St Dunstan's Well Catchment

Coordinates: 51°13′33″N 2°28′36″W / 51.2257°N 2.4768°W / 51.2257; -2.4768
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St. Dunstan's Well Catchment
Notification
1967 (1967)
Natural England website

St. Dunstan's Well Catchment (

notified
in 1967. It is of both geological and biological significance.

Formerly known as Stoke St Michael Slocker, it contains nine SSSI units consisting of rock and calcareous grassland.[1]

Geological

St Dunstan's Well Catchment is an important and well-known cave system which includes a series of spectacularly-decorated caves which in total extend to about 4 miles (6.4 km) of mapped passage. The caves at Fairy Cave Quarry were formed mainly by the erosive action of water flowing beneath the water-table at considerable pressure (so called '

stalactites and calcite curtains) which in their extent and preservation are amongst the best in Britain. Shatter Cave and Withyhill Cave
are generally considered to be amongst the finest decorated caves in Britain in terms of their sheer abundance of pure white and translucent calcite deposits.

Biological

An area of nationally rare species-rich unimproved calcareous grassland of the Sheep's-fescue-Meadow Oat-grass type occurs in the field to the east of Stoke Lane Quarry. Small numbers of greater horseshoe bat (Rhinolophus ferrumequinum), lesser horseshoe bat (Rhinolophus hipposideros) and Natterer's bat (Myotis nattereri) hibernate in the cave system.[2]

References

  1. ^ "SSSI units for St. Dunstan's Well Catchment". Natural England. Retrieved 12 January 2014.
  2. ^ "St. Dunstan's Well Catchment" (PDF). English Nature. Retrieved 20 July 2006.