The Caterham Bourne and rising groundwater
The Caterham Bourne is a chalk stream that stays dry most years. After a very wet winter the groundwater rises and it flows down the valley through Whyteleafe and Kenley, as it did in early 2014 when roads and homes along the valley flooded.
When the water table is that high, basements and pump chambers on the valley floor can take in groundwater and run far more often than usual. A pump that is already worn may not keep up. Having the station serviced in autumn, before the wet months, is a sensible precaution for homes near the bottom of the valley.
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