65 Microtesla To Tesla

Magnetic anomalies are local variations of the magnetic field produced by magnetic material subsurface layers. The intensity of the magnetic field on the earth ranges from a minimum of about 025 Gauss G or 25 microtesla μT at the magnetic equator to more than 065 G near the magnetic poles.

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Fields Greater Than 0 2 Or 0 4 µt

Fields Greater Than 0 2 Or 0 4 µt

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