File:Landsat-2000 Submarine-springs Argolis-Gulf Greece.jpg

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Deutsch: Ostküste des Peloponnes, Küste des Argolischen Golfs und Ort einer Kette von Karstquellen ( „Küstenquellen“ und „submarine Quellen“).

Das Niederschlagswasser sinkt durch das hochgradig verkarstete Kalkgebirge des nordöstlichen Peloponnes (500-700 m) ins Karstgrundwasser. Unterschiedlich große, meist aber kleine Karstquellen fließen in abflusslose Becken (Poljen) und dort gleich wieder in Katavothren (pl., griechisch für Ponore), die über große Gänge (oder sogar Höhlen) mit ihrer Verkarstungsbasis („Grundwasservorfluter“), dem Meer, verbunden sind. Die gangartig weiten Wasserwege im Karst sind an den Küsten denen der Mittemeerküsten vergleichbar.

Public Domain Image NASA World Wind, Landsat 7.

English: East coast of the Peloponnese, the Argolic Gulf and a chain of karst springs (coastal and submarine springs, beeing related to their natural water base level).

The karst water at sea level comes mainly from the karstified plateau (500 – 700 m) of the Northeast Peloponnese. Many small karst springs emerge in eight large and several smaller poljes (closed depressions). Their fresh water then collects in katavothres (pl., Greek for ponors) and flows through conduits to the karst base level “sea”. Conduits and karst springs at sea level may be compared with similar karst conditions at coasts of the Mediterranean Sea.

Image based on Landsat 7, NASA World Wind.
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Author Ustill

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This image is in the public domain because it is a screenshot from NASA’s globe software World Wind using a public domain layer, such as Blue Marble, MODIS, Landsat, SRTM, USGS or GLOBE.

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Date/TimeThumbnailDimensionsUserComment
current16:23, 9 March 2020Thumbnail for version as of 16:23, 9 March 2020800 × 1,200 (1.52 MB)Ulrichstill (talk | contribs)corrected positions and added some names
17:17, 16 December 2016Thumbnail for version as of 17:17, 16 December 2016800 × 1,200 (1.51 MB)Ulrichstill (talk | contribs)User created page with UploadWizard

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