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Sinkholes

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Encyclopedia of Engineering Geology

Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

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Sinkholes are among the most obvious karst phenomena. They are closed depressions in the ground surface resulting from downward movement into karst cavities of exposed soluble rocks; of soluble rocks together with covering soils, rocks, and particles; or of covering material only without dissolution. This movement can be the result of dissolution, erosion, and various hydraulic failures, as well as by gravitational failure of rocks and soils. Sinkholes may be full of water (Fig. 1). Old sinkholes that are filled with, and often covered by, younger sediments are termed buried sinkholes.

Fig. 1
figure 1

Sinkhole formed in 2012 in Belozerye village, Nizhny Novgorod region, Russia

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References

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Correspondence to Victor P. Khomenko .

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Khomenko, V.P., Tolmachev, V.V. (2017). Sinkholes. In: Bobrowsky, P., Marker, B. (eds) Encyclopedia of Engineering Geology. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-12127-7_262-1

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  • DOI: https://doi.org/10.1007/978-3-319-12127-7_262-1

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  • Print ISBN: 978-3-319-12127-7

  • Online ISBN: 978-3-319-12127-7

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