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Gap topographic map
Click on the map to display elevation.
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Gap
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.
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About this map
Name: Gap topographic map, elevation, terrain.
Average elevation: 1,146 m
Minimum elevation: 629 m
Maximum elevation: 2,374 m
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