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The following sites have been selected to represent the different aspects of geology and landscape in the district. Not all sites have something to see; many are solely of historical interest as a record of an important or interesting discovery.

Some sites are not strictly geological but have a geological connection. Geological sites are therefore defined in their widest sense and include, for example, buildings, walls, wells, spas, springs, graves, boreholes, plaques, landslips and viewpoints.

This is not a complete list of geological sites in the district. Others will be added and descriptions expanded as further research is carried out.

Note:
Not all of the sites here described are accessible. Some sites are on private land and can only be viewed from footpaths that pass through or alongside the site. Inclusion of a site on this list does not, therefore, imply any right of access. Please remember not to trespass on private land.

Erratic boulders beside the lake in Hatfield Forest.
Photo G.Lucy


Sites of Special Scientific Interest (SSSIs)

UGLEY. Hall's Quarry SSSI (also known as Ugley Park Quarry) (TL 519 280)
The complex sequence of sands, gravels and boulder clay at this quarry is important for showing that, during the Anglian cold stage (450,000 years ago), the Thames catchment was repeatedly invaded by ice. The evidence from Ugley is critical in demonstrating that there were at least four of these ice advances, each one depositing a characteristic boulder clay. The quarry is still active but is partly infilled. Two representative sections were intended to be maintained in the northern part of the pit. There are several fine sarsen stones by the road at the entrance to the quarry. Private land. Permission to visit is required from the quarry owners.

Local Geological Sites (LoGS)


SAFFRON WALDEN. The Gibson Boulders (Local Geological Site) (TL 5369 3817)
At the junction of Gibson Gardens and Margaret Way is a mound of grass and trees containing at least 25 glacial erratic boulders of varying sizes. At least 10 different rock types are represented. The largest is a slab of colourful puddingstone 1.2 metres (4 feet) long. The site also has great historic interest. The Gibson Gardens estate was built on land which was formerly the gardens owned by George Stacey Gibson (1818-1883), naturalist, who had a great interest in geology. An 1877 map shows this mound to be the site of his summer house and it seems certain that he accumulated these boulders in his garden. They were almost certainly gathered from the farmland that he owned in the vicinity.

Other sites

ARKESDEN. Arkesden War Memorial (TL 4821 3456)

The war memorial in St. Mary's churchyard consists of a very large, single boulder of puddingstone 1.7 x 1.7 x 0.8 metres in size (5'6" x 5'6" x 2'8"). It is not known where this was obtained but it is a fine and unusual use for an erratic boulder.

ARKESDEN. Clatterbury Lane Puddingstone (TL 4834 3422)
Almost hidden in vegetation at the side of Clatterbury Lane to the south of the village is a very large and colourful boulder of Hertfordshire puddingstone (200x130x100cm in size). It is close to the road and access is difficult.

ARKESDEN. Wicken Water Boulders (TL 4821 3449)

A large concentration of glacial erratic boulders can be seen in the bed of the Wicken Water, which is the stream running through the village. The boulders are on the west side of the road bridge near the village hall. There are at least 12 stones here, one about 1.5 by 1.1 metres in size (5 feet by 4 feet), and they are of two types - puddingstones and sarsens. The stones are safe to visit provided care is taken when traversing the stream bed. The stream bed is usually dry. These boulders may actually be 'in-situ' erratics. They are situated at the apex of a hairpin bend in the river but it is not known whether this is significant.

ASHDON. Ashdon Meteorite (site of fall) (TL 581 409)
The Ashdon meteorite that fell in 1923 is the only meteorite to have been found in Essex. The fall was witnessed by a farm worker in broad daylight on Ashdon Hall Farm and subsequently dug up from a depth of two feet. The site of the fall is therefore historically important although there is nothing to see at the site. It is hoped that a plaque commemorating the event could be erected in the future. In England in the last 100 years only three other meteorites were seen to fall and were subsequently recovered. The meteorite is now in the meteorite collection at the Natural History Museum, London and is still available for study. A cast of the meteorite can be seen in Saffron Walden Museum. Ashdon Museum also has a cast with a small display on the fall.

ASHDON. Ashdon Parish Church

Erratic cobbles can be seen in the fabric of the church. Geologist Sir John Smith Flett (1869-1947) is buried in the churchyard. His grey granite tombstone is in the shadow of All Saints' church tower with the following epitaph "He richly enlarged man's knowledge of the earth".

AUDLEY END. Audley End House Septarian nodule (TL 5217 3831)
On display in the Stable Block is a fine, large septarian nodule (165x115x30cm in size) cut in half to display the internal calcite-lined cracks or 'septa'. This nodule was no doubt collected locally and was part of the natural history collection acquired by the fourth Lord Braybrooke in the 19th century. It was moved from its previous position on the Tea House Bridge in 2003 to deter vandalism.

AUDLEY END. Audley End Sarsen Stone (TL 5234 3800)
Fine sarsen stone by the road opposite the entrance to Audley End House (110x90x50cm in size).

CATMERE END. Catmere End Sarsen Stone (TL 497 388)
A very large sarsen stone 2.1 metres long sits in the long grass by the signpost at the crossroads.

CLAVERING. Clavering Swallow Hole (TL 4764 3175)
A swallow hole is a depression in the ground in a limestone or chalk area into which a stream disappears underground. This example currently takes the form of a two metre wide solution hole in the chalk bedrock of the river. It is the route by which water flows into the chalk aquifer. Discovered by the Environment Agency. It is choked with debris and usually not visible due to the growth of vegetation. Access to the stream bed is hazardous. View from the road only.

DUDDENHOE END. Coopers End Farm Puddingstone (TL 4649 3596)
Large Hertfordshire puddingstone (160x140x55cm in size) by the entrance to a plant hire company at Coopers End Farm. The boulder is unusual as the base is free of pebbles and therefore takes on the appearance of a sarsen stone.

GREAT CHESTERFORD. Great Chesterford C of E Primary School (TL 5072 4282)
The main school building, built in 1849, consists of knapped flints, with limestone dressings on a gault brick plinth. A very fine example of flint architecture.

GREAT DUNMOW. Flitch Way Ballast Pit and Tufa Springs (TL 6195 2160)
An old overgrown railway ballast pit adjacent to the railway cutting, which is now the route of the Flitch way footpath. The adjacent cutting provides limited exposures of Kesgrave Sands and Gravels overlain, or butting up against, Anglian till. Also of particular interest are hard-water 'petrifying' springs, which are the source of crystal-clear streams that run in the cutting, depositing calcium carbonate 'tufa' and encrusting all the objects in the steam bed including leaves and twigs.

HATFIELD FOREST. Hatfield Forest Boulders (TL 541 198)
On the southern edge of the lake were three partially-submerged and largely innaccessible boulders, two of Hertfordshire puddingstone (the largest 135x90x70cm in size) and one of sandstone (140x110x70cm in size). They were discovered when the lake was created in about 1750. Adjacent to the Shell House a boulder of limestone(?) (80x45) protrudes from the ground. The National Trust has now moved several of the lakeside boulders to near the Shell House so they are more accessible.

LANGLEY. Highest point in Essex (TL 4429 3619)
A point 1 kilometre north of Langley church is the highest point in Essex. It is 147 metres (482 feet) above sea level on the rolling chalk hills of north-west Essex. The Harcamlow Way, a long distance footpath, passes through this point.

MANUDEN. Puddingstones.
Next to the Yew Tree Inn (TL 491 267) is a colourful boulder of Hertfordshire puddingstone (120 x 100 x 30 cm in size) that has been whitewashed in the past. At Maggots End, one kilometre north of Manuden at the junction of the road to Pinchpools (TL 486 276), is another fine puddingstone one metre square and 60 cm thick.

NEWPORT. Chalk Farm Lane Chalk Pit (TQ 5234 3352)
Small disused chalk pit just beyond Newport Station on the former access road to Newport Limeworks.

NEWPORT. Debden Road Chalk Pit. (TL 5244 3384)
Very small roadside pit with minor exposure of Upper Chalk overlain by Anglian till (boulder clay) consisting of brown clay with chalk pebbles and other erratics. The till is material dumped by a glacier as it ground its way across the landscape 450,000 years ago. This is one of the few exposures of till in north Essex. The site is adjacent to a layby on the Debden Road.

NEWPORT. Debden Water Gravel Pit. (TL 5358 3399)
A small disused gravel pit in the valley of the Debden Water east of Newport. A low cliff of glacial gravel can be seen here which was laid down by torrents of meltwater from the Anglian Ice Sheet 450,000 years ago. In marked contrast to the sedate nature of the valley today. Piles of gravel with large nodular flints can be seen on the floor of the pit.

NEWPORT. Newport Puddingstone (TL 521 335)

A large boulder of Hertfordshire puddingstone 1.5 metres (5 feet) long can be seen by the village hall in Station Road. It was brought here from the outskirts of the town in the 1950s when the village hall was built . It stood outside the village hall until 2008 when it was moved a few metres onto the grass verge.

NEWPORT. The Leper Stone (TL 5199 3496)
A large coarse-grained sarsen stone 1.7 by 1.2 metres (6 feet by 4 feet) in size known as the Leper Stone sits upright on the grass verge on the side of the road at the north entrance to the village. This is the best known erratic boulder in north Essex. Adjacent to this is a wall constructed largely of blocks of clunch, a hard variety of chalk formerly used for building.

SAFFRON WALDEN. Ashdon Road Swallow Hole (TL 561 391)
A swallow hole is a depression in the ground in a limestone or chalk area into which a stream disappears underground. Some swallow holes are not obvious on the surface and are merely a point where a stream appears to dry up as it percolates through its gravel bed to continue its journey underground. An example of the latter is in the valley of The Slade where, during most times of the year, the stream disappears underground as it flows from the boulder clay plateau onto the Chalk at a point adjacent to the public footpath midway between Martins Wood and the Ashdon Road.

SAFFRON WALDEN. Elm Grove Summer House (TL 5398 3828)
Elm Grove is a group of bungalows for elderly persons, which were built on land which was formerly the rear garden of a property called Elm Grove which was built in 1828 and demolished in the 1970s. Against the flint boundary wall is a small structure built as a summer house or grotto in the former garden. The summer house is remarkable as it is built almost entirely from erratic boulders. There are at least 20 boulders of different rock types but of particular interest is a giant Hertfordshire puddingstone 2.6 by 1.2 metres (9 feet by 4 feet) in size at the base of the south wall, which may be the largest puddingstone in Essex. The summer house is not the only structure in the garden to survive the subsequent redevelopment. In the centre of the grounds is the prominent ruin of a delightful flint 'folly' which was once used as a tiny museum. Elm Grove is private property and permission for access must be obtained from the Estate Manager.

SAFFRON WALDEN. Grave of Edward Charlesworth (TL 5469 3847)

In the town cemetery is the grave of Edward Charlesworth (1813-1893), an eminent but controversial Victorian geologist who coined the term Red Crag. It has a very fine gravestone with an excellent epitaph.

SAFFRON WALDEN. Limefields Pit Nature Reserve (TL 541 396)

Disused chalk quarry less than 10 minutes walk from the town centre. The floor of the pit is occupied by housing. A buffer zone between the houses and the chalk face is an Essex Wildlife Trust nature reserve. The 6 metre high face is a fine exposure of Upper Chalk. The access gate is locked and the access is available by contacting the nature reserve warden. However, the face can be clearly seen from the road.

SAFFRON WALDEN. Radwinter Road Chalk Quarry (TL 553 385)
Fine disused chalk quarry with clean vertical faces. On the north side of Radwinter Road just east of Tesco's and currently used as a private depot. According to early 20th century geological survey records this was a very fossiliferous quarry. Fossil sponges, corals, crinoids, echinoids and even a belemnite and shark tooth have all been reported. Access is not possible but the faces are clearly visible from the pavement.

SAFFRON WALDEN. Ravine in the valley of The Slade
Remarkable natural ravine in the valley revealing chalky gravel that has yielded remains of mammoth and woolly rhinoceros.

SAFFRON WALDEN. Saffron Walden Museum Boulders (TL 5384 3872)
An interesting collection of erratic boulders in the grounds of the Museum, the most prominent being a very large and complete septarian nodule over two metres (6 feet) in diameter. There is also a fine basalt boulder (rare in Essex).

SAFFRON WALDEN. Westley Lane Chalk Pit. (TL 5363 4016)
Small chalk pit on the side of Westley Lane, a track leading to Westley Farm. Very fine exposures of clean, white chalk. The track is a public footpath but the pit is private land.

TAKELEY. Stansted Airport Stone (TL 561 212)
A sarsen stone about one metre square is situated on the grass by the crossroads. It was found by archaeologists in a Bronze Age pit at Stansted Airport and had clearly been placed in the pit some 3,500 years ago, suggesting that it had ceremonial significance. The stone was moved here in 2003 and provided with a plaque by the Takeley Local History Society.

THAXTED. Buckingam Farm Sarsen Stone (TL 606 295)
A sarsen stone 90 by 60 centimetres (3'x2') in size sits by the roadside outside the entrance to Buckingham Farm.

THAXTED. Stoney Lane (TL 611 309)
Stoney Lane, adjacent to the famous Guildhall, is a good example of a street paved with local erratics. The majority of the cobbles are flint but there are also a large number of other rock types.

TYE GREEN. Tye Green Kettle Hole (TL 538 238)
The public footpath from Tye Green to Warmans Farm passes around the rim of the north portal of the Stansted Airport railway tunnel. Prior to construction of the railway in 1989, trial boreholes along the proposed route of the tunnel revealed the presence of a deep depression in the boulder clay, which was filled with black organic sediments dating from the Hoxnian interglacial stage (400,000 years old). When the tunnel portal was constructed the sediments yielded interglacial fossils. This feature has been interpreted as a 'kettle hole' dating back to the time of the Anglian Ice Sheet some 450,000 years ago. Kettle holes are depressions created by the melting of blocks of stagnant ice left behind by the retreat of a glacier or ice sheet, in this case the Anglian Ice sheet that covered north Essex 450,000 years ago. Nothing now visible on the ground. Of historical interest only.

UGLEY GREEN. Ugley Green Puddingstone (TL 524 271)

Beside the green, next to the village pump, is a fine, rounded and colourful boulder of Hertfordshire puddingstone 1.2 metres (4 feet) long.

WENDENS AMBO. Wenden Place Boundary Wall (TL 512 363)
On the bend of the main road opposite the church is a high, ancient wall, which is remarkable for the variety of local rocks used in its construction, including many large boulders. The largest is a puddingstone 1.4 metres (4'6") long. The wall is a grade 2 listed building.

WICKEN BONHUNT. St. Helen's Chapel (TL 5114 3349)
This small, thatched, 11th century chapel is one of the oldest buildings in Essex. Apart from the front wall, which is brick, the walls consist almost entirely of glacial erratic cobbles and boulders gathered from the local fields 1,000 years ago. A large variety of rock types are present (inside and out) including at least 16 pieces of Hertfordshire puddingstone. The north-eastern corner is supported by a large sarsen stone.

WIDDINGTON. Widdington Puddingstone (TL 533 322)
At the road junction north of the village is a puddingstone 1.4 metres by 1 metre (4'x3') in size standing upright on the corner of a large wooded traffic island. As a result of recent road widening the boulder is now at risk from lorries turning this tight corner.

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