Karst

Karst is a type of landscape shaped as groundwater dissolves soluble bedrock, most often limestone or dolomite. Its interconnected surface and underground features can include sinkholes, caves, sinking streams and springs. Karst also forms important aquifers, but water can move through them quickly with limited natural filtration, making them particularly vulnerable to contamination.

Last updated
17 October 2026
Confidence
High (96%)
Sources
5
Versions
1
This article was researched and drafted with AI assistance and checked by an automated review pass. It is not guaranteed to be accurate — verify important facts against the references below.

Formation and defining features

Karst develops where water circulates through soluble rock and gradually enlarges cracks, fractures and other openings. Limestone and dolomite are common bedrock, while marble and gypsum can also form karst landscapes. Rainwater that absorbs carbon dioxide in soil becomes mildly acidic; over long periods, it dissolves carbonate rock and widens passages underground. The resulting terrain may contain caves, underground streams and springs as well as sinkholes—depressions formed when bedrock dissolves below the surface or a cave roof collapses. A stream may disappear into a fissure or sinkhole and re-emerge at a spring. Because drainage often runs beneath the surface, some karst regions have few permanent surface streams or lakes. Caves are one visible part of karst systems, but the term describes a broader landscape and drainage pattern.

Different karst landscapes

Karst does not have a single appearance. Local rock type, fractures, rainfall and groundwater circulation help determine which features dominate. Some areas have exposed, grooved limestone pavement; others are marked by enclosed depressions, cave networks, or cone-shaped and tower-like hills. The name comes from the Karst (Kras) region of Slovenia, where limestone terrain displays characteristic karst forms. Similar landscapes occur in many parts of the world, although their surface features and underground drainage differ from place to place.

Groundwater and human communities

Karst formations can store and transmit substantial groundwater, and springs fed by karst aquifers are important water sources. Their open, connected flow paths also create a vulnerability: water and contaminants entering at the surface can move rapidly through underground conduits, often with less filtration than in many other aquifers. Understanding where water enters, travels and emerges is therefore important for protecting drinking-water supplies. Sinkhole formation is another practical concern; when underground dissolution or a cave collapse removes support beneath the surface, the ground above can subside suddenly and damage buildings or infrastructure.

Key facts

Subject
A landscape and drainage system formed by the dissolution of soluble bedrock
Common rocks
Limestone and dolomite; marble and gypsum can also host karst features
Typical features
Sinkholes, caves, sinking streams, underground drainage and springs
Water significance
Karst aquifers can be productive groundwater sources but are vulnerable to contamination
Name origin
The term comes from the Karst (Kras) region of Slovenia

Ask about this article

Answers use only “Karst” and its references, with citations.

References

  1. 1.
    Karst Limestone, Sinkholes & Caves

    Encyclopaedia Britannica · encyclopedia · reliability: high · retrieved 17 October 2026

    Supports: Overview of karst terrain, its development and forms, global distribution, and the historical origin of the term.

  2. 2.
    Karst Aquifers

    U.S. Geological Survey · other · reliability: high · retrieved 17 October 2026

    Supports: Describes soluble-rock karst, characteristic landforms, aquifer structure, groundwater value and contamination vulnerability.

  3. 3.
    Karst Landscapes - Caves and Karst

    U.S. National Park Service · other · reliability: high · retrieved 17 October 2026

    Supports: Explains characteristic surface features, soluble rocks, underground water movement, springs, sinkholes and water-quality concerns.

  4. 4.
    Solution Caves - Caves and Karst

    U.S. National Park Service · other · reliability: high · retrieved 17 October 2026

    Supports: Explains the dissolution of limestone and other soluble rocks by acidic water and the formation of solution caves associated with karst.

  5. 5.
    Karst, Sinkholes, and Land Subsidence

    U.S. Geological Survey · other · reliability: high · retrieved 17 October 2026

    Supports: Provides USGS information and resources on karst terrain, sinkholes and land subsidence.

References are suggested by the research engine and may be incomplete. Unverified URLs are omitted rather than guessed.

Article history

  1. Version 117 October 2026 · EditorCreated by Zapia