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1 See also  





2 References  














Epiphreatic zone






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From Wikipedia, the free encyclopedia
 


Cross section showing the water table varying with surface topography as well as a perched water table
Cross-section of a hillslope depicting the vadose zone, capillary fringe, water table, and the phreatic or saturated zone. (Source: United States Geological Survey.)

In a cave system, the epiphreatic zoneorfloodwater zone is the zone between the vadose (unsaturated) zone above and phreatic (saturated) zone below. It is regularly flooded and has a significant porosity. It has a great potential for cave formation.[1]

See also

[edit]

References

[edit]
  1. ^ Prelovšek, Mitja (2009). Present-Day Speleogenetic Processes, Factors and Features in the Epiphreatic Zone: Dissertation (PDF). University of Nova Gorica. p. 5.
  • ^ "Aquifer Anatomy | EARTH 111: Water: Science and Society". www.e-education.psu.edu. Retrieved 2024-06-08.
  • ^ "Infiltration | hydrologic cycle | Britannica". www.britannica.com. Retrieved 2024-06-08.
  • ^ "saturated zone". Oxford Reference. Retrieved 2024-06-08.
  • ^ "USGS Unsaturated Zone Flow Project". wwwrcamnl.wr.usgs.gov. Retrieved 2024-06-08.
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  • Retrieved from "https://en.wikipedia.org/w/index.php?title=Epiphreatic_zone&oldid=1230592808"

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