Ceres Nunataks
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The Ceres Nunataks () are a group of three nunataks located immediately east of the base of
Shostakovich Peninsula 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 im ...
in southern
Alexander Island 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, Antarc ...
,
Antarctica Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean, it contains the geographic South Pole. Antarctica is the fifth-largest cont ...
. They were mapped by the
Directorate of Overseas Surveys The Ordnance Survey International or Ordnance Survey Overseas Directorate its predecessors built an archive of air photography, map and survey records for the United Kingdom from 1946 to 1999. The Ordnance Survey International Collection (formerly ...
from satellite imagery supplied by the U.S. National Aeronautics and Space Administration in cooperation with the
U.S. Geological Survey The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and ...
, and named by the
UK Antarctic Place-Names Committee The UK Antarctic Place-Names Committee (or UK-APC) is a United Kingdom government committee, part of the Foreign and Commonwealth Office, responsible for recommending names of geographical locations within the British Antarctic Territory (BAT) and ...
after
Ceres Ceres most commonly refers to: * Ceres (dwarf planet), the largest asteroid * Ceres (mythology), the Roman goddess of agriculture Ceres may also refer to: Places Brazil * Ceres, Goiás, Brazil * Ceres Microregion, in north-central Goiás ...
, one of the asteroids lying between the orbits of the planets
Mars Mars is the fourth planet from the Sun and the second-smallest planet in the Solar System, only being larger than Mercury. In the English language, Mars is named for the Roman god of war. Mars is a terrestrial planet with a thin at ...
and
Jupiter Jupiter is the fifth planet from the Sun and the largest in the Solar System. It is a gas giant with a mass more than two and a half times that of all the other planets in the Solar System combined, but slightly less than one-thousandth t ...
.


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 Diorite ( ) is an intrusive igneous rock formed by the slow cooling underground of magma (molten rock) that has a moderate content of silica and a relatively low content of alkali metals. It is intermediate in composition between low-sili ...
and
Tonalite Tonalite is an igneous, plutonic ( intrusive) rock, of felsic composition, with phaneritic (coarse-grained) texture. Feldspar is present as plagioclase (typically oligoclase or andesine) with alkali feldspar making up less than 10% of the total ...
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: * Barker, P. F. - Studied the Cenozoic subduction history of the Antarctic Peninsula region. * Bell, C. M. - Observed the geology of the southern portion of Alexander Island. * Bhattacharyya, B. K. - Examined the magnetic anomalies due to prism-shaped bodies with arbitrary polarization. * Burn R. W. - Studied multiple fields of Alexander Island, such as the early Tertiary calc-alkaline volcanism on the island and researching the geology of the nearby LeMay Mountain Range due 40-50 kilometers north of Staccato Peaks. * Care, B. W. - Like Burn, Care studied the vast majority of fields involving Alexander Island, such as archiving geographic reports on the
Havre Mountains The Havre Mountains () are a large group of mountains forming the northwestern extremity of Alexander Island, Antarctica, extending in an east–west direction between Cape Vostok and the Russian Gap. They were first seen in 1821 by a Russian ex ...
,
Lassus Mountains The Lassus Mountains () are a large group of mountains, long and wide, rising to and extending south from Palestrina Glacier in the northwest part of Alexander Island, Antarctica. They overlook Lazarev Bay and a few minor islands within the ba ...
and other miscellaneous peaks within the vicinity of northern Alexander Island. * Coles R. W. - Conducted two magnetic interpretation methods using rectangular prisms. * Collinson, D. W. - Created an anisotropic susceptibility meter, along with Molyneux, L. and Stone, D. B. * Crabtree, R. D. - Constructed a British Antarctic Territory ice thickness map * Crawford, I. A. - Proposed an analysis of aeromagnetic data over the Staccato Peaks region of Alexander Island, Antarctica, along with Girdler, R. W. * Edwards, C. W. - Collected early Mesozoic marine fossils from the central portion of Alexander Island. * Fabiano, E. B. - Observed grid values of total magnetic intensity, along with the help of former geophysicist Peddie, N. W. * Pankhurst, R. J. - Studied the geochronology of
Graham Land Graham Land is the portion of the Antarctic Peninsula that lies north of a line joining Cape Jeremy and Cape Agassiz. This description of Graham Land is consistent with the 1964 agreement between the British Antarctic Place-names Committee an ...
, Antarctica. * Peddie, N. W. - Former geophysicist of BAS. * Renner R. G. B. - Former member of BAS and accepted the aeromagnetic survey to commence, chief of the 1975 survey. * Smellie, J. L. - A complete arc-trench system recognized in Gondwana sequences of the Antarctic Peninsula region. * Streckeisen, A. - Gave to each plutonic body its proper name. * Suarez, M. - Credited for having charted a Plate-tectonic model for the southern portion of the Antarctic Peninsula (Palmer Land) and its relation to the southern Andes Mountain Range.


References

* {{usgs-gazetteer, id=2579

Nunataks of Alexander Island