Ceres Nunataks

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The Ceres Nunataks ( 72°3′S70°25′W / 72.050°S 70.417°W / -72.050; -70.417 ) are a group of three nunataks located immediately east of the base of Shostakovich Peninsula in southern Alexander Island, Antarctica. They were mapped by the Directorate of Overseas Surveys from satellite imagery supplied by the U.S. National Aeronautics and Space Administration in cooperation with the U.S. Geological Survey, and named by the UK Antarctic Place-Names Committee after Ceres, one of the asteroids lying between the orbits of the planets Mars and Jupiter.

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Geology

According to the British Antarctic Survey's (BAS) aeromagnetic 1975 survey of Ceres Nunataks and nearby Astraea Nunatak, this geographical feature is rich in the igneous rocks Diorite and Tonalite as presumed by the rock samples which were observed by BAS during this survey.

Aeromagnetic Survey of Ceres Nunataks and Astraea Nunatak

In December 1975, the British Antarctic Survey (BAS) (originally known as the Falkland Islands Dependencies Survey (FIDS)) embarked on an 8-week long survey observing the proposed theory of Ceres Nunataks and Astraea Nunatak having an aeromagnetic connection between one another. I. A. Crawford and R. W. Girdler embarked on the survey, along with other accompanists and personnel members, flying at a constant barometric altitude of approximately 1130 meters (3707 feet, with an east–west flightline separation of about 7.5 kilometers. Here, they proved that these geographical features were rich in geologic minerals which shared similar characteristics. Data was sampled at one-second intervals, which, at ground speed of approximately 240 kilometers per hour, equates to 15 data points for every kilometer covered. The total distance traveled on the surface was 2200 kilometers (1367 miles). The equipment used included a Geometrics G-803 proton precision magnetometer with both analogue and digital recording, a Bendix DRA-12 Doppler navigation system and Sperry C-12 gyro-magnetic compass, and a Bonzer radio altimeter.

Overall, the 2-month long survey was a successful event and contributed to the history of Alexander Island and the Antarctic Peninsula in itself. Former contributors to this survey include:

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Recluse Nunatak is an isolated rock exposure lying on the Handel Ice Piedmont, midway between Haydn Inlet and the Colbert Mountains in the west-central portion of Alexander Island, Antarctica. The nunatak was first mapped from air photos taken by the Ronne Antarctic Research Expedition (RARE), 1947–48, by Searle of the Falkland Islands Dependencies Survey (FIDS) in 1960. The name given by the United Kingdom Antarctic Place-Names Committee (UK-APC) suggests the isolated position of the nunatak, considering this landform is situated far away from other landforms of Alexander Island.

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