where do the white cliffs start and end
White Cliffs of Dover The White Cliffs of Dover are cliffs that form part of the English coastline facing the Strait of Dover and France. The cliffs are part of the North Downs formation. The cliff face, which reaches up to 350 feet (110Â m), owes its striking appearance to its composition of chalk accented by streaks of black flint. The cliffs stretch along the coastline for eight miles (13 km), spreading east and west from the town of Dover in Kent, and part of them were purchased by the National Trust in 2016.[1] They are part of the Dover to Kingsdown Cliffs Site of Special Scientific Interest[2] and Special Area of Conservation[3]
Fold mountains Fold mountains form when two tectonic plates move towards each other at a convergent plate boundary. Fold mountains form from sedimentary rocks that accumulate along the margins of continents. When plates and the continents riding on them collide, the accumulated layers of rock may crumple and fold like a tablecloth that is pushed across a table, particularly if there is a mechanically weak layer such as salt.[1] They are also present in south africa, in many regions of the Western cape province.