Linked from
The 114 pages that link to Karst, each with the reason it gives.
LimestoneRelated: Carbon dioxide-rich water dissolves limestone and creates karst terrain.
CalciteRelated: Groundwater dissolves calcite-rich rock to create caves, sinkholes, and underground drainage.
Land subsidenceRelated: Dissolution and collapse of underground cavities can lower or suddenly break the surface.
Mediterranean basinRelated: Karst landscapes redirect water underground in parts of the basin.
MarbleRelated: Water dissolves marble along fractures, producing caves and sculpted landscapes.
DolomitesRelated: Dissolution of carbonate rocks shapes parts of the range’s terrain and water flow.
CarbonateRelated: Carbonate-rock dissolution creates caves, sinkholes, and underground drainage.
GuangxiRelated: Limestone karst landscapes shape much of Guangxi’s distinctive scenery.
Carbonate mineralRelated: Dissolving carbonate minerals create caves, sinkholes, and distinctive drainage systems.
HydrogeologyRelated: Karst aquifers can channel groundwater through conduits unlike ordinary porous media.
GuizhouRelated: Limestone dissolution gives much of Guizhou its distinctive landforms.
Madagascar dry deciduous forestsRelated: Limestone karst underlies distinctive forest habitats, including the Tsingy formations.
Cave BiologyRelated: Karst geology creates many of the connected underground habitats studied in cave biology.
Three GorgesRelated: Limestone formations and karst terrain occur around parts of the Three Gorges region.
Western DesertRelated: Limestone dissolution contributes to caves and depressions in parts of the desert.
Carbonate rockRelated: Carbonate dissolution creates caves, sinkholes, and distinctive drainage patterns.
Taurus MountainsRelated: Limestone in the Taurus Mountains supports extensive caves and underground water systems.
SloveniaRelated: The Slovenian Karst gave this landscape type its international name.
GigantopithecusRelated: Many Gigantopithecus fossils come from caves in southern China’s karst terrain.
OzarksRelated: Limestone and dolomite make karst features widespread across the region.
Xiling GorgeRelated: Limestone features around Xiling reflect processes associated with karst landscapes.
Apuan AlpsRelated: Limestone dissolution helps shape the Apuan Alps’ rugged terrain and cave systems.
Apuseni MountainsRelated: Limestone dissolution produced many of the range’s caves and landforms.
Cave of SwallowsRelated: Dissolution of limestone helped create the cave's deep shaft.
LiuzhouRelated: Limestone karst formations characterize the terrain around Liuzhou.
Nanjing ManRelated: Hulu Cave formed in a karst setting that accumulated fossils and sediments.
OoliteRelated: Dissolution can enlarge openings in oolitic limestone and create karst features.
Subterranean biologyRelated: Karst geology creates many connected cave and groundwater habitats.
Verdon GorgeRelated: Limestone dissolution contributes to the wider terrain surrounding the canyon.
Aare GorgeRelated: Limestone dissolution helps explain how water can widen fractures around the river channel.
Calcium bicarbonateRelated: Bicarbonate-forming water dissolves limestone and contributes to caves and sinkholes.
Cerro SarisariñamaRelated: The summit pits resemble karst sinkholes, though Sarisariñama’s sandstone setting differs from classic limestone karst.
Huanglong Scenic and Historic Interest AreaRelated: Dissolving and redepositing carbonate rock links Huanglong’s scenery to karst processes.
Judaean MountainsRelated: Dissolving limestone creates caves and other features in the range.
Jugurtha TablelandRelated: Limestone dissolution is a regional process that can shape the mesa’s rock surfaces and cavities.
KönigsseeRelated: Karst drainage helps connect the lake’s mountain setting with its clear waters.
Kuang Si FallsRelated: The falls lie in a limestone landscape where water can dissolve and redeposit rock.
MangaiaRelated: Rainwater has dissolved Mangaia’s limestone makatea into rugged terrain and caves.
Near-surface geophysicsRelated: Shallow surveys can detect cavities and void-prone zones that threaten construction.
Ordesa ValleyRelated: Karst processes shape the limestone terrain around the valley.