File:Subfluvial-karst-springs Pellana-basin Peloponnese.jpg
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Deutsch: 19 subfluviale Karstquellen entspringen am Rande des poljeähnlichen „Pellana“-Beckens im Flussbett und am Ufer des Flusses Evrotas, auf dem Peleponnes, Griechenland. Bei Hochwasser treten fast alle Quellen unter Wasser aus. Am Pellana-Beckenboden und dem Fluss Evrotas richten sich langfristig die Verkarstung des Kalksteingebirges Parnon, der Karstgrundwasserspiegel und die Austrittsstellen aus. Subfluviale Quellen sind ein seltenes und auch wenig dokumentiertes, Phänomen. Vier der Quellen haben eine große Schüttung. English: 19 Subfluvial karst springs, Peloponnese. The springs emerge at the river bed or its banks. All conduits and porous structures in the groundwater of the karstic Parnon mountains have their hydrological base level for discharge at the impermeable “Pellana”-polje floor (5km wide close depression, well cultivated) and at the river Eurotas. During floods, all springs are submerged. Subfluvial springs are relatively rare and poorly documented. Four springs have large water yields. “Landsat 8”, 30 m sensor image, 2015, courtesy U.S. Geological Survey. |
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| Source | Own work |
| Author | Ustill |
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| current | 17:09, 16 December 2016 | | 1,200 × 1,568 (2.05 MB) | Ulrichstill (talk | contribs) | User created page with UploadWizard |
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