English churches - building stones

BGS Image ID: P209976

Drewsteignton village square, Devon. Looking east. Drewsteignton village is sited high on the northern edge of Dartmoor. Holy Trinity Church and Church House with its large chimney stack are both built of Dartmoor granite blocks. Drewsteignton village is typical of many on the the northern fringe of Dartmoor. The church tower is built of Dartmoor granite (imported to the district). The house to the right of the lych gate is built largely of rough hewn granite blocks. The wall to the left of the lych gate is built of blocks of impure limestone and hornfelsed mudstone from the local quarries (now disused). The granites of Devon and Cornwall and their associated intrusive and metamorphic rocks have commonly been worked in the past for building stone, both for local housing and for major building projects elswhere in the United Kingdom such as the many 19th century dock construction schemes in London.

BGS Image ID: P210728

Snettisham Church, Norfolk. Looking east. This large, late medieval church at Snettisham is typical of many in this area where a mixture of local building stones are used for the main walling material, chalk, flints and ferruginous carstone, with better quality oolitic freestones of the Lincolnshire Limestone Formation imported for more ornate mouldings and carved stonework. Built in the 14th century decorated style, Snettisham Church has its nave and tower constructed of partially dressed blocks of chalk and flint. The spire, pinnacles, copings, buttresses and window tracery are made of oolitic limestone, one of the Middle Jurassic freestones. The wall in the foreground is made of dressed Carstone blocks which have suffered some frost damage. While this area of Norfolk produced a wide variety of local building materials, including sandstones, limestones and flints, none were good enough to qualify as freestones. Consequently from medieval times onwards the oolitic limestones of Lincolnshire were commonly imported for the stonework in all the more prestigious buildings.

BGS Image ID: P210855

St Mary's Church, Purton, Wiltshire. Looking north-west. This Norman / Medieval church with its spire and crossing tower is constructed of Jurassic Coral Rag limestones. The term Rag refers to the coarse grained shelly (or ragged nature) of the limestone when fractured. The ragstone beds are generally very hard and durable stones but are consequently, therefore, very difficult to work, commonly they are used as undressed rubblestone blocks. This church at Purton is largely built of local 'Coral Rag' Limestone from the local Osmington Oolite Formation.The roof of the church is covered with stone slates which in this area are likely to be from the Forest Marble Formation, although some use of local Purbeck limestones is also known. The hard, pale grey, coarsely oolitic and shelly limestones of the Corallian Group were widely used in buildings along their outcrops in Dorset, Wiltshire and Oxfordshire.

Posted by Bob McIntosh

Mining subsidence in Ferniehill, Edinburgh, 2000

BGS Image ID: P100363

Ferniehill, Gilmerton, Edinburgh. Limestone mine subsidence event, November 9th 2000 to March 2001; 'Tumbledown Terrace'. The subsidence has caused damage to buildings, roads etc. The Carboniferous Gilmerton Limestone was quarried and mined at Ferniehill from time immemorial until about 1829. Collapsing old limestone mineworkings were responsible for what became catastrophic damage to many properties.

Download a leaflet explaining the subsidence, by Mike Bowne

BGS image ID:  P100365

BGS image ID: P100398

Posted by Bob McIntosh

Malmesbury Abbey, Wiltshire, Middle Jurassic limestone

BGS Image ID:P212039

Malmesbury Abbey, Malmesbury, Wiltshire. Looking north-east. 

Malmesbury Abbey was constructed in the 12th century of pale yellow, oolitic limestone from the Middle Jurassic limestones of the Bath area (Box Ground Stone). Only part of the Abbey now remains intact. The pale yellow oolitic limestones used in the Abbey have proved to be reasonably durable probably because the building is in a rural setting away from the problems caused by the industrial pollution of the last few centuries. A monastery was established on the site in around 676 but this building dated from the 12th century when the building was consecrated in 1180. The south portch is the most natable feature that survives from that period. At one time the abbey had a spire taller than salisbury Cathedral but it fell down some time before the Reformation when Henry VIII dissolved the monastery in 1539. Dissolution of the monastries in the 16th century lead to the stripping, sale and removal of building materials from many monastic buildings such as Malmesbury Abbey.
Date taken: 1977

BGS Image ID: P212040

One of the characteristic features of Norman ecclesiastical architecture is the high quality of the building materials selected and the outstanding workmanship of their masons. The remains of Malmsbury Abbey, now the parish church still preserve examples of this fine craftsmanship in stone. Considered to be one of the most outstanding examples of Norman decorative stone carving in Britain, this doorway in the south porch of the Abbey is carved from oolitic limestone from the Middle Jurassic, Box Ground Quarries near Bath. The limestones generically known as Bath Stones are one of the principal sources of building limestone in the United Kingdom. They were worked from numerous mines in the vicinity of the Bath which now sits upon several kilometres of old stone mine galleries. The limestones are pale to dark yellow in colour and dominantly oolitic though some shelly ragstone beds were also worked.

Posted by Bob McIntosh

Stone mason working on a capital, Bath & Portland Stone Firms Ltd.

BGS image No: P539472

Stone mason at work on a capital, Bath & Portland Stone Firms Ltd., West Wells Masonry Works, Corsham.  From the Hugh O'Neill Collection. Date: c. 1961.

Bob McIntosh

St Mary's Church, Purton, Wiltshire

BGS image ID: P210855

St Mary's Church, Purton, Wiltshire. Looking north-west. This Norman / Medieval church with its spire and crossing tower is constructed of Jurassic Coral Rag limestones. The term Rag refers to the coarse grained shelly (or ragged nature) of the limestone when fractured. The ragstone beds are generally very hard and durable stones but are consequently, therefore, very difficult to work, commonly they are used as undressed rubblestone blocks. This church at Purton is largely built of local 'Coral Rag' Limestone from the local Osmington Oolite Formation.The roof of the church is covered with stone slates which in this area are likely to be from the Forest Marble Formation, although some use of local Purbeck limestones is also known. The hard, pale grey, coarsely oolitic and shelly limestones of the Corallian Group were widely used in buildings along their outcrops in Dorset, Wiltshire and Oxfordshire.

Date taken: 1967

BGS old photograph No. A11054

Bob McIntosh

Stoop and room, Middleton Quarry and Mine, Gorebridge. Midlothian.

BGS image ID: P000178

Middleton Quarry and Mine, Gorebridge. Midlothian.

Stoop and room (pillar and stall) is an old method of mining where the material, in this case limestone is extracted leaving pillars of limestone in place to support the roof.

Interior view of the mine illustrating the method of extraction. A figure in the centre of the image illustrates the scale. Mining the North Greens (No. 2) Limestone. The thickness of the seam is 50 ft. though only the lower 20 ft. is in massive beds and suitable for mining. Chemical analysis shows it is 94.09% calcium carbonate and is of uniform high quality. The limestone was burnt in vertical, continuous mixed-feed kilns to produce lime for both agriculture and building purposes. Ground limestone was also produced. The rocks are of the Lower Limestone Group of the Carboniferous period. The quarry is now disused.

Date of image: 1945.

Bob McIntosh

Raising a block of Portland Stone from the Seacombe Quarry, Worth Maltravers, Dorset

BGS image ID: P023962

Raising a block of Portland Stone from the Seacombe Quarry, Worth Matravers, Dorset. The block, cut from the face of the quarry by the plug and feathers method weighs about 4.5 tons. One of the advantages that the Portland Stone quarries have over other producers is the large size of the limestone blocks that can be produced. The limestone quarries of Portland Bill have been in operation since Roman times. The characteristic white limestones which have proved to be extremely durable, even in the most polluted of urban environments, can be found in important buildings in all major cities and most large towns in the United Kingdom.

The Isle of Purbeck, though perhaps more famous as the source of the fossiliferous Purbeck Marble, is also a major producer of Portland Stone. The same succession of worked beds - Basebed, Whitbed and Roach - that outcrop in the Isle of Portland extends into the Purbeck area. Many of the quarries in the Isle of Purbeck were sited along the coastal cliffs and the stone was worked via an extensive series of underground galleries.

BGS Old photograph number A4985
Date of photograph: 1930.
Photographer: J. Rhodes

Bob McIntosh

St. Paul's Quarry, Isle of Portland, Dorset.

BGS image ID: P023964

St. Paul's Quarry, Isle of Portland, Dorset. Splitting a block with a technique called 'plug and feather'.

Stone has been worked on the Isle of Portland since ancient times for building and ornamental purposes. The commonly known Purbeck Marble is not a true marble but a polished fossiliferous limestone that contains the fossil shells of tiny water snails (the gastropod viviparus). The Purbeck rocks were deposited in the Jurassic and Cretaceous geological periods from about 155 to 45 million years ago. The quarrymen had their own terms for the various beds they came across. Rag stone, at the top was described as crumbly and very good; Grub, a fine bed able to produce fine paving stones and would take a polish; Roach, followed by Thornback would produce a 'blue hued stone'. At the base is the Freestone and above that the Whetson. The stone was both quarried and mined, both dangerous occupations. The limestone quarries of Portland Bill have been in operation since Roman times. The characteristic white limestones which have proved to be extremely durable, even in the most polluted of urban environments, can be found in important buildings in all major cities and most large towns in the United Kingdom.

Date of photograph: 1930. Photographer: Jack Rhodes. Original BGS photograph number: A4987.