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Du Toit Nunataks
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Du Toit Nunataks
The Du Toit Nunataks (80°43′S 25°50′W / 80.717°S 25.833°W) are a group of nunataks between Cornwall Glacier and Glen Glacier, marking the western end of the Read Mountains in the Shackleton Range of Antarctica.
The Du Toit Nunataks were photographed from the air by the United States Navy, 1967, and surveyed by the British Antarctic Survey, 1968–71. In association with the names of geologists grouped in this area, they were named by the UK Antarctic Place-Names Committee after Alexander Logie du Toit, a South African geologist.
The Du Toit Nunataks lie to the south of the Shotton Snowfield to the west end of the Read Mountains. They lie between the Cornwall Glacier and the Glen Glacier, both of which flow south to join the Recovery Glacier, which flows westward past the south of the Du Toit Nunataks.
The Du Toit Nunataks are in the Read Group of the southern belt of the Shackleton Mountains. They are mainly composed of partly migmatised quartzitic, basic, calcareous and pelitic rocks. In places they are interlayered with gneissic granites, and intruded by granites and basic rocks. Dating of the metagranites gives ages of around 1,760 and 1,600 million years. Rb–Sr and K-Ar mineral cooling ages are 1650–1550 million years.
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Named geographical features on the 1983 United States Geological Survey map include:
80°44′S 25°36′W / 80.733°S 25.600°W. A small debris-covered area with elevation about 1,350 metres (4,430 ft) on the east margin of Du Toit Nunataks, Read Mountains, in the Shackleton Range. Photographed from the air by the U.S. Navy, 1967, and surveyed by BAS, 1968–71. In association with the names of geologists grouped in this area, named by the UK-APC in 1971 after Frederick Henry Hatch (1864–1932), British consulting geologist; author of standard textbooks on igneous and sedimentary petrology.
80°44′S 25°57′W / 80.733°S 25.950°W An east-facing escarpment rising to about 1,300 metres (4,300 ft) and trending northeast–southwest for 3.5 miles (5.6 km) in the Du Toil Nunataks, Read Mountains, Shackleton Range. Photographed from the air by the U.S. Navy, 1967, and surveyed by BAS, 1968-71. In association with the names of geologists grouped in this area, named by the UK-APC in 1971 after Professor Arie Poldervaart (1919–64), Dutch petrologist known for his research on basaltic rocks.
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Du Toit Nunataks
The Du Toit Nunataks (80°43′S 25°50′W / 80.717°S 25.833°W) are a group of nunataks between Cornwall Glacier and Glen Glacier, marking the western end of the Read Mountains in the Shackleton Range of Antarctica.
The Du Toit Nunataks were photographed from the air by the United States Navy, 1967, and surveyed by the British Antarctic Survey, 1968–71. In association with the names of geologists grouped in this area, they were named by the UK Antarctic Place-Names Committee after Alexander Logie du Toit, a South African geologist.
The Du Toit Nunataks lie to the south of the Shotton Snowfield to the west end of the Read Mountains. They lie between the Cornwall Glacier and the Glen Glacier, both of which flow south to join the Recovery Glacier, which flows westward past the south of the Du Toit Nunataks.
The Du Toit Nunataks are in the Read Group of the southern belt of the Shackleton Mountains. They are mainly composed of partly migmatised quartzitic, basic, calcareous and pelitic rocks. In places they are interlayered with gneissic granites, and intruded by granites and basic rocks. Dating of the metagranites gives ages of around 1,760 and 1,600 million years. Rb–Sr and K-Ar mineral cooling ages are 1650–1550 million years.
Download coordinates as:
Named geographical features on the 1983 United States Geological Survey map include:
80°44′S 25°36′W / 80.733°S 25.600°W. A small debris-covered area with elevation about 1,350 metres (4,430 ft) on the east margin of Du Toit Nunataks, Read Mountains, in the Shackleton Range. Photographed from the air by the U.S. Navy, 1967, and surveyed by BAS, 1968–71. In association with the names of geologists grouped in this area, named by the UK-APC in 1971 after Frederick Henry Hatch (1864–1932), British consulting geologist; author of standard textbooks on igneous and sedimentary petrology.
80°44′S 25°57′W / 80.733°S 25.950°W An east-facing escarpment rising to about 1,300 metres (4,300 ft) and trending northeast–southwest for 3.5 miles (5.6 km) in the Du Toil Nunataks, Read Mountains, Shackleton Range. Photographed from the air by the U.S. Navy, 1967, and surveyed by BAS, 1968-71. In association with the names of geologists grouped in this area, named by the UK-APC in 1971 after Professor Arie Poldervaart (1919–64), Dutch petrologist known for his research on basaltic rocks.
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