Geology
Kent is an eroded dome or anticline, between the chalk of the North and South downs. the Kentish Weald, which is visible where top of the dome has been eroded, is made up of sandstone and clay. The vineyard lies on the Hastings beds, a series of clay and sand deposits in the Lower Cretaceous of southeast England. The excellent drainage means that the vines have to put down deep and stable roots, and do not get soggy feet.