Karst topography is a landscape formed from the dissolution of soluble rocks such as
limestone,
dolomite, and
gypsum. It is characterized by underground drainage systems with
sinkholes,
dolines, and
caves. It has also been documented for
weathering-resistant rocks, such as
quartzite, given the right conditions. Subterranean drainage may limit surface water with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst surface developments might be totally missing.