A general view of the east elevation |
Standing back in the very large churchyard of All Saints church, in Darfield, the east elevation appears as a vast expanse of Mexborough Rock, laid out in large and often wide ashlar blocks. This massive, cross-bedded medium grained sandstone is generally light brown in colour, with a variable content of oxides and hydroxides of iron, which can add a general orange colour in places, with concentrations in bands and Liesegang rings.
Also, like the variation of the Mexborough Rock known locally as “Rotherham Red” sandstone, it contains varying amounts of clay ironstone pebbles, which are often found concentrated in distinct beds - sometimes containing fossils of Carboniferous plants.
With various old quarries located a few hundred metres away to the east, on the other side of the River Dearne, the fabric of the church provides geologists with a good opportunity to study these various physical characteristics.
Looking more closely at the individual blocks of stone, very many have been blackened by the pollution from industry and coal fires. Others are covered in soluble white salts, which have evaporated from rising groundwater and, during continual phases of wetting and drying, have broken down the stone by forces generated by their recrystallisation.
When investigating mediaeval churches, I am always interested to see how changes in the patterns of masonry indicate various phases of construction, as seen in the tower of All Saints church, but the ashlar masonry of the east elevation is quite uniform.
As a geologist, I have developed a good eye for detecting variations in colour and texture of the stones that I encounter, but I am still learning from Pevsner, Historic England, church guides and other published sources, when it comes to the dating of the various architectural elements – all of which are generally not very methodical or comprehensive.
The three windows of the east elevation are quite different, with those of the chancel and north chapel being Perpendicular Gothic in style, with their emphasis on upright elements to the tracery and use of simple cusps, but that of the Lady Chapel – in a Decorated Gothic style with headstops - seems to be disproportionately large.
Further examination of the plinth courses and butted joints in the masonry, between the chancel and the chapels on either side, reveals that the north chapel is an obvious new addition and that the pre-existing south chapel has been partially rebuilt.
A general view from the south-east |
Thanks for the continuing story, as a local lad and Building Surveyor with an interest in traditional buildings this is fascinating, particularly the damp/salt effects on the face of the stone.
ReplyDeleteI am glad you found it to be of interest. I used to work in the building restoration industry in London, with specialist interests in matching stone (see my "Stone Matching" post in June 2014).
ReplyDeleteSmall world, I currently live in the South of England, did ten years in the same environment, who'd did you work for,
DeleteCliveden Conservation, IJP ?
I started off with Stonewest Ltd and then formed Triton Building Restoration Ltd. with my brother.
DeleteExtremely Small world, I used work for RHPS based at Windsor, remember seeing Stonewest on tender lists
DeleteHi Scott! Really enjoying your blog. Any advice, resources or groups you would recommend for someone just getting started with an interest in Geology? I also live in Rotherham.
ReplyDeleteThanks and I am glad that it interests you. As for learning about geology, Geospupplies Ltd in Chapeltown run paid courses but not much is happening in Rotherham, although the Sheffield Area Geology Trust (SAGT) occasionally have events for the public - https://www.sagt.org.uk/
Delete