Panoramic view from Manneporte in southwestern direction to the cliffs of the Falaise d'Aval, consisting mainly of white chalk, but also flintstone. Freeze-thaw effects in combination with rainwater and breaking of waves are the main causes of the frequent rock falls from the cliffs.
- Location
- View on OpenStreetMap
- Created
- on Thursday 29 August 2013 by Martin Mergili
- Keywords
- beach, cliff, coastscape, landslide, lightscape, marine processes, rock fall, sedimentary rocks
- Visits and license
- 6000 visits, CC BY-NC-SA 4.0 DEED license