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©2018 Enviroprobe Service, Inc. : 81 Marter Avenue : Mt. Laurel, NJ 08054 : 856.858.8584

SINKHOLE LOCATING

A sinkhole is the result of erosion of the subsurface. When underground water dissolves carbonate bedrock such as limestone, dolomite, or other soluble rock it creates subterranean passages, cavities and caves. This irregular, subsurface rock topography is known as karst.

 

These voids in the bedrock are inclined to sudden surface collapses (sinkholes). Sinkholes can also occur in areas with soft soil, in mining areas, or where some other subsurface disturbance has occurred.

Human activities which accelerate sinkhole formation

  • New development demands for ground-water resources

  • Lowering the water table

  • Changes in surface water flow

  • Increased weight from structures upon the cavernous bedrock.

Locating sinkholes and subsidence without digging, probing, or drilling can be accomplished using non-destructive field surveys.

 

The two main methods for detecting sinkholes are aerial photography and geophysical procedures.

Various geophysical investigation techniques can be used in Karst terrains including ground penetrating radar, electrical conductivity, electrical resistivitymagnetic field, very low frequency measurement (ELF), gravity field recording and seismic velocity measurements.

Logarithmic electrical resistivity color scale

2D Electrical Resistivity Profiling

A sinkhole is the result of erosion of the subsurface. When underground water dissolves carbonate bedrock such as limestone, dolomite, or other soluble rock it creates subterranean passages, cavities and caves. This irregular, subsurface rock topography is known as karst. These voids in the bedrock are inclined to sudden surface collapses (sinkholes). Sinkholes can also occur in areas with soft soil, in mining areas, or where some other subsurface disturbance has occurred.

Human activities which accelerate sinkhole formation

  • New development demands for ground-water resources

  • Lowering the water table

  • Changes in surface water flow

  • Increased weight from structures upon the cavernous bedrock.

Locating sinkholes and subsidence without digging, probing, or drilling can be accomplished using non-destructive field surveys. The two main methods for detecting sinkholes are aerial photography and geophysical procedures.

Various geophysical investigation techniques can be used in Karst terrains including ground penetrating radar, electrical conductivity, electrical resistivitymagnetic field, very low frequency measurement (ELF), gravity field recording and seismic velocity measurements.

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