A History of the County of York East Riding, Volume 4
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The volume covers a large area at the southern end of the Yorkshire Welds, lying west of the city of Hull and the town of Beverley. It is concerned with the history of fourteen parishes which comprise the greater part of the Hunsley Beacon division of Harthill wapentake. Though the rolling chalk hills of the wolds dominate the area, several of the parishes extend into the low- lying ground of the Hull valley to the east and the Vale of York to the west. InSouth Cave parish the reclamation of Broomfleet Island from the river Humber adds further variety to the agricultural history of the area. T...
The volume covers a large area at the southern end of the Yorkshire Welds, lying west of the city of Hull and the town of Beverley. It is concerned with the history of fourteen parishes which comprise the greater part of the Hunsley Beacon division of Harthill wapentake. Though the rolling chalk hills of the wolds dominate the area, several of the parishes extend into the low- lying ground of the Hull valley to the east and the Vale of York to the west. InSouth Cave parish the reclamation of Broomfleet Island from the river Humber adds further variety to the agricultural history of the area. There are several deserted medieval villages. Much of the countryside described here is still wholly rural in character, but some of the settlements lying on the eastern slopes of the welds, like Cherry Burton and Skidby, have become commuter villages for the near-by towns. The large medieval vil-lage of Cottingham became a popular place of residence for Hull merchants in the late 18th century, and much of the parish has since been absorbed within the city; the village now houses many of the students of the University of Hull. Notable country houses described in the volume include Dalton Hall and Houghton Hall, and the churches include an outstanding Norman building at Newbald. Many of the villages consist of brick houses of the 18th century and later, but 17th-centurytimber-framed houses survive at South Dalton and Cot-tingham. In other villages, however, much use is made of the local Jurassic limestone which outcrops below the wolds escarp-ment. At Leconfield there survives the moated site ofa seat of the Percy family, earls of Northumberland, and it was from Rowley that the rector emigrated in the 17th century to found a town of the same name in Massachusetts.
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