Subjacent karst collapse dolines: Overlying non-carbonate rock collapsed into a limestone cavern Factors conducive to sinkhole formation : flat land : doline formation is inversely proportional to slope as a result of lower infiltration rates and greater runoff rates.
(Subjacent karst collapse dolines: Overlying non-carbonate rock; collapsed; into a limestone cavern Factors conducive to sinkhole formation) (doline formation; is; inversely proportional to slope as a result of lower infiltration rates and greater runoff rates) (doline formation; to slope; as a result of lower infiltration rates and greater runoff rates)
Subjacent karst collapse dolines: Overlying non-carbonate rock doline formation doline formation
collapsed is to slope
into a limestone cavern Factors conducive to sinkhole formation
inversely proportional to slope as a result of lower infiltration rates and greater runoff rates
as a result of lower infiltration rates and greater runoff rates