Upper Hall Farm Quarry and Grasslands

Much Wenlock Limestone, Elton Formation (Lower Ludlow Shales)

Upper Hall Farm Quarry and Grassland

Exposed Units: Much Wenlock Limestone, Elton Formation (Lower Ludlow Shales)

Conservation status: Site of Special Scientific Interest

Upper Hall Farm Quarry and Grasslands is a complex of quarries, woodland scrub and grassland on the slopes of the Silurian Limestone Hill to the west of the Malvern Hills. The locality shows the best exposure of the junction of the Wenlock and Ludlow series outside the Ludlow area. At this locality, the calcareous siltstones of the Lower Elton Formation rest conformably on the Much Wenlock Limestone Formation. This is the only locality in the Malvern Hills where the relationship between the representatives of two major divisions of the Silurian system can be studied and is thus significant in understanding the stratigraphy, structure and geological history of the area.

This quarry was opened in the upper part of the Much Wenlock Limestone Formation and the lower part of the Lower Elton Beds. The Much Wenlock Limestone consists of a 65-150m sequence of interbedded calcareous mudstones and nodular limestones. The latter form the bulk of the unit and vary from thinly bedded, argillacous limestones to massive limestones. Shale interbeds are common, where they generally appear somewhat squeezed and are frequently seen wrapping around lenses of limestone. An extensive fossil assemblage is present in the Much Wenlock Limestone at this locality and includes brachiopods, bryozoans (moss animals), stromatoporids (reef-forming organisms), corals, algae, trilobites and crinoids.

The Elton Formation is a medium grey, calcareous shaley mudstone with bands of nodular limestone common towards the base of the unit. Fossil assemblages in the unit are exceptionally preserved, but are not as diverse as the assemblages in the underlying Much Wenlock Limestone. The fossil assemblage is dominated by brachiopods but small solitary corals are also important, as are several species of ostracod, which are a type of microfauna belonging to the crustacean family.


Argillacous – Containing clay minerals


General view of horizontally bedded Much Wenlock Limestone at Upper Halll Farm Quarry.

General view of nodular limestones of the Much Wenlock Limestone Formation

View of the quarry face exposing the Much Wenlock Limestone and overlying Lower Ludlow Shales.


Anon, 1991, ‘SSSI notifications [OS 1:50000 sheet 149]’, In Anon (eds), Statutory sites under the National Parks and Access to the Countryside Act 1949 and the Wildlife and Countryside Act 1981, English Nature, Peterborough.

Penn, J.S.W., and French, J., (1971), The Malvern Hills, Geologists’ Association Guides; Geologists’ Association.

March 2011

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