Babbacombe Bay is a South-East Devon shallow, wide, continuation of the main sweep of Lyme Bay which, in turn, to the east is the western end of the Jurassic Coast (mainly in Dorset) in England, UK. It faces east towards the parent, notably large bay of the English Channel, weakly sheltered from large tides from the east but much so from Atlantic tides, currents and storms from the west. As a sub-bay it covers about 4.5 mi. It is bounded by: Some of the much removed crystalline deposits of gold at the southern point are in a longstanding exhibit of the Natural History Museum, London. These are notable to mineral collectors. Dawlish along the bay is a town which saw its seaside mainline railway rebuilt quickly due to the unusually fierce 2013–14 United Kingdom winter floods. Sand in several places, and cliffs are often red and derived from Permian New Red Sandstone, interspersed with outcrops of Devonian Limestone.