File:Kato-Lousi-Kampos Polje Peloponnese Greece.jpg

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Ελληνικά: οροπέδιο, Κάτω_Λουσοί_Αχαΐας, η καρστικο 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: Plateau Lousi, Achaea (a karst depression 950-1050 m, polje), on all sides surrounded by mountains. On its north east border is the village Kato Lousi. 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 become wet. Depending on the capacity of the ditches and the geologically old ponors some fields may even be flooded.

Deutsch: Hochebene von Lousi in 950-1050 m, (ein Karstbecken, Polje). Die große Polje (ca. 14 km) wird vollständig von Bergen umgeben. An seinem nordöstlichen Rand liegt das Dorf Kato Lousi. Das oberirdisch abflusslose Karstbecken ist eine relativ häufige geologische Erscheinung im Peloponnes, Griechenland.
Die landwirtschaftliche Nutzung der Felder ist bei hohem Niederschlag beeinträchtigt. In besonders niederschlagsreichen Wintern kann der Boden zu lange nass sein, wenn die Kapazität von Entwässerungsgräben und der uralten Ponore nicht ausreicht, oder sogar unterirdische Karstwasserwege verstopft sind.
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Author ulrichstill

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11 May 2006

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current17:01, 14 November 2018Thumbnail for version as of 17:01, 14 November 20181,800 × 1,200 (1.31 MB)wikimediacommons>Ulrichstill

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