Field technician carrying magnetometer across rocky hillside during potential field methods survey to measure natural magnetic variations and map subsurface structure and lithologic contrasts across regional terrain.
Potential Fields

Measuring Natural Field Variations

Potential field methods measure naturally occurring variations in the Earth’s magnetic and gravitational fields. These variations are influenced by subsurface material properties and structure, allowing broad-scale characterization without introducing energy into the ground.

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Potential Fields

When Broad Coverage Is Needed

In many settings, subsurface features extend beyond the resolution of localized investigation methods. Potential field surveys are used to identify large-scale geologic features, material contrasts, and structural trends that support regional understanding and guide focused follow-up investigations.

Potential Fields

Field-Based Potential Methods

Potential field methods rely on passive measurement of natural Earth fields. These approaches are well suited for regional-scale investigation and are commonly used to support broader subsurface characterization efforts.

Magnetic Surveys

Measure variations in the Earth’s magnetic field caused by subsurface materials.

Gravity Surveys

Detect small changes in gravitational acceleration related to density contrasts.

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