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Continuous inflow of seawater and outflow of brackish water in the substratum of the Karstic Island of Cephalonia, Greece
Continuous inflow of seawater and outflow of brackish water in the substratum of the Karstic Island of Cephalonia, Greece
dc.date.accessioned:
2021-08-04T20:53:23Z
dc.date.available: 2021-08-04T20:53:23Z
dc.date.issued: 1988
dc.identifier.uri: http://ermis.di.ionio.gr/xmlui/handle/123456789/1146
dc.description: This study proposes a new explanation connected with the existence of a marine current which creates a hydraulic gradient between the two sides of the island but with inflow being maintained by density flow. This made possible by a deep karstic conduit created during the Cenozoic period and which runs in the same direction as the marine current.
dc.language.iso: en
dc.subject: Cephalonia
dc.subject: Ionian Islands
dc.subject: Geology
dc.subject: Cenozoic period
dc.title: Continuous inflow of seawater and outflow of brackish water in the substratum of the Karstic Island of Cephalonia, Greece
dc.type: Working Paper
dc.date.available: 2021-08-04T20:53:23Z
dc.date.issued: 1988
dc.identifier.uri: http://ermis.di.ionio.gr/xmlui/handle/123456789/1146
dc.description: This study proposes a new explanation connected with the existence of a marine current which creates a hydraulic gradient between the two sides of the island but with inflow being maintained by density flow. This made possible by a deep karstic conduit created during the Cenozoic period and which runs in the same direction as the marine current.
dc.language.iso: en
dc.subject: Cephalonia
dc.subject: Ionian Islands
dc.subject: Geology
dc.subject: Cenozoic period
dc.title: Continuous inflow of seawater and outflow of brackish water in the substratum of the Karstic Island of Cephalonia, Greece
dc.type: Working Paper
This study proposes a new explanation connected with the existence of a marine current which creates a hydraulic gradient between the two sides of the island but with inflow being maintained by density flow. This made possible by a deep karstic conduit created during the Cenozoic period and which runs in the same direction as the marine current.
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