Folkestone - Geography

Geography

Folkestone is located where the southern edge of the North Downs, escarpment meets the sea. In contrast to the white cliffs at Dover further to the east, the cliffs at Folkestone are composed of Greensand and Gault Clay. A small stream, the Pent Stream, cuts through the cliffs at this point, and provided the original haven for fishermen and cross-channel boats. The cliffs are constantly under attack from the sea: the original headlands, which once protected the port, ceased to do so, and artificial protection, in the form of breakwaters and piers have been necessary since the 17th century.

The town is now built on both sides of the original valley: the West Cliff and The Bayle to the West, and the East Cliff on the other side of the stream. The Pent Stream now runs through a culvert from the fire station, at the junction of Radnor Park Road, Park Farm and Pavilion Road, until it reaches the inner harbour. Remains of a quay, dating to the 17th century, were discovered under what is now a public car park, between the Old High Street and the railway viaduct, adjacent to the current harbour. Included in the town is Cheriton, where the Channel Tunnel northern exit is located; Newington; and Peene.

On 28 April 2007, an earthquake with its epicentre 1 km East of Folkestone occurred at 8:18am. It was registered at 4.2 on the Richter scale, and was felt for up to 15 seconds.

On 3 March 2009, a second earthquake shook Folkestone, measuring 2.8 on the Richter Scale. It only lasted around two seconds.

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