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Southeast Lachlan, NSW, 2010 (P1218), elevation line data
The Digital Elevation Model represents ground surface topography between points of known elevation. The elevation data was calculated using the altimeters and Global Positioning... -
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Southeast Lachlan, NSW, 2010 (P1218), radiometric line data, AWAGS levelled
The radiometric, or gamma-ray spectrometric method, measures the natural variations in the gamma-rays detected near the Earth's surface as the result of the natural radioactive... -
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GSNSW Southeast Lachlan Uranium Grid Geodetic
The radiometric, or gamma-ray spectrometric method, measures the natural variations in the gamma-rays detected near the Earth's surface as the result of the natural radioactive... -
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GSNSW Southeast Lachlan TMI Grid Geodetic
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... -
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GSNSW Southeast Lachlan Doserate Grid Geodetic
The radiometric, or gamma-ray spectrometric method, measures the natural variations in the gamma-rays detected near the Earth's surface as the result of the natural radioactive... -
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GSNSW Southeast Lachlan Potassium Grid Geodetic
The radiometric, or gamma-ray spectrometric method, measures the natural variations in the gamma-rays detected near the Earth's surface as the result of the natural radioactive... -
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GSNSW Southeast Lachlan Elevation Grid Geodetic
Digital Elevation data record the terrain height variations from the processed point- or line-located data recorded during a geophysical survey. This GSNSW Southeast Lachlan... -
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GSNSW Southeast Lachlan Thorium Grid Geodetic
The radiometric, or gamma-ray spectrometric method, measures the natural variations in the gamma-rays detected near the Earth's surface as the result of the natural radioactive... -
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Southeast Lachlan, NSW, 2010 (P1218), magnetic line data, AWAGS levelled
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...
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