The late Cainozoic evolution of the Carpentaria Plains, North Queensland: a discussion

Created 17/10/2025

Updated 17/10/2025

Grimes and Doutch (1978) have identified five predominantly alluvial stages in the depositional landforms of the Carpentaria Plains. In the light of the factors which they consider to be the most likely controls on the evolution of the plains, they suggest a correlation between these stages, sea-level, climatic changes, and other depositional sequences in Queensland.

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Field Value
Title The late Cainozoic evolution of the Carpentaria Plains, North Queensland: a discussion
Language eng
Licence Not Specified
Landing Page https://data.gov.au/data/dataset/570d60e2-6712-4945-9972-8b1228bca5ee
Contact Point
Geoscience Australia Data
clientservices@ga.gov.au
Reference Period 20/04/2018
Geospatial Coverage
Map data © OpenStreetMap contributors
{
  "coordinates": [
    [
      [
        138.0,
        -29.2
      ],
      [
        154.0,
        -29.2
      ],
      [
        154.0,
        -10.0
      ],
      [
        138.0,
        -10.0
      ],
      [
        138.0,
        -29.2
      ]
    ]
  ],
  "type": "Polygon"
}
Data Portal Geoscience Australia

Data Source

This dataset was originally found on Geoscience Australia "The late Cainozoic evolution of the Carpentaria Plains, North Queensland: a discussion". Please visit the source to access the original metadata of the dataset:
https://ecat.ga.gov.au/geonetwork/srv/eng/csw/dataset/the-late-cainozoic-evolution-of-the-carpentaria-plains-north-queensland-a-discussion