
Aggregates of Herefordshire
Herefordshire has a rich history of geological time stretching 500 million years or more.
Herefordshire has a rich history of geological time stretching 500 million years or more.
Geological Time
Geological time is divided into eons, eras, periods, epochs and ages, with eons representing the largest stretches of time (500 million years or more). Each eon is subdivided into eras, which in turn are divided into periods etc… This nomenclature ends with ‘ages’, which represent the smallest increments of geological time, on the order of a few hundred thousand years.
Rocks of similar age can grouped together and placed into a geological succession, where they lie in between rock units of greater and lesser age. As geology varies across distances, these geological successions are only relevant to a specific geographical area. Geologists can get some idea of what processes were taking place in Herefordshire over millions of years, by looking at what types of rocks were forming at different times in the geological succession. The most useful subdivisions of geological time are periods, epochs and ages, as rocks dated to these resolutions can give both general and detailed information on the ancient environment.
In this geological succession, periods and epochs are used to describe the older geological succession (Precambrian – Jurassic) that is seen in Herefordshire. The most recent geological period (the Quaternary) is described in terms of period and age, as the detail preserved within these young rocks and sediments allows for more detailed interpretation.
Period |
Epoch |
Stratigraphic Unit |
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Quaternary |
Holocene |
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Devensian |
Herefordshire Formation |
Cradley Valley Formation |
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Ham Green Member |
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First Terrace |
First Terrace |
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Ipswichian |
Second Terrace |
Second Terrace |
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Wolstonian |
Third Terrace |
Third Terrace |
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Fourth Terrace |
Fourth Terrace |
Colwall Member |
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Hoxian |
Cradley Silt Member |
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Anglian |
Starpit Formation |
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Humber Formation |
Mathon Formation |
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TIME GAP |
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Period |
Epoch |
Stratigraphic Unit |
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Permian |
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Warwickshire Group |
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Carboniferous |
Westphalian |
Trenchard Formation |
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Pennine Coal Measures Group |
Upper Coal Measures |
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Middle Coal Measures |
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Lower Coal Measures |
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Cornbrook Sandstone Formation |
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Carboniferous Limestone Supergroup |
Pembroke Limestone Group |
Cromhall Sandstone Formation |
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Llanelly Formation |
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Devonian |
Upper Old Red Sandstone |
Tintern Sandstone Formation |
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Quartz Conglomerate Formation |
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Lower Old Red Sandstone |
Breconian Group |
Brownstones Formation |
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Sandy Haven Formation |
Townsend Tuffs Beds |
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Silurian |
Pridoli |
Downton Group |
Raglan Mudstone Formation/ Bishop’s Frome Limestone |
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Ledbury Formation |
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Temeside Mudstone Formation |
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Downton Castle Sandstone Formation |
Ludlow Bone Bed |
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Ludlow |
Cefn Einion Formation |
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Knucklas Castle Formation |
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Bailey Hill Formation |
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Bringewood Formation |
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Wenlock |
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Coalbrookdale Formation |
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Llandovery |
Haugh Wood Formation |
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Ordovician |
Tremadoc |
Habberley Shale Formation |
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Shineton Shale Formation |
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Bronsil Shale Formation |
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Cambrian |
Merioneth |
White-Leaved Oak Shale Formation |
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Precambrian |
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Reproduced with the permission of the British Geological Survey © NERC. All Rights Reserved. Based upon information in the BGS Lexicon and the BGS memoir ‘Geology of the country between Hereford and Leominster, 1:50,000 scale sheet 198‘, with the permission of the British Geological Survey
Geological time is divided into eons, eras, periods, epochs and ages, with eons representing the largest stretches of time (500 million years or more).
Geological time is divided into eons, eras, periods, epochs and ages, with eons representing the largest stretches of time (500 million years or more).