Seeing Beneath the Surface — Geophysical Survey Methods Explained

Geophysical Survey Methods Explained

Why Geophysical Surveys Matter

Geophysics lets us explore what lies beneath Earth’s surface without digging. Whether you’re hunting for gold, mapping groundwater, or planning a city, geophysical methods reveal hidden layers, faults, and resources.


Core Geophysical Methods

MethodWhat It DetectsBest For
SeismicWave velocity through rock layersOil & gas, fault zones, site stability
MagneticMagnetic anomalies in subsurface rocksMineral exploration, structural mapping
ElectricalResistivity of underground materialsGroundwater, pollution, archaeology
GravityDensity variations in Earth’s crustBasin modeling, tectonic studies
GPRRadar reflections from shallow featuresUtilities, archaeology, shallow mapping

How Each Method Works

  • Seismic: Sends shock waves into the ground; measures how fast they bounce back.
  • Magnetic: Detects iron-rich or magnetized zones using field sensors.
  • Electrical: Injects current into the ground; measures resistance to flow.
  • Gravity: Measures tiny changes in gravitational pull caused by rock density.
  • GPR: Emits radar pulses; records reflections from buried objects or layers.

Real-World Applications

  • Mining: Locate ore bodies, faults, and safe drilling zones.
  • Urban Planning: Assess subsurface stability before construction.
  • Environmental Studies: Detect buried waste, groundwater flow, or contamination.
  • Archaeology: Reveal buried structures without excavation.
Seeing Beneath the Surface — Geophysical Survey Methods Explained

What’s Next

In the next post, we’ll explore the importance of geology.

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