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Geology of the Prince Charles Mountains, Antarctica

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Created 20/01/2025

Updated 20/01/2025

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The Prince Charles Mountains constitute by far the best-exposed cross section through the East Antarctic Shield, extending for over 500 kilometers along the drainage basin of the Lambert Glacier-Amery Ice Shelf system. They consist of three distinct geological terranes: the Archaean to 'Mesoproterozoic Ruker Terrane in the south and the Mesoproterozoic to early Neoproterozoic Fisher and Beaver-Lambert Terranes in the north.

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Title Geology of the Prince Charles Mountains, Antarctica
Language eng
Licence notspecified
Landing Page https://devweb.dga.links.com.au/data/dataset/ce21b7f5-d0c3-499d-88a7-d42563f187f9
Contact Point
Geoscience Australia
clientservices@ga.gov.au
Reference Period 20/04/2018
Geospatial Coverage {"type": "Polygon", "coordinates": [[[60.0, -75.0], [70.0, -75.0], [70.0, -70.0], [60.0, -70.0], [60.0, -75.0]]]}
Data Portal data.gov.au