File:Kandila-Valley Peloponnese Greece.jpg

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Ελληνικά: οροπέδιο, κοντά σε Κανδήλα Αρκαδίας, καρστικο φαινομένων στο Λεκάνη του Ορχομενόυ, Πελοπόννησος, 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: Kandila section of the Plateau Orchomenus, a karst basin/depression in 630 m, (polje). Kandila Plateau is the north eastern extension of the large basin, with the village Kandia on its slope. Relatively frequent geological phenomenon in the karst basins of the northeast Peloponnese, Greece.
The plateau 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 geologically old ponors at the Plateau Orchomenus’ western section, a temporary lake may result even nowadays.

Deutsch: Kandila Plateau, Hochebene Orchomenos in 630 m, ein Karstbecken (Polje). Das große Becken Orchomenos hat einen nordöstlichen Ausläufer, an dessen Osthang liegt das Dorf Kandila. Das oberirdisch abflusslose Karstbecken ist eine relativ häufige geologische Erscheinung im nordöstlichen Peloponnes, Griechenland.
Die landwirtschaftliche Nutzung der Felder ist durch Niederschlag immer potentiell gefährdet. In besonders niederschlagsreichen Wintern kann es auch heute noch zu sehr nassen Böden kommen, so dass auch gepflegte Entwässerungsgräben nicht reichen.
Date 25th April, 2007, time 7 a.m.
Source Own work
Author ulrichstill

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current16:21, 13 November 2018Thumbnail for version as of 16:21, 13 November 20181,800 × 1,200 (2.19 MB)Ulrichstill (talk | contribs)User created page with UploadWizard

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