Jump to content

Chicksgrove Quarry: Difference between revisions

Coordinates: 51°03′57″N 2°03′20″W / 51.06572°N 2.05561°W / 51.06572; -2.05561
From Wikipedia, the free encyclopedia
Content deleted Content added
m External links: Rem stub tags (class = non-stub & non-list) using AWB
Rescuing 1 sources and tagging 0 as dead. #IABot (v1.2.7.1)
Line 18: Line 18:
==External links==
==External links==
* [http://www.chicksgrovequarry.co.uk Chicksgrove Quarry Ltd - Operators website]
* [http://www.chicksgrovequarry.co.uk Chicksgrove Quarry Ltd - Operators website]
* [http://www.english-nature.org.uk English Nature website] (SSSI information)
* [https://web.archive.org/web/20060813070641/http://www.english-nature.org.uk:80/ English Nature website] (SSSI information)


{{SSSIs Wilts geological}}
{{SSSIs Wilts geological}}

Revision as of 22:29, 21 November 2016

Chicksgrove Quarry (grid reference ST962296) is a 14 acres (5.7 ha) geological Site of Special Scientific Interest in Wiltshire, England notified in 1971.

Chilmark stone, a form of limestone, is quarried at the site.

Chicksgrove Quarry Ltd also operates Chilmark Mine, a site 1.5 miles away. See Chilmark Quarries

Chilmark Stone

Chilmark stone is a fine quality building stone used extensively for construction and restoration projects throughout the South of England and nationally as a match for other stones such as Reigate Stone, Malmstone and Kentish Rag. Thousands of tonnes of Chilmark Stone from Chicksgrove Quarry have been used in the restoration of Salisbury Cathedral. Recent restoration uses for the stone include Westminster Abbey Chapter House and Hampton Court Palace.

Geological Interest

The geology exposed by the present and historical workings at Chicksgrove Quarry contribute heavily towards its classification as SSSI and access to the former quarry faces for future generations features in the quarry’s restoration plans.

The Chilmark Stone at Chicksgrove Quarry dates from the latter part of the Jurassic period so is around 145 million years old, the stone is from the upper part of the Portland Stone Formation and the very lower beds of the Purbeck Limestone Group.

51°03′57″N 2°03′20″W / 51.06572°N 2.05561°W / 51.06572; -2.05561