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Wicken Water Boulders, ARKESDEN, Uttlesford District, TL48203449, Potential Local Geological Site
Site name: Wicken Water Boulders.
Grid reference: TL 4820 3449
Brief description of site:
A large number of large erratic boulders situated in the bed of the stream (Wicken Water) by the road bridge in the centre of Arkesden village. The stream bed is usually dry, and thus the stones are safe to visit provided care is taken when traversing the stream bed.
A large concentration of boulders can be seen in the bed of the Wicken Water, a stream running through Arkesden village. They are by the road bridge (near the village hall) and consist of boulders of Hertfordshire puddingstone and sarsen stones. There are at least 12 boulders here, of varying sizes and shapes, the largest boulder being a slab of colourful puddingstone 1.5 metres by 1.1 metres in size. Most of the stones are obscured by silt from the stream or covered in moss. One rounded boulder of puddingstone has been cleaned to reveal its colour and texture. A sarsen stone is present at each end of the bridge itself.
Hertfordshire puddingstone it contains well-rounded flint pebbles bound together with quartz ‘cement’, making it a very tough rock. Sarsen stones are boulders of extremely hard sandstone. They are distinctly different rocks but were both formed under the same conditions around 55 million years ago when the climate of Britain was very hot. Both rocks are very resistant to erosion. The formation of silcretes (which include puddingstone and sarsens) has been the subject of recent scientific debate. Research has compared the conditions under which puddingstones and sarsens were formed with the present day climate in the Kalahari Desert and parts of Australia.
Arkesden is unique in Essex for the number of erratic boulders that are scattered around the village. They can also be seen on the roadside, by the inn, and in private gardens.
The boulders of puddingstone that are found in Essex most probably originated in Hertfordshire and were brought to Essex by the Thames when it flowed far to the north of its present course. Sarsens are thought to have been brought into Essex from the chalk hills to the north by ice. However, the large number of stones in the stream bed here raises the intriguing possibility that there might have once been a more local source (Lucy 2015). Such boulders are usually concentrated in river valleys as they have slowly moved downhill under gravity during the ice age. These boulders may therefore even be “in situ” erratics and not moved by man. Support for this theory is the existence of a circular hole in a large sarsen stone in the stream bed which, it has been suggested, may be a pothole formed when the river through this valley was a torrent of meltwater each year during the brief Summers of the coldest parts of the Ice Age.
The boulders are situated beneath the road bridge, which was opened in 1911, and are found at the apex of a hairpin bend in the stream. It is not known whether this location is significant. A.E. Salter, in his 1914 paper, refers to the stones in the stream bed here.
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Reference: Salter 1914, Lucy 2015.
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