Unconfined versus confined speleogenetic settings: variations of solution porosity.
Speleogenesis in confined settings generates cave morphologies that differ much from those formed in unconfined settings. Cavesdeveloped in unconfined settings are characterised by broadly dendritic patterns of channels due to highly competing development.In contrast, caves originated under confined...
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| Format: | Article |
| Language: | English |
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University of South Florida Libraries
2006-01-01
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| Series: | International Journal of Speleology |
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| Online Access: | http://www.ijs.speleo.it/pdf/63.534.35_Klimchouk.pdf |