A geographic
sink is a depression within an
endorheic basin where water collects with no visible outlet. Instead of
discharging, the collected water is lost due to evaporation and/or
penetration (water sinking underground, e.g., to become
groundwater in an
aquifer). If the sink has
karstic terrain, water will sink at a higher rate than the surface evaporation, and conversely if the lakebed or sink bed has a layer of soil that is largely impervious to water (
hardpan), evaporation will predominate. Since dry lakes in sinks with hardpan have little penetration, they require more severe aridity/heat to eliminate collected water at a comparable rate as for a similar sink with appreciable penetration.