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The crater, situated on calcareous soil, has collapsed due to erosion from rainfall and presents some characteristic depressions

Doline lungo il sentiero per il Colle dell'Arpione

Credit : Enzo Piacenza

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Description

The crater, situated on calcareous soil, has collapsed due to erosion from rainfall and presents some characteristic depressions, some of them quite large. These typical carsic features, formed by a collapse of the underlying soil, funnel water underground and are known locally as doline or inghiottitoi [swallowers, literally].

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44.27617967.3088093

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Point of Interest updated on 23/01/2023

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