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Action for the River Kennet

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About the River


Introduction
The Upper Reaches
Management of the River
Threats to the River
- Abstraction
- Pollution
- Climate Change
The Passing of a River
Recent Research

'Chalk streams are fed by groundwater. They rely on autumn and winter rainfall to recharge the aquifer and maintain flows through the year.' 'The water we use every day has to come from somewhere - using water carefully will reduce the stress on chalk stream environments.'

Contact: info@riverkennet.org

The winterbournes that feed the top of the river include: the main winter stream originating at Uffcott and running through Winterbourne Monkton; the smaller stream flowing at times from Highway Pennings via Yatesbury to join the larger one just west of Avebury; and the tiny stream starting at Beckhampton pond which runs (albeit rarely) along the A4 into the excavation moat around Silbury Hill.

The most common definition of the source, however, is near Silbury Hill. Just south of the A4, the river traditionally rose around New Year from the Swallowhead Springs, which emerge from a small wall of chalk at a corner of the meadow. This joins the stream flowing south from Avebury, past Silbury Hill and under the A4. The joined streams then turn east.

Half a mile downstream from the Swallowhead Spring, another spring feeds into the Kennet at times from the south end of Waden Hill. At West Kennet the remains were found of a large enclosure of upright tree trunks - a henge - that straddled the river in the early Bronze Age. Further downstream the ancient Ridgeway descends southwards and crosses the River Kennet at East Kennet.

River Kennet
River Kennet at Manton in Wiltshire
River Kennet when dry

Surface residue on River Kennet

Swindon in Wiltshire

Volunteer workers on the River Kennet