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Solution (CTX_1)
DGIF baseline 2026-1, the latest. Earlier baselines: timemap.
RDF: ctx_1.ttl
- Name
solution
- Attribute
- CTX Cave Type
- Definition
- Predominately formed in carbonate and sulphate rocks such as limestone, dolomite, marble, and gypsum by the action of slowly moving ground water that dissolves the rock to form tunnels, irregular passages, and caverns along bedding-planes, faults and joints.
- Description
- Caves can also form in other materials, including chalk, salt, granite, loess, sandstone and gypsum. The natural acids in groundwater assist in dissolving the rocks. Limestone caves are frequently adorned with formations such as, stalactites, stalagmites, soda straws and columns. Most of the caves in the world are solution cave. It takes geological epochs for cracks to expand into caves or cave systems.
- Accepted
- 2013-10-18
- Allowed for
Source: DGIF 2026-1 QEA model, DGIWG. Standard: DGIWG 206-3. Licence: CC BY 4.0, © DGIWG.