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Kingston magnetic grid geodetic

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Created 20/01/2025

Updated 20/01/2025

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Total magnetic intensity (TMI) data measures variations in the intensity of the Earth's magnetic field caused by the contrasting content of rock-forming minerals in the Earth crust. Magnetic anomalies can be either positive (field stronger than normal) or negative (field weaker) depending on the susceptibility of the rock. The data are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose. This Kingston magnetic grid geodetic has a cell size of 0.00083 degrees (approximately 88m). The units are in nanoTesla (or nT). The data used to produce this grid was acquired in 1998 by the WA Government, and consisted of 47325 line-kilometres of data at 400m line spacing and 80m terrain clearance.

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Title Kingston magnetic grid geodetic
Language eng
Licence notspecified
Landing Page https://devweb.dga.links.com.au/data/dataset/7a7c7dc8-4526-49e6-88fe-1aebb3248e9e
Contact Point
Geoscience Australia
clientservices@ga.gov.au
Reference Period 08/07/1998 - 05/09/1998
Geospatial Coverage {"type": "Polygon", "coordinates": [[[121.4895, -27.0072], [123.0103, -27.0072], [123.0103, -25.9923], [121.4895, -25.9923], [121.4895, -27.0072]]]}
Data Portal data.gov.au