Keal Cotes - Geography

Geography

The village is situated on flat ground at the south western rim of the attractive rolling Lincolnshire Wolds. Keal Cotes is at the northern edge of a tract of marsh and fen land, bounded by Boston deeps and the North Sea and is within seventeen miles inland from the holiday centre of Skegness, on what many consider is the best part of the Lincolnshire coast.

The Wolds comprise a series of low hills and steep valleys underlain by calcareous chalk, green limestone and sandstone rock, laid down in the Cretaceous period under a shallow warm sea. The characteristic open valleys of the Wolds were created during the last ice age through the action of glaciation and meltwater.

Geographically, the Lincolnshire Wolds are a continuation of the Yorkshire Wolds which run up through the East Riding of Yorkshire, the Wolds as a whole having been bisected by the tremendous erosive power of the waters of the Humber. The Fenlands that stretch down as far as Norfolk are former wetlands consisted both of peat bogs and tidal silt marshes which were virtually all drained by the end of the 19th century when Keal Cotes had its longest period of Victorian expansion. The former peat fens and silt marshes provided a rich loamy soil that was ideal for the growing of cereal and vegetable crops and gave Lincolnshire its reputation as being the 'bread basket' of England. The resulting flat lands also made an ideal environment for the later mechanisation of farming in the mid 20th century. The soil in the village is a rich brown loamy earth over a heavy clay subsoil.

The drainage of the wetlands was organised into a combination of river and manmade drainage, aiding the passing of upland water through the region with internal drainage of the land between existing rivers. The internal drainage was designed to be organized by levels or districts each of which includes the fen parts of one or several parishes. The details of the organisation varies with the history of their development, but Keal Cotes falls within the Witham Fourth District: (East, West and Wildmore Fens and the Townland from Boston to Wainfleet). The manmade East Fen Catchwater Drain passes close to Keal Cotes ensuring that, although low lying, the possibility of flooding is almost non existent. Minor problems have occurred in recent years through farmers and householders failing to properly complete the expected annual clearing of minor feeder drains around their properties. Additionally many householders have chosen to pipe the drains through and around their gardens, greatly reducing their ability to handle higher levels of land drainage in heavy rain.