Whitman’s Hill Quarry
Much Wenlock Limestone, Coalbrookdale Formation
Exposed Units: Much Wenlock Limestone Formation, Coalbrookdale Formation
Conservation Status: Local Geological Site
Whitman’s Hill Quarry is located within a complex of faulted Silurian rocks just north of the Malvern Hills.
There are two rock formations present in the quarry: 12m of the Coalbrookdale Formation which forms the basal units, and 25m of the Much Wenlock Limestone Formation which sits above. The boundary between the two units represents a rapid decrease in sea levels in the area
The Coalbrookdale is characterised by olive grey to dark blue-grey silty mudstones with some calcareous siltstones and contain calcareous nodules and impersistent nodular calcareous beds. These beds are highly fossiliferous and contain a wide range of marine fauna, including brachiopods, trilobites, corals, calcareous algae, bivalves, orthocone nautiloids, crinoids and bryozoa. IN the eastern rock face at the bottom of the quarry are examples of spheroidal (‘onion skin’) weathering in the siltstones of the Coalbrookdale Formation. This weathering process has a produced ball-like structures ranging in size from 100mm to just over 2m.
The overlying Much Wenlock Formation is characterised by pale grey nodular to thinly bedded limestones. Some of the more nodular beds are known locally as the ‘Storridge Porridge’. The Much Wenlock Formation also contains small reef structures known as bioherms and one of these structures is found in the centre of the northern rock face
Within these two formations nine bentonite layers can be identified. These 2-3cm layers of fine clay are volcanic ash layers, formed when a volcano erupts and the ash is deposited on the surface of the sea. The ash sinks through the water column, killing much of the sea life. These soft bentonite layers are easily identified within the rock face as they have weathered preferentially in comparison to the harder limestones. Radiometric dating of uranium and lead in the bentonites yielded ages of around 425 million years for the deposition of these ash layers and demonstrates that the Coalbrookdale and Much Wenlock Formations were deposited around this time.
The nodular Much Wenlock Limestone (425 million years) was primarily quarried for aggregates and for the use in Lime Kilns. Eventually the underlying silty Coalbrookdale Formation (427 million years) was reached and quarry operations ceased, as the Coalbrookdale Formation is not a good aggregate material.
Fault: A line of weakness within the Earth’s crust along which movement and displacement occurs
Much Wenlock Limestone Formation overlying the Coalbrookdale Formation (Facing SE).
Bioherm (reef mass) in Much Wenlock Limestone Formation on east face of the quarry.
Ball of spheroidal weathering (Onion-skin) in Colbrookdale Formation unit.
Quarrying at Whitman’s Hill during Summer 1977
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