From Geoscience Australia
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Some observations on laterites in the Northern Territory

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Created 20/01/2025

Updated 20/01/2025

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In the Northern Territory laterites are formed in situ as: (i) an illuvial soil horizon; and (ii) a chemical lake laterite deposit. The end product of extensive weathering processes of certain favourable beds is considered by some to be a true mature laterite, whereas others believe it is merely a duricrust. The denudation of laterite and transportation, deposition and cementation of the fragments with other rock fragments result in a detrital laterite deposit. Water-rounded rock fragments in the detrital laterites are readily coated and cemented with iron oxides and resemble the pisolites in the ferruginous zone of the lateritic profile. This similarity results in an exaggeration of the true extent of laterization. The similarity in environmental conditions between the process of precipitation of uranium minerals and laterization is discussed. True mature and detrital laterites are illustrated by photographs.

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Title Some observations on laterites in the Northern Territory
Language eng
Licence notspecified
Landing Page https://devweb.dga.links.com.au/data/dataset/cfb23fea-a65f-4df8-92b0-6693495298ba
Contact Point
Geoscience Australia
clientservices@ga.gov.au
Reference Period 22/04/2018
Geospatial Coverage {"type": "Polygon", "coordinates": [[[129.5, -15.0], [133.5, -15.0], [133.5, -12.0], [129.5, -12.0], [129.5, -15.0]]]}
Data Portal data.gov.au

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This dataset was originally found on data.gov.au "Some observations on laterites in the Northern Territory". Please visit the source to access the original metadata of the dataset:
https://devweb.dga.links.com.au/data/dataset/some-observations-on-laterites-in-the-northern-territory

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