Continuous inflow of seawater and outflow of brackish water in the substratum of the Karstic Island of Cephalonia, Greece

Έτος έκδοσης: 1988
URI: http://ermis.di.ionio.gr/xmlui/handle/123456789/1146
Περιγραφή: 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.
Γλώσσα: en
Λέξη-κλειδί: Cephalonia
Λέξη-κλειδί: Ionian Islands
Λέξη-κλειδί: Geology
Λέξη-κλειδί: Cenozoic period
Τίτλος: Continuous inflow of seawater and outflow of brackish water in the substratum of the Karstic Island of Cephalonia, Greece
Τύπος περιεχομένου: Working Paper