Marl
Naturally occurring alluvial clay containing a relatively large amount of calcium carbonate, used to counteract acidic soils and stabilise reclaimed mosslands.
The most common type of cave, formed by the solution of carboniferous rocks by the action of rainwater.
Now deprecated term for multiple layers of mudstone and siltstone that occur beneath parts of the English Midlands and beyond.
Grade II listed structure in Stretford, Greater Manchester, probably the base of an Anglo-Saxon cross shaft.
Sandstones interbedded with mudstones and siltstones in the Lower Coal Measures of West Yorkshire, once extensively quarried.
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| Marl | |
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| Naturally occurring alluvial clay containing a relatively large amount of calcium carbonate, used to counteract acidic soils and stabilise reclaimed mosslands. | |
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