One of the Kennet's sources is Swallowhead Spring near Silbury Hill in Wiltshire, and others are springs north of Avebury near the small villages of Uffcott and Broad Hinton. These then converge. In these early stages it passes close by many prehistoric sites including Avebury Henge, West Kennet Long Barrow and Silbury Hill. The land drained by the headwaters normally has a deep water table (being in the North Wessex Downs which is mostly chalk as the upper subsoil), thus many stretches are winterbournes when and where precipitation is low and surrounding soils are not so dense with impermeables as to form a surface spring.