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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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Newport Grammar School Borehole (site of), NEWPORT, Uttlesford District, TL51993439, Historical site only

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Site category: Borehole or well

Site name: Newport Grammar School Borehole (site of)

Grid reference: TL 5199 3439

Brief description of site:

Site of borehole that in 1887 revealed the existence of the Cam-Stort buried "tunnel' valley.



This borehole at Newport is one of several that have revealed the presence of a remarkable buried valley in north-east Essex. This steep-sided valley is cut into the Chalk beneath the town and is completely filled with glacial gravel and sand with no sign of it on the surface. It was carved by gravel-laden meltwater under tremendous pressure beneath an ice sheet.

The borehole was sunk in 1887 at Newport Grammar School (now Joyce Frankland Academy) in Burywater Lane. It failed to reach the chalk bedrock at the remarkable depth of 104 metres (340 feet) and was abandoned when sand rose up the bore and prevented the tube being driven further. Just a short distance away the chalk bedrock is close to the surface indicating that the valley has steep sides. The surface of the ground at this point is 205 feet above present sea level which means that the valley bottom is at least 135 feet below sea level.

Tunnel Valleys

In parts of East Anglia boreholes have revealed deep, steep-sided valleys cut into the chalk bedrock and now completely filled with glacial sand and gravel and often hidden by a covering of boulder clay. Known as buried valleys or tunnel valleys these remarkable natural features were formed beneath the Anglian ice sheet when it covered north Essex 450,000 years ago and were the main drainage routes for meltwater. To carve such deep channels the gravel-laden water must have been under tremendous pressure (due to the weight of the ice above) and the irregular surface of the channel floors indicate that in some places the water was even forced uphill.

In Essex the best example of a buried valley is the Cam-Stort Buried Valley which is present from north of the border with Cambridgesire south as far as Bishops Stortford and at Newport it is over 100 metres (300 feet) deep. It was first recognised by William Whitaker in his paper ‘On a deep channel of drift in the valley of the Cam, Essex’ which was published in 1890 in the Essex Naturalist.

The deepest buried valley, however, is beneath the Stour valley on the northern border of Essex. In the vicinity of Cavendish the base of this valley is well below sea level at the remarkable depth of 143 metres (470 feet).


Cam-Stort buried valley at Newport (from Lake and Wilson 1990)
Cam-Stort buried valley at Newport (from Lake and Wilson 1990)

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Reference: Whitaker 1890, Whitaker and Thresh 1916 (p. 230), Lake and Wilson 1990 (p. 28-31)

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