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4 unusual facts about Vale of Pickering


Vale of Pickering

On the southern edge of the vale lies West Heslerton, where recent excavation has revealed continuous habitation since the Late Mesolithic Age, about 5000 BC.

In the 17th and 18th centuries wealthy landowners created fine buildings and estates such as those at Wykeham Abbey estate, Nunnington Hall and Ebberston Hall.

For its latitude this area is mild in winter and cooler in summer due to the influence of the Gulf Stream in the northern Atlantic Ocean.

Nunnington Hall, 17th century manor House with a sheltered walled garden on the banks of the River Rye.


Bransdale

It carries a river called Hodge Beck en route from Cockayne to the River Dove from Farndale three miles south of Kirkbymoorside, which runs on into the Vale of Pickering and the River Rye.

Kirkdale, North Yorkshire

Kirkdale is a valley in North Yorkshire, England, which along with Sleightholmedale makes up the larger Bransdale and carries the Hodge Beck from its moorland source near Cockayne to the River Dove and onto the River Rye in the Vale of Pickering.

Corallian Limestone which outcrops on the hills surrounding the Vale of Pickering runs across the region, and this appears as an aquifer in Kirkdale swallowing most of the water from Hodge Beck, which reappears further downstream.

River Waveney

The ice sheet closed the natural drainage from the Vale of Pickering, the Humber and The Wash so that a lake of a complex shape formed in the Vale of Pickering, the Yorkshire Ouse valley, the lower Trent valley and the Fenland basin.


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