From Geoscience Australia
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Broken Hill 1 100k magnetic grid geodetic

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Created 13/01/2025

Updated 13/01/2025

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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 Broken Hill 1 100k magnetic grid geodetic has a cell size of 0.00021 degrees (approximately 21m). The units are in nanoTesla (or nT). The data used to produce this grid was acquired in 1994 by the NSW Government, and consisted of 56310 line-kilometres of data at a line spacing between 100m and 400m, and 60m terrain clearance.

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Title Broken Hill 1 100k magnetic grid geodetic
Language eng
Licence notspecified
Landing Page https://devweb.dga.links.com.au/data/dataset/d97f18b3-2707-4a7c-91ef-ffae7d08a802
Contact Point
Geoscience Australia
clientservices@ga.gov.au
Reference Period 01/10/1994 - 01/12/1994
Geospatial Coverage {"type": "Polygon", "coordinates": [[[140.9997, -31.9997], [141.4997, -31.9997], [141.4997, -31.4997], [140.9997, -31.4997], [140.9997, -31.9997]]]}
Data Portal data.gov.au

Data Source

This dataset was originally found on data.gov.au "Broken Hill 1 100k magnetic grid geodetic". Please visit the source to access the original metadata of the dataset:
https://devweb.dga.links.com.au/data/dataset/broken-hill-1-100k-magnetic-grid-geodetic