Classifier Instance:

Anchor text: Fetcham
Target Entity: Fetcham
Preceding Context: Not all of the water removed from the river by the swallow holes, is returned to the channel at Leatherhead. The chalk aquifer also feeds the springs at the southern end of
Succeeding Context: Mill Pond, which have never been known to run dry. A survey carried out in March 1883, estimated that the Fetcham springs were producing approximately 3.6 million gallons of water every day. A second survey performed in 1948, estimated that the same springs were yielding approximately five million gallons of water a day. The water table in the chalk of the Wey Gap is significantly higher than might be expected from natural rainwater percolation alone. It has been suggested that a proportion of the excess water originates from the Mole Gap.
Paragraph Title: null
Source Page: River Mole

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