Gypsey (spring)

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A gypsey is a name given to intermittent springs and streams in the Yorkshire Wolds, England. Gypseys are streams formed from springs from the waterladen chalk that constitutes the Yorkshire Wolds. The springs flow in late winter or early spring, with the water emanating through unbroken turf. [1]

In Wiltshire and Dorset the same phenonoma is known as winterbournes , in Kent known as nailbournes , and as lavants in Hampshire. [2]

See also

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Gypsey Race

The Gypsey Race is a winterbourne stream that rises to the east of Wharram-le-Street and flows through the villages of Duggleby, Kirby Grindalythe, West Lutton, East Lutton, Helperthorpe, Weaverthorpe, Butterwick, Foxholes, Wold Newton, Burton Fleming, Rudston and Boynton. The stream flows into the North Sea in Bridlington harbour. It is the most northerly of the Yorkshire chalk streams.

References

  1. Thomas Allen (1831), "12. Survey of Dickering Wapentake", A new and complete history of the county of York, 4, I.T. Hinton, p. 96
  2. Paul F. Greenfield; Greg Oliver, eds. (2001), Riversymposium 2000: sustaining rivers - defining the new international agenda : selected proceedings of the 3rd International Riversymposium (Brisbane, Australia, 6-8 September 2000), 43, IWA, p. 20