Mapa topográfico Gap
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The cover of morainic debris is omnipresent in the Sillon de Gap but is not the only vestige of the Quaternary glaciation. There is also the typical topography of glacial valleys. The location of the town of Gap corresponds to an Ombilic glaciaire, where large quantities of clay were deposited. Upstream lies the Verrou glaciaire [fr] [glacial lock] of Pont-Sarrazin and downstream of Tourronde.