Blisworth Limestone Formation relationship to the Jurassic ridge, to the west of Peterborough. (BGS sheet 157) Around Towcester it reaches a thickness of 9m. (Hains & Horton p. 85) Blisworth limestone is used as a building material, in particular as blocks of stone. Lilford Hall in Northamptonshire is made from Blisworth limestone. Blisworth Limestone Formation The Blisworth Limestone Formation is a geological formation primarily consisting of limestone deposited during the Bathonian stage of the Middle Jurassic, found in the Jurassic ridge which extends north and south through England. It was laid down in the shallows of the Jurassic sea and is part of
Blisworth and Birmingham Railway, under the surveying and construction control of Robert Stephenson, bypassed Northampton and opened a station in Blisworth in 1839. In 1842, after much discussion, Lord Grafton agreed to fund a new station as long as it was a "first class" station - i.e., all trains stopped at it. Ford Lane became Station Road, the location of Blisworth station. In 1845 a branch line on to Peterborough was completed via Northampton, and in 1866 a single-track line was built to Banbury. Blisworth station closed in January 1960 and both branch lines have also long since gone. The main