The geology of Wales |
A view west towards Sheffield |
This outcrop forms part of a cyclical succession of thin sandstones and shales, with once important seams of coal, that lies between the Mansfield Marine Band and the Mexborough Rock, and which form scarp-and-vale topography that gives most of Rotherham its character.
A view of the Rotherham Red sandstone to the north |
Getting off the bus on the outskirts of the village, on a bright and sunny day, views of the Millstone Grit moors on the edge of the Peak District National Park - which rise to the west of Sheffield - can be clearly seen.
Walking towards the centre of the old village of Wales, the first building stones that can be seen are from the Magnesian Limestone - to build a school and for the dressings of a Methodist church and a couple of houses of similar age. One house, dated 1987, uses both Rotherham Red sandstone and another indeterminate Carboniferous sandstone but, arriving at the centre of the old village, a handful of old agricultural buildings are again built of Magnesian Limestone.
A quick exploration of the historic buildings in the immediate area reveals that both Magnesian Limestone and Rotherham Red sandstone have been used extensively, in combination with the local sandstone that was presumably once quarried in the vicinity of Old Quarry Avenue, which now forms part of a modern housing estate.
An old agricultural building constructed in limestone and sandstone |
Once I had taken a good look at the war memorial, I continued with my principal objective of the day – to investigate the construction history of the church of St. John the Baptist.
Wales War Memorial |
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