Subterranean drainage may limit surface water, with few to no rivers or lakes. In regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground.[4]
^"What is Karst?"(PDF). Environmental Science Institute. The University of Texas at Austin. 16 May 2006. Retrieved 25 December 2020.
^Jackson, Julia A., ed. (1997). "Karst". Glossary of geology (Fourth ed.). Alexandria, Virginia: American Geological Institute. ISBN0922152349.
^Doerr, S. H. (18 March 1999). "Karst-like landforms and hydrology in quartzites of the Venezuelan Guyana shield: Pseudokarst or "real" karst?". Zeitschrift für Geomorphologie. 43 (1): 1–17. Bibcode:1999ZGm....43....1D. doi:10.1127/zfg/43/1999/1.
^Billi, Andrea; De Filippis, Luigi; Poncia, Pier Paolo; et al. (February 2016). "Hidden sinkholes and karst cavities in the travertine plateau of a highly-populated geothermal seismic territory (Tivoli, central Italy)". Geomorphology. 255: 63–80. Bibcode:2016Geomo.255...63B. doi:10.1016/j.geomorph.2015.12.011.
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