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File:Sinas-Valley misty-morning Levidi Peloponnese Greece.jpg

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Ελληνικά: οροπέδιο, κάμπος κοντά σε Λεβίδι Αρκαδίας, ηκαρστικο φαινομένων, Πελοπόννησο, Ελλάδα. Καθε 4-5 χρονια, οταν οι μεγαλες ποσοτητες νερου συσσωρευτηκαν η μπλοκαριστηκαν, υπηρχε κατακρατηση νερου. Οταν η ποσοτητα του νερου, ηταν πολυ μεγαλη, διμιουργηθη λιμνη.

English: Valley-like plateau, a connection between the Levidi polje and the very large Tripoli Polje (28 km; a karst basin/depression in 670 m. Relatively frequent geological phenomenon in the karst basins of the northeast Peloponnese, Greece.
The valley has no natural surface water outlet. Precipitation must be drained by ditches. When precipitation of winters is exceptionally rich, some agricultural fields may be wet or even flooded - depending on the capacity of the ditches and the small Sinas ponor.

Deutsch: Trichterförmige Hochebene in 670 m, ein Karstbecken (Polje). Die von Berghöhen flankierte, talartige Hochebene ist ein Verbindungstück zwischen dem Levidi Polje und dem sehr großen Tripoli-Polje (28 km). Die oberirdisch abflusslose Hochebene ist eine relativ häufige geologische Erscheinung im nordöstlichen Peloponnes, Griechenland.
Die landwirtschaftlich genutzten Felder sind durch Niederschlag schnell nass. In besonders niederschlagsreichen Wintern kann es auch heute noch zu sehr nassen Böden kommen, so dass auch gepflegte Entwässerungsgräben und das kleine Sinas-Polje nicht reichen.
Date 2nd May, 2007, time 7 a.m.
Source Own work
Author ulrichstill

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current16:23, 13 November 2018Thumbnail for version as of 16:23, 13 November 20181,800 × 1,200 (1.18 MB)Ulrichstill (talk | contribs)User created page with UploadWizard

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