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Ironstone quarrying in the Vale


The ironstone ridge near Hose.


The prominent ridge which defines the southern boundary of the Vale of Belvoir, and on which the eponymous castle is sited, was created because a layer of ironstone about six to eight feet thick sits on top of softer marlstone deposits. Over millennia the marlstone has eroded away while the ironstone resists erosion creating the geomorphology of the escarpment.


The crossing of two footpaths to the north of Goadby Marwood probably marks the centre of a Roman small town producing iron. However all archaeological evidence was quarried away in the 1950s.


There was Iron Age and Roman quarrying and smelting just to the south of the ridge close to the modern village of Goadby Marwood. Two footpaths cross in a field where the centre of the Roman town probably was. The east-west one is a former Roman road still known as the Salters Way.

So when – and why – did we get back into quarrying this resource? Well it happened more by accident than design. The Midland Railway had the bright idea that the people of Melton Mowbray might want to travel to Nottingham. In 1871 they commissioned a surveyor to work out the best route. The route they actually used is now known as the Old Dalby test track. But one of the routes being considered was to the east and went via Holwell. The surveyor noted the ironstone deposits. And made a business deal with the landowner to open up a quarry. Ore was first extraced at Holwell in 1875, first taking it almost off the cliff-side and then by quarrying, before later mining it. But mining is never a cheap option so extraction ceased in 1943.


The approximate extent of ironstone extraction in Leicestershire, Rutland and south-west Lincolnshire (after Tonks 1992). Not all the quarries were operating at the same time. The red dot indicates the location of the Holwell Works.


From the 1880s onwards ironstone extraction took place over a substantial part of north-east Leicestershire and into adjoining parts of Lincolnshire. For about two-thirds of the Salters Way running along the ironstone ridge from near Holwell to Belvoir Castle the road was hemmed in by successive quarries. Other large quarries were further away at Sproxton, Tilton on the Hill and in north Rutland.

A whole network of standard gauge railway lines were built to take the ore to smelters at Scunthorpe, Rotherham, Corby and more locally to the Holwell Works at Asfordby Hill near Melton Mowbray.


from railmaponline.com


This gives you an idea of what fields looked like during quarrying. The top soil is shovelled to one side to allow access the ironstone. Eventually it will be levelled off to allow farming to resume.


But now the only evidence of where the quarries once were is fields that are roughly six feet below the level of the road. After the working ceased the soil was just put back and levelled off. But clearly a few feet lower than it had been before the quarrying.


As well as the ironstone being used for making iron it was also used locally as building stone. Very attractive the buildings usually are. But the ironstone tends to weather badly so needs repairing after a few hundred years.


In 1974 the blast furnaces at Scunthorpe started using higher iron-content ores from Scandinavia and cancelled contracts with the quarries still operating. Where was the last quarry operating? It was just inside Lincolnshire at Woolsthorpe but known as Denton Park Quarry.


The last day of operations at Denton Park Quarry, Woolsthorpe, on 14th February 1974. The locomotive is now preserved at Rocks by Rail museum, Cottesmore. (From Tonks 1992.)


Lots more information and maps about the ironstone quarries of Leicestershire in this YouTube video.

Main source

Eric Tonks, 1992, The Ironstone Quarries of the Midlands: History, operation and railways Part IX Leicestershire, Runpast Publishing.


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