The Alpine orogeny also led to more distant and smaller geological features such as the chalk hills in southern England and northern France (the 'Weald–Artois Anticline'). The remains of this can be seen in the chalk ridges of the North and South Downs in southern England. Its effects are visible on the Isle of Wight, where the chalk and overlying Eocene strata are folded to near-vertical, as seen at Alum Bay and Whitecliff Bay, and on the Dorset coast near Lulworth Cove.