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Essex Field Club
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EFC Centre at Wat Tyler Country ParkWe are closed due to the Covid-19 situation, but we are otherwise normally open to the public at our centre at Wat Tyler Country Park every Saturday, Sunday and bank holiday 11am-4pm, check. We are also normally open on Wednesdays 10am-4pm.

Geology Site Account

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Fultons Farmhouse Boulder, BICKNACRE, Chelmsford District, TL788006, Potential Local Geological Site

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Site category: Boulders - other types

Site name: Fultons Farmhouse Boulder

Grid reference: TL 788 006

Brief description of site:

On private land, next to the garage of Fultons Farmhouse, is a splendid boulder of basalt 90 centimetres (3 feet) long. Large erratic boulders of basalt are very rare in Essex.

The actual size of the boulder is 90cm x 60cm x 35cm. This boulder was probably transported from Scotland by the Anglian ice sheet about 450,000 years ago. Bicknacre is close to the southern limit of the ice sheet.



Stones such as this boulder are known as glacial erratics and were carried to Essex by the Anglian Ice Sheet that covered almost the whole of Britain during the coldest period of the Ice Age, some 450,000 years ago. At this time Essex was situated at the southern edge of the ice sheet, which was up to 2 kilometres (over a mile) thick in places. Its extent is fairly well known because it has left behind evidence of its existence in the form of a rock called boulder clay, or till. A great thickness of Boulder clay exists across north and central Essex except in river valleys where it has been removed by erosion.

As the ice moved it ground up and carried along pieces of the rocks over which it passed, just as glaciers and ice sheets do today, and when the ice melted an unsorted clayey residue called boulder clay, or till, was left behind. Boulder clay contains rocks transported long distances by the ice and known as glacial erratics. By matching rock types with known outcrops in other parts of Britain geologists are able to establish the direction of ice movement across the country from its origins in Scotland or Scandinavia.


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Reference: Lucy 2003a

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