Ditton, Kent - Geography

Geography

This history of Ditton has, in part, been shaped by the availability of natural resources in the area, especially water, soil and rocks. Its position in relation to transport links with London, notably the main roads and railways which tend towards the capital city, has also contributed to the village's development. Nowadays the parish is characterised by industrial units to the north, the middle by residential estates, and the south by fields and woodland.

The parish of Ditton lies in the Medway valley and borders the River Medway to the north and the Weald to the south. The river Medway is Kent’s principal river and rises near East Grinstead in Sussex, flowing eastwards to Maidstone. After passing Ditton parish it turns north and cuts through the North Downs at Rochester, joining the estuary of the River Thames as its final tributary near Sheerness. The Medway is some 112 kilometres (70 mi) long.

The availability of water to transport products and raw materials, and as a resource used in the manufacture of paper, was essential to the historical development of paper mills in the area. Bradbourne stream, which meanders through the parish in a south-east to north-west direction, rises in East Malling, crosses under the A20 road and M20 motorway, and joins the river Medway near the Aylesford Newsprint site. Historically the availability of running water was essential to the early settlements that grew up in Kent, and to the establishment of industries in the area; such as providing power to drive the mills which ground grain.

Ditton is situated between the Lower Weald and the Chalk (North) Downs. The parish encompasses the Lower Greensand strata, where a formation of hard sandy limestone known as the Hythe Beds is abundant. From this formation ragstone is obtained. Kentish ragstone was a historically important building material in south east England. The Romans used ragstone in the construction of London and villas in the south-east. Medieval builders used ragstone to build churches, civic buildings, houses and bridges over local rivers. The predominance of ragstone beds in the locality gave Ditton a legacy of quarrying which continues today.

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