Runoff in the Brunel Chamber

Ruissellements de la salle Brunel

In the southwest of the chamber, runoff (a) from the Entrance sector (b) cuts through the fine sediment making up the floor. The particles carried were deposited by decantation, and have covered the Palaeolithic circulation surface to the northwest. One area of subsidence is visible on the left of the photo (c).

Vist the site : The Chauvet-Pont d'Arc cave