308:, as described in the Yucatán peninsula (Mexico). The vertical shaft gives access to the water table (where you can do a round trip on a small boat). This groundwater is brackish, mixing between fresh water recharge inland and sea water intruded in depth in the island. Huge karst conduits have been explored by speleo-divers. The bay of Sami has many cenotes, with impressive shafts, that have been inventoried in a GIS Database . The brackish water flowing through the cenotes outflows along the sea shore, forming brackish coastal and submarine springs. The groundwater of Melissani cave outflows at the "Fridi" beach. This brackish water is part of a famous hydrogeological phenomena : seawater is sucked in the west part of the island of Kefalonia, near Argostoli, and expelled in the bay of Sami. In Argostoli, the seawater flows into sinkholes, named
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The lake's bottom is covered with stones. Plants grow at the opening of the cave. The color of the stone near the opening is stucco to honey-like brown.
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Melissani cave is a typical feature of karst environment in coastal carbonate aquifer. It forms a kind of
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332:. V. Maurin, J. Zoetl. Symposium on hydrology of fractured rocks 1965, IAHS Redbooks Pub74 1967.
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Salt water encroachment in the low-altitude karst water horizons of the island of
Kephallinia
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The cave was rediscovered in 1951 by [[ Leonardo ]].
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419:Tourist attractions in the Ionian Islands (region)
16:Cave located on the island of Kefalonia, Greece
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109:Learn how and when to remove this message
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149:Excavations from Melissani, made under
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260:Latitude: 38.26 (38°15′25″) N
257:Longitude: 20.6 (20°37′25″) E
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169:Λιμνοσπήλαιο Μελισσάνης
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