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Part of Mont Aiguille
Credit
: A. Poiraud
Description
The alluvial fan is the lower section of a mountain stream where sediment is deposited. The fan is clearly visible in front of you, and its sediment comes from the northern foot of Mont Aiguille. The Côtes stream from Trézanne struggles to make its way through all the tributaries of the Ruines stream.
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Lat, Lng
44.83924285.5823066
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Point of Interest updated on 24/06/2025
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