Cave detection using multiple geophysical methods: Unicorn cave, Harz Mountains, Germany

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  • Georg Kaufmann
    Free University of Berlin, Institute of Geological Sciences 1 , Berlin, Germany . E-mail: georg.kaufmann@fu-berlin.de ; dromanov@zedat.fu-berlin.de .
  • Douchko Romanov
    Free University of Berlin, Institute of Geological Sciences 1 , Berlin, Germany . E-mail: georg.kaufmann@fu-berlin.de ; dromanov@zedat.fu-berlin.de .
  • Ralf Nielbock
    Gesellschaft Unicornu Fossile 2 , Osterode am Harz, Germany . E-mail: ralf@nielbock.de .

Bibliographic Information

Published
2011-04-12
DOI
  • 10.1190/1.3560245
Publisher
Society of Exploration Geophysicists

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Description

<jats:title>Abstract</jats:title> <jats:p>Unicorn cave in the southern Harz Mountains of Germany is a show cave in dolomitic rocks of the Zechstein Formation. The cave's trunk passage is interrupted by larger rooms. The overburden is only around 15 m. The passages are filled with sediments that can be up to 50 m thick. We used gravimetry and electrical resistivity imaging over the cave area to identify the subsurface voids and the extent of the sediment infill of the cave passages. Our choice of methods was based on several conditions unique to the cave: (1) well surveyed, (2) shallow overburden, (3) large air-filled passages, and (4) thick sediment cover, concealing true passage size. Using the cave survey as an initial model for the subsurface structure, we successfully identified the air-filled cave with both methods. We then inferred the thickness of the sediment infill by forward modeling and identified a possible southward continuation beyond the currently explored passages.</jats:p>

Journal

  • Geophysics

    Geophysics 76 (3), B71-B77, 2011-04-12

    Society of Exploration Geophysicists

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