 1965-66. 75°52′S 68°23′W / 75.867°S 68.383°W / -75.867; -68.383 . A peak rising to about 1,100 metres (3,600 ft) high, 5 nautical miles (9.3 km; 5.8 mi) southeast of Mount Leek. Mapped by USGS from surveys and United States Navy aerial photographs, 1961-67. Climbed in December 1977 by members of
510-527: The November 2006 sighting of several large icebergs from the coast of the South Island of New Zealand , the first time since 1931 that any icebergs had been observed from the New Zealand mainland. A large group of small icebergs (the largest some 1000 metres in length), were seen off the south-east coast of the island, with one of them drifting close enough to shore to be visible from the hills above
540-708: The Orville Coast, west of Spear Glacier. The feature was mapped by USGS from surveys and United States Navy aerial photographs, 1961-67, and was visited by a USGS geological party, 1977-78, led by Peter D. Rowley. Named by US-ACAN after Commander (later Captain) David A. Srite, United States Navy, chief navigator of an LC-130 aircraft in support of the geological party in this area, 1977-78; Commanding Officer, Antarctic Development Squadron Six, 1979 to 1980; Commanding Officer, Naval Support Force, Antarctica, 1985 to 1987. 75°58′S 70°00′W / 75.967°S 70.000°W / -75.967; -70.000 . A group of peaks including Carlson Peak and Novocin Peak, which form
570-685: The Spear Glacier from the Peterson Hills and Wilkins Mountains. The Witte Nunataks are to the north. The Hauberg Mountains were discovered by the Ronne Antarctic Research Expedition (RARE), 1947–48, led by Finn Ronne , and named by him for John Hauberg, of Rock Island, Illinois , a contributor to the expedition. 75°53′S 70°27′W / 75.883°S 70.450°W / -75.883; -70.450 . An isolated nunatak, 4 nautical miles (7.4 km; 4.6 mi) northeast of Carlson Peak in western Hauberg Mountains. Mapped by
600-1054: The Sweeney Mountains. Discovered by the RARE, 1947-48, under Ronne, who named these mountains for Sir Hubert Wilkins. 75°45′S 65°30′W / 75.750°S 65.500°W / -75.750; -65.500 . A glacier on the east side of the Wilkins Mountains, draining south to enter the Ronne Ice Shelf just west of Dodson Peninsula . Mapped by the USGS from surveys and United States Navy air photos, 1961-67. Named by US-ACAN for J.D. Matthews, engineman at South Pole Station in 1963. 75°39′S 68°10′W / 75.650°S 68.167°W / -75.650; -68.167 . A group of nunataks rising to about 1,200 metres (3,900 ft) high, 12 nautical miles (22 km; 14 mi) north-northeast of Mount Leek. Mapped by USGS from surveys and United States Navy aerial photographs, 1961-67. Visited in December 1977 by
630-701: The area between 84°W and 90°W is claimed by Chile only, and the remainder by Chile and the United Kingdom as a part of the British Antarctic Territory . Eights Coast stretches between 103°24'W and 89°35'W, and Bryan Coast between 89°35'W and 79°45'W. It is largely a high ice plateau, but includes the Ellsworth Mountains and a number of scattered mountain groups: Hudson , Jones , Behrendt , Hauberg , Merrick , Sweeney and Scaife Mountains . This land lies near
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#1732801401210660-570: The center of the area traversed by American explorer Lincoln Ellsworth on an airplane flight during November–December 1935. It was named for him by the Advisory Committee on Antarctic Names in 1962 to commemorate that historic transcontinental flight from Dundee Island to the Ross Ice Shelf . Information regarding the biodiversity of Ellsworth Land is comparatively limited due to the fewer research surveys and visitations in
690-714: The city of Dunedin . If these were indeed the remnants of this calving, then over the course of five and a half years they had travelled slowly north and also east around over half the globe, a journey of some 13,500 km. From January 12 and January 13, 2010, an area of sea ice larger than the state of Rhode Island , or one-seventh the size of Wales , broke away from the Ronne–Filchner Ice Shelf and shattered into many smaller pieces. The Moderate-Resolution Imaging Spectroradiometer (MODIS) on NASA's Aqua and Terra satellites captured this event in this series of photo-like images. In May 2021, Iceberg A-76 broke off
720-434: The ice shelf was larger than previously charted, that it extends southward to preempt most of " Edith Ronne Land ". Inasmuch as Capt. James Lassiter's name has been assigned to a coast of Palmer Land , the Advisory Committee on Antarctic Names (US-ACAN) approved the name Ronne Ice Shelf for this large ice shelf, on the basis of first sighting and exploration of the ice shelf by Ronne and parties under his leadership. The shelf
750-473: The larger Western (Ronne) 78°30′S 61°00′W / 78.500°S 61.000°W / -78.500; -61.000 sections by Berkner Island . The whole ice shelf covers some 430,000 km , making it the second largest ice shelf in Antarctica (and on Earth), after the Ross Ice Shelf . It grows perpetually due to a flow of inland ice sheets. From time to time, when the shearing stresses exceed
780-624: The northeast part of the Hauberg Mountains. First observed from the air by the RARE, 1947-48. Mapped by USGS from surveys and United States Navy air photos, 1961-67. Named by US-ACAN for Gouke M. Leek, glaciologist at Byrd Station, summer 1965-66. 75°47′S 68°24′W / 75.783°S 68.400°W / -75.783; -68.400 . A peak rising to about 1,100 metres (3,600 ft) high, located 3 nautical miles (5.6 km; 3.5 mi) northeast of Mount Leek. Named by US-ACAN in 1985 after Commander William A. Morgan, United States Navy, command pilot of an LC-130 aircraft in support of
810-424: The northwest corner of the shelf. At 4320 km , it is larger than Majorca , several times larger than Iceberg A-74 which calved in the same year, or approximately 14% the size of Belgium . The ice of the Filchner–Ronne ice shelf can be as thick as 600 m; the water below is about 1400 m deep at the deepest point. The international Filchner–Ronne Ice Shelf Programme (FRISP) was initiated in 1973 to study
840-418: The region. Forty species of lichen and five of moss have been identified, with Usnea sphacelata being amongst the most prominent species in the region. Colonies of Adélie penguins have been observed on multiple offshore islands in the adjacent Amundsen Sea . 75°30′S 80°00′W / 75.500°S 80.000°W / -75.500; -80.000 This Ellsworth Land location article
870-749: The southwest part of the Hauberg Mountains. First sighted from the air by the RARE, 1947-48. Mapped by USGS from ground surveys and United States Navy air photos, 1961-67. Named by US-ACAN for Lawrence D. Bean, electrician with the South Pole Station winter party in 1967. 75°57′S 70°33′W / 75.950°S 70.550°W / -75.950; -70.550 . One of the Bean Peaks. Mapped by USGS from ground surveys and United States Navy air photos, 1961-67. Named by US-ACAN for Paul R. Carlson, meteorologist at Byrd Station, summer 1965-66. 76°01′S 69°33′W / 76.017°S 69.550°W / -76.017; -69.550 . One of
900-510: The strength of the ice, cracks form and large parts of the ice sheet separate from the ice shelf and float off and disperse as icebergs . This is known as calving . The Ronne ice shelf is the larger and western part of the Filchner–Ronne ice shelf. It is bounded on the west by the base of the Antarctic Peninsula ( Graham Land with Zumberge Coast and Orville Coast ) and Ellsworth Land . Commander Finn Ronne , USNR, leader of
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