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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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Field Value
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

Data Source

This dataset was originally found on data.gov.au "Geology of the Prince Charles Mountains, Antarctica". Please visit the source to access the original metadata of the dataset:
https://devweb.dga.links.com.au/data/dataset/geology-of-the-prince-charles-mountains-antarctica