Monteverdi Peninsula

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Monteverdi Peninsula ( 72°30′S72°0′W / 72.500°S 72.000°W / -72.500; -72.000 ) is a large ice-covered peninsula lying between the Bach Ice Shelf and George VI Sound, forming the southernmost extremity of Alexander Island, Antarctica. The southern side of the feature was first seen and charted by Finn Ronne and Carl Eklund of the United States Antarctic Service, 1939–41, who traversed the entire length of George VI Sound. The peninsula was mapped from trimetrogon air photography taken by the Ronne Antarctic Research Expedition in 1947–48, and from survey by the Falkland Islands Dependencies Survey, 1948–50. It was named by the UK Antarctic Place-Names Committee after Italian composer Claudio Monteverdi. [1]

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The north side of the peninsula is surrounded by the Bach Ice Shelf, a large ice shelf that separates it from Beethoven Peninsula. Fauré Inlet is the only inlet that indents the south side of the peninsula, and is filled with flowing from the adjacent George VI Ice Shelf and George VI Sound. Monteverdi Peninsula extends due east–west mainly because there are no peninsulas protruding out of either the north nor the south sides of this peninsula. Monteverdi Peninsula is one of the eight peninsulas of Alexander Island.

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<span class="mw-page-title-main">Alexander Island</span> Island in the Bellingshausen Sea off Antarctica

Alexander Island, which is also known as Alexander I Island, Alexander I Land, Alexander Land, Alexander I Archipelago, and Zemlja Alexandra I, is the largest island of Antarctica. It lies in the Bellingshausen Sea west of Palmer Land, Antarctic Peninsula from which it is separated by Marguerite Bay and George VI Sound. The George VI Ice Shelf entirely fills George VI Sound and connects Alexander Island to Palmer Land. The island partly surrounds Wilkins Sound, which lies to its west. Alexander Island is about 390 kilometres (240 mi) long in a north–south direction, 80 kilometres (50 mi) wide in the north, and 240 kilometres (150 mi) wide in the south. Alexander Island is the second-largest uninhabited island in the world, after Devon Island.

<span class="mw-page-title-main">Beethoven Peninsula</span> Peninsula in Antarctica

The Beethoven Peninsula is a deeply indented, ice-covered peninsula, 60 miles (100 km) long in a northeast–southwest direction and 60 miles (100 km) wide at its broadest part, forming the southwest part of Alexander Island, which lies off the southwestern portion of the Antarctic Peninsula. The south side of the peninsula is supported by the Bach Ice Shelf whilst the north side of the peninsula is supported by the Wilkins Ice Shelf. The Mendelssohn Inlet, the Brahms Inlet and the Verdi Inlet apparently intrude into it. The Bach Ice Shelf, Rossini Point and Berlioz Point are some distance away, on the Ronne Entrance from the Southern Ocean. Beethoven Peninsula is one of the eight peninsulas of Alexander Island.

<span class="mw-page-title-main">George VI Sound</span> Body of water in Palmer Land, Antarctica

George VI Sound or Canal Jorge VI or Canal Presidente Sarmiento or Canal Seaver or King George VI Sound or King George the Sixth Sound is a major bay/fault depression, 300 miles (483 km) long and mainly covered by a permanent ice shelf. It is in the shape of the letter J without any upper bar. It lines the east and south shores of Alexander Island, separating it from the vestigial, quite small, Wordie Ice Shelf and Palmer Land and the north-facing "English Coast". A quite central point of it is 71°S68°W.

Gardner Inlet is a large, ice-filled inlet at the southwest side of Bowman Peninsula, on the east coast of Palmer Land, Antarctica.

<span class="mw-page-title-main">Bach Ice Shelf</span> Ice shelf in Antarctica

The Bach Ice Shelf is an ice shelf which is irregular in shape and 45 miles (72 km) in extent, occupying an embayment in the south part of Alexander Island entered between Berlioz Point and Rossini Point. The ice shelf supports the south face of the Beethoven Peninsula, along with some minor extensive peninsulas and small inlets Bach ice shelf also supports the north side of the Monteverdi Peninsula. A minor embayment in this position first appeared on the charts of the US Antarctic Service, which explored the south part of Alexander Island by air and from the ground in 1940. The ice shelf was delineated by Derek J.H. Searle of the Falkland Islands Dependencies Survey in 1960, from air photos obtained by the Ronne Antarctic Research Expedition in 1947–48. It was named by the UK Antarctic Place-Names Committee after the German composer Johann Sebastian Bach.

Weber Inlet is a broad ice-filled inlet, which indents the south part of the Beethoven Peninsula, lying southwest of Bennett Dome, forming the northwest arm of Bach Ice Shelf in the southwest portion of Alexander Island, Antarctica. The inlet was first mapped from air photos taken by the Ronne Antarctic Research Expedition in 1947–48, by Searle of the Falkland Islands Dependencies Survey in 1960, and named by the UK Antarctic Place-Names Committee after Carl Maria von Weber (1786–1826), a German composer.

<span class="mw-page-title-main">Sulzberger Bay</span> Bay in Antarctica

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Shostakovich Peninsula is an ice-covered peninsula lying north of Stravinsky Inlet and extending into Bach Ice Shelf in southern Alexander Island, Antarctica. The peninsula was first mapped by Directorate of Overseas Surveys from satellite imagery of Antarctica supplied by NASA in cooperation with U.S. Geological Survey. Named by United Kingdom Antarctic Place-Names Committee after Dmitri Shostakovich, Russian composer (1906–1975). Shostakovich Peninsula is one of the eight peninsulas of Alexander Island.

<span class="mw-page-title-main">George VI Ice Shelf</span> Ice shelf in Antarctica

The George VI Ice Shelf is an extensive ice shelf that occupies George VI Sound which separates Alexander Island from Palmer Land in Antarctica. The ice shelf extends from Ronne Entrance, at the southwest end of the sound, to Niznik Island, about 30 nautical miles (56 km) south of the north entrance between Cape Brown and Cape Jeremy. It was named by the UK Antarctic Place-Names Committee in association with George VI Sound.

Gilbert Glacier is a glacier about 20 nautical miles (37 km) long flowing south from Nichols Snowfield into Mozart Ice Piedmont, situated in northern Alexander Island, Antarctica.

<span class="mw-page-title-main">Crane Glacier</span> Glacier in the Aristotle Mountains of the Antarctic Peninsula

Crane Glacier is a narrow glacier which flows 30 miles (50 km) in an east-northeasterly direction along the northwest side of Aristotle Mountains to enter Spillane Fjord south of Devetaki Peak, on the east coast of the Antarctic Peninsula. Sir Hubert Wilkins photographed this feature from the air in 1928 and gave it the name "Crane Channel", after C.K. Crane of Los Angeles, reporting that it appeared to be a channel cutting in an east-west direction across the peninsula. The name was altered to "Crane Inlet" following explorations along the west coast of the peninsula in 1936 by the British Graham Land Expedition, which proved that no through channel from the east coast existed as indicated by Wilkins. Comparison of Wilkins' photograph of this feature with those taken in 1947 by the Falklands Islands Dependencies Survey shows that Wilkins' "Crane Channel" is this glacier, although it lies about 75 miles (120 km) northeast of the position originally reported by Wilkins.

Fletcher Ice Rise, or Fletcher Promontory, is a large ice rise, 100 miles (160 km) long and 40 miles (64 km) wide, at the southwest side of the Ronne Ice Shelf, Antarctica. The feature is completely ice covered and rises between Rutford Ice Stream and Carlson Inlet. The ice rise was observed, photographed and roughly sketched by Lieutenant Ronald F. Carlson, U.S. Navy, in the course of a C-130 aircraft flight of December 14–15, 1961 from McMurdo Sound to this vicinity and returning. It was mapped in detail by the U.S. Geological Survey from Landsat imagery taken 1973–74, and was named by the Advisory Committee on Antarctic Names for Joseph O. Fletcher, director of the Office of Polar Programs, National Science Foundation, 1971–74.

<span class="mw-page-title-main">Boccherini Inlet</span> Ice-filled inlet in Alexander Island

Boccherini Inlet is an ice-filled inlet, 18 nautical miles (33 km) long and 16 nautical miles (30 km) wide, lying between Bennett Dome and Shostakovich Peninsula, which indents the south side of Beethoven Peninsula and forms the northern extremity of the Bach Ice Shelf in Alexander Island. It was first mapped from air photos taken by the Ronne Antarctic Research Expedition, 1947–48, by Derek J.H. Searle of the Falkland Islands Dependencies Survey in 1960, and named by the UK Antarctic Place-Names Committee for Luigi Boccherini, the Italian composer.

Carroll Inlet is an inlet, 40 nautical miles long and 6 nautical miles wide, trending southeast along the coast of Ellsworth Land, Antarctica, between the Rydberg Peninsula and Smyley Island. The head of the inlet is divided into two arms by the presence of Case Island and is bounded to the east by Stange Ice Shelf.

Mount Edred is a prominent ice-covered mountain, 2,195 metres (7,200 ft) high, which stands 10 nautical miles (19 km) inland from George VI Sound, lies about 12 miles (19 km) north of Galileo Cliffs, and marks the southern limit of the Douglas Range on Alexander Island, Antarctica. It was first photographed from the air on November 23, 1935 by Lincoln Ellsworth and mapped from these photos by W.L.G. Joerg. Its east side was roughly surveyed in 1936 by the British Graham Land Expedition and resurveyed in 1949 by the Falkland Islands Dependencies Survey (FIDS). It was named by the FIDS for Edred, a Saxon king of England in the 10th century. The west face of the mountain was mapped from air photos taken by the Ronne Antarctic Research Expedition, 1947–48, by D. Searle of the FIDS in 1960. Mount Edred is the ninth highest peak of Alexander Island, succeeded by Mount Calais and proceeded by Mount Spivey.

Eroica Peninsula is an ice-covered peninsula lying north of Beethoven Peninsula and Mendelssohn Inlet in western Alexander Island, Antarctica. The tip of the peninsula is Kosar Point, marking the western extremity of the Eroica Peninsula. It was mapped from trimetrogon air photography taken by the Ronne Antarctic Research Expedition, 1947–48, and from survey by the Falkland Islands Dependencies Survey, 1948–50. It was named by the UK Antarctic Place-Names Committee after Beethoven's Eroica symphony, in association with Beethoven Peninsula. Eroica Peninsula is one of the eight peninsulas of Alexander Island.

Fauré Inlet is an ice-filled inlet on the south side of the Monteverdi Peninsula and is also the only inlet on the Monteverdi Peninsula in the south portion of Alexander Island, Antarctica. It was discovered and first charted by Finn Ronne and Carl Eklund of the United States Antarctic Service, 1939–1941. It was named by the UK Antarctic Place-Names Committee, 1977, in association with the names of composers grouped in this area, after Gabriel Fauré, the French composer 1845–1924.

Stephenson Nunatak is a prominent, pyramid-shaped rock nunatak, rising to about 640 m, which rises 300 m above the surrounding ice at the northwest side of Kirwan Inlet in the southeast part of Alexander Island, Antarctica. Discovered and roughly surveyed in 1940-41 by Finn Ronne and Carl R. Eklund of the United States Antarctic Service. Resurveyed in 1949 by the Falkland Islands Dependencies Survey and named by the United Kingdom Antarctic Place-Names Committee for Alfred Stephenson, surveyor with the British Graham Land Expedition, who led a sledge party south into George VI Sound to about 72S in 1936. There happens to be another landform on Alexander Island which is named after Alfred Stephenson, that being Mount Stephenson, the highest point of Alexander Island rising to 2,987 m.

<span class="mw-page-title-main">Stange Sound</span> Body of water in Antarctica

Stange Sound is a sound about 60 nautical miles long and 25 nautical miles wide along the coast of Ellsworth Land, Antarctica. An ice shelf occupies the sound, which is bounded on the west by Smyley Island and Case Island, on the south by the mainland, on the east by Spaatz Island and on the north by open water in the Ronne Entrance. Photographed from the air and roughly plotted by the Ronne Antarctic Research Expedition under Finn Ronne. Named for Henry Stange of New York, a contributor to RARE who gave much time to assisting in preparations for the expedition.

Holoviak Glacier is a glacier flowing west into the head of Mendelssohn Inlet, facing towards the Wilkins Ice Shelf on the north side of the Beethoven Peninsula, lying in the southwestern portion of Alexander Island, Antarctica. It was mapped by the United States Geological Survey from U.S. Navy aerial photographs taken 1967–68 and from Landsat imagery taken 1972–73, and was named by the Advisory Committee on Antarctic Names for Judy C. Holoviak, technical editor, 1964–77, of the Antarctic Research Series, published by the American Geophysical Union, and director of publications for the Union from 1978.

References

  1. "Monteverdi Peninsula". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 1 November 2013.

PD-icon.svg This article incorporates public domain material from "Monteverdi Peninsula". Geographic Names Information System . United States Geological Survey.