Go with the flow – get involved with CrowdWater!
Help us track chalk stream flow regimes Chalk streams have unique hydrogeology – they are fed from springs bubbling up from the chalk aquifers. This means as groundwater levels fall, they can dry up, with many chalk streams having ‘winterbourne’ sections which dry up as part of a natural cycle. However, flow regimes have been altered in many ways including climate change, over-abstraction and physical modification. In...