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.

• WeatheringBroader topic: Chemical weathering of soluble rock creates caves, sinkholes, and other karst features.

• CalciteRelated: Groundwater dissolves calcite-rich rock to create caves, sinkholes, and underground drainage.

• SpeleothemNarrower topic: Karst drainage supplies the mineral-rich water from which many speleothems form.

• Land subsidenceRelated: Dissolution and collapse of underground cavities can lower or suddenly break the surface.

• Cave conservationNarrower topic: Cave protection must account for surface activities that affect connected underground water systems.

• Carbonic acidBroader topic: Carbonic-acid-bearing water dissolves limestone and helps create karst landscapes.

• Chemical weatheringBroader topic: Carbonic-acid dissolution of carbonate rock creates characteristic caves and landforms.

• Mediterranean basinRelated: Karst landscapes redirect water underground in parts of the basin.

• Cave tourismNarrower topic: Karst processes create many of the caves visited by tourists.

• SpeleologyNarrower topic: Karst processes create many caves that speleologists investigate.

• 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.

• SpeleogenesisNarrower topic: Karst landscapes express the same dissolution processes that form many caves.

• GeomorphologyBroader topic: Karst terrain shows how groundwater can sculpt distinctive surface and underground forms.

• Groundwater flowBroader topic: Conduits can channel groundwater far faster than porous-media models predict.

• Yucatán PeninsulaNarrower topic: Limestone dissolution channels much of the peninsula’s rainfall underground.

• Underground RiverNarrower topic: Karst terrain commonly channels surface water into subterranean rivers.

• Carbonate mineralRelated: Dissolving carbonate minerals create caves, sinkholes, and distinctive drainage systems.

• Cave ecologyNarrower topic: Karst processes connect cave habitats to water, soils, and surface disturbance.

• Karst HydrologyNarrower topic: Karst hydrology concerns water behavior in this distinctive terrain.

• SinkholeNarrower topic: Sinkholes are characteristic surface features of landscapes shaped by underground dissolution.

• CavingNarrower topic: Many caves explored by cavers form in karst limestone landscapes.

• HydrogeologyRelated: Karst aquifers can channel groundwater through conduits unlike ordinary porous media.

• Show CaveNarrower topic: Many show caves form in karst landscapes where water dissolves limestone.

• StalagmiteNarrower topic: Karst landscapes supply the caves and fractured rock through which mineral-bearing water travels.

• Dinaric AlpsNarrower topic: Limestone dissolution gives much of the range its characteristic rugged terrain.

• Fluvial processesCompared with: Chemical dissolution shapes karst terrain, distinguishing it from sediment-driven fluvial landforms.

• Mammoth CaveNarrower topic: Mammoth Cave is part of a karst landscape where groundwater dissolves limestone.

• GuizhouRelated: Limestone dissolution gives much of Guizhou its distinctive landforms.

• Madagascar dry deciduous forestsRelated: Limestone karst underlies distinctive forest habitats, including the Tsingy formations.

• Sea caveCompared with: Karst caves form chiefly through chemical dissolution rather than coastal wave action.

• Cave BiologyRelated: Karst geology creates many of the connected underground habitats studied in cave biology.

• Cave formationNarrower topic: Karst landscapes form where groundwater dissolves limestone and other soluble rocks into cave systems.

• CenoteNarrower topic: Cenotes are characteristic sinkholes in karst terrain.

• 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.

• Cave passageNarrower topic: Karst processes produce many passages in limestone and other soluble rocks.

• LandformBroader topic: It shows how bedrock chemistry can create a distinctive landscape and drainage pattern.

• Postojna CaveNarrower topic: Postojna Cave is part of a landscape formed by groundwater dissolving limestone.

• Carbonate rockRelated: Carbonate dissolution creates caves, sinkholes, and distinctive drainage patterns.

• Cave explorationNarrower topic: Karst landscapes contain many caves and surface clues to underground openings.

• Taurus MountainsRelated: Limestone in the Taurus Mountains supports extensive caves and underground water systems.

• Yunnan–Guizhou PlateauNarrower topic: Limestone dissolution creates the plateau’s distinctive tower karst, sinkholes, and underground drainage.

• Nullarbor PlainNarrower topic: Limestone dissolution creates the Nullarbor’s caves and sinkholes.

• Sierra Madre OrientalBroader topic: Limestone in parts of the range has developed extensive caves and sinkhole terrain.

• GuilinNarrower topic: Karst processes created the steep limestone peaks that define the Guilin area.

• Hạ Long BayNarrower topic: Limestone dissolution created the bay’s rugged terrain and many of its caves.