MERIT vs. Other Methods
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Comparison of an image of a sinkhole at the USF Geo-Park using ground penetrating radar, electrical resistivity and MERIT.
Results: Surface methods only imaged the near surface clay layer, while the MERIT imaged the entire subsurface including topography of the limestone.
MERIT Image
- Penetration to 60 feet
- Limestone Surface Geometry Imaged
- Anomalies Fully Imaged
GPR Image
- Penetration to 12 feet
- Upper Clay Surface Imaged
ER Image
- Penetration to 24 feet
- Anomaly at 12 feet
- Sinkhole Not Imaged