Wurt Pit and Devil's Punchbowl

Last updated

Wurt Pit and Devil's Punchbowl
Site of Special Scientific Interest
The Devils Punch Bowl (geograph 2679658).jpg
Somerset UK location map.svg
Red pog.svg
Location within Somerset
Location Somerset
Grid reference ST543537
Coordinates 51°16′50″N2°39′24″W / 51.2806°N 2.6566°W / 51.2806; -2.6566 Coordinates: 51°16′50″N2°39′24″W / 51.2806°N 2.6566°W / 51.2806; -2.6566
InterestGeological
Area0.2 hectares (0.0020 km2; 0.00077 sq mi)
Notification 1987 (1987)
Natural England website

Wurt Pit and Devil's Punchbowl (grid reference ST543537 ) is a 0.2 hectare (0.5 acre) geological Site of Special Scientific Interest between East Harptree and the Priddy Circles in the Mendip Hills, Somerset, notified in 1987.

Natural England describes the site as:

"This site consists of the two largest subsidence depressions in the Mendips, formed by the underlying limestones having been dissolved by subterranean waters causing the surface rocks to collapse into the void. Clear evidence of their being collapsed structures rather than erosional or solutional features, is gained from the fact that the surface rocks at both localities are insoluble, being marls at Devil's Punchbowl and a series of limestones and clays which have been impregnated by silica at Wurt Pit." [1] "The silica-enrichment of the limestones and clays at Wurt Pit (known as the 'Harptree Beds', of early Jurassic age) is also of considerable mineralogical importance since it took place as part of the main phase of mineralisation which emplaced the principal Mendip orefields during Jurassic times. The Harptree Beds show varying degrees of silica-enrichment, and also contain traces of other minerals, such as limonite and yellow ochre (hydrous ferric oxides), barite (barium sulphate), sphalerite (zinc sulphide) and galena (lead sulphide)." [1]

Wade and Wade, in their 1929 book Somerset, described the Devil's Punch Bowl as one of the most notable Swallet Holes on the Mendips [2]

Related Research Articles

Chert Hard, fine-grained sedimentary rock composed of cryptocrystalline silica

Chert is a hard, fine-grained sedimentary rock composed of microcrystalline or cryptocrystalline quartz, the mineral form of silicon dioxide (SiO2). Chert is characteristically of biological origin, but may also occur inorganically as a chemical precipitate or a diagenetic replacement, as in petrified wood.

Mendip Hills Range of limestone hills to the south of Bristol and Bath in Somerset, England

The Mendip Hills is a range of limestone hills to the south of Bristol and Bath in Somerset, England. Running from Weston-super-Mare and the Bristol Channel in the west to the Frome valley in the east, the hills overlook the Somerset Levels to the south and the Chew Valley and other tributaries of the Avon to the north. The hills give their name to the local government district of Mendip, which administers most of the area. The higher, western part of the hills, covering 198 km2 (76 sq mi) has been designated an Area of Outstanding Natural Beauty (AONB), which gives it a level of protection comparable to a national park.

Geology of Dorset

Dorset is a county in South West England on the English Channel coast. Covering an area of 2,653 square kilometres (1,024 sq mi); it borders Devon to the west, Somerset to the north-west, Wiltshire to the north-east, and Hampshire to the east. The great variation in its landscape owes much to the underlying geology, which includes an almost unbroken sequence of rocks from 200 to 40 million years ago (Mya) and superficial deposits from 2 Mya to the present. In general, the oldest rocks appear in the far west of the county, with the most recent (Eocene) in the far east. Jurassic rocks also underlie the Blackmore Vale and comprise much of the coastal cliff in the west and south of the county; although younger Cretaceous rocks crown some of the highpoints in the west, they are mainly to be found in the centre and east of the county.

Devil's Punch Bowl may refer to:

Geology of Somerset

Somerset is a rural county in the southwest of England, covering 4,171 square kilometres (1,610 sq mi). It is bounded on the north-west by the Bristol Channel, on the north by Bristol and Gloucestershire, on the north-east by Wiltshire, on the south-east by Dorset, and on the south west and west by Devon. It has broad central plains with several ranges of low hills. The landscape divides into four main geological sections from the Silurian through the Devonian and Carboniferous to the Permian which influence the landscape, together with water-related features.

East Harptree Human settlement in England

East Harptree is a village and civil parish in Somerset, England. It is situated 5 miles (8.0 km) north of Wells and 15 miles (24.1 km) south of Bristol, on the northern slope of the Mendip Hills overlooking the Chew Valley. The parish has a population of 644. The parish includes the hamlet of Coley.

The Chew Valley is an affluent area in North Somerset, England, named after the River Chew, which rises at Chewton Mendip, and joins the River Avon at Keynsham. Technically, the area of the valley is bounded by the water catchment area of the Chew and its tributaries; however, the name Chew Valley is often used less formally to cover other nearby areas, for example, Blagdon Lake and its environs, which by a stricter definition are part of the Yeo Valley. The valley is an area of rich arable and dairy farmland, interspersed with a number of villages.

Harptree Combe

Harptree Combe is a 13.63-hectare (33.68-acre) Site of Special Scientific Interest (SSSI) near East Harptree notified in 1954. "Combe" or "coombe" is a West Country word meaning a steep-sided valley. It is also the site of a 19th-century aqueduct and is overlooked by the site of a castle dating from around 1100.

Cloford Quarry Geological Site of Special Scientific Interest in Somerset, England

Cloford Quarry is a 39.92-hectare (98.6-acre) geological Site of Special Scientific Interest to the south of the A361 approximately 350 metres (1,150 ft) north of the hamlet of Cloford and 1 kilometre (0.6 mi) west of Nunney on the Mendip Hills in Somerset. It was notified in 1994.

Leighton Road Cutting is a 0.6 hectare geological Site of Special Scientific Interest between East Cranmore and Cloford in Somerset, notified in 1984. It is a Geological Conservation Review site

Sandpit Hole and Bishop's Lot is a 1.8 hectare geological Site of Special Scientific Interest near Ebbor Gorge in Somerset, notified in 1987.

Radiolarite Type of sedimentary rock

Radiolarite is a siliceous, comparatively hard, fine-grained, chert-like, and homogeneous sedimentary rock that is composed predominantly of the microscopic remains of radiolarians. This term is also used for indurated radiolarian oozes and sometimes as a synonym of radiolarian earth. However, radiolarian earth is typically regarded by Earth scientists to be the unconsolidated equivalent of a radiolarite. A radiolarian chert is well-bedded, microcrystalline radiolarite that has a well-developed siliceous cement or groundmass.

Wanstrow Human settlement in England

Wanstrow is a village and civil parish 6 miles (9.7 km) south west of Frome in the Mendip district of Somerset, England. The parish includes the village of Cloford.

Geology of England Overview of the geology of England

The geology of England is mainly sedimentary. The youngest rocks are in the south east around London, progressing in age in a north westerly direction. The Tees-Exe line marks the division between younger, softer and low-lying rocks in the south east and the generally older and harder rocks of the north and west which give rise to higher relief in those regions. The geology of England is recognisable in the landscape of its counties, the building materials of its towns and its regional extractive industries.

Colemans Quarry Limestone quarry in Somerset, England

Colemans Quarry, grid reference ST726452 is a limestone quarry at Holwell, near Nunney on the Mendip Hills, Somerset, England.

Gurney Slade quarry Limestone quarry in Somerset, England

Gurney Slade quarry, grid reference ST626497 is a limestone quarry near Gurney Slade between Binegar and Holcombe, on the Mendip Hills, Somerset, England.

Torr Works Limestone quarry in Somerset, England

Torr Works quarry, grid reference ST695446 is a limestone quarry at East Cranmore, near Shepton Mallet on the Mendip Hills, Somerset, England. The quarry was formerly known as Merehead, a name which has been retained for its rail depot on the opposite side of the A361 road.

Blue Lias Triassic/Jurassic geological formation in the UK

The Blue Lias is a geological formation in southern, eastern and western England and parts of South Wales, part of the Lias Group. The Blue Lias consists of a sequence of limestone and shale layers, laid down in latest Triassic and early Jurassic times, between 195 and 200 million years ago. The Blue Lias is famous for its fossils, especially ammonites.

Geography of Somerset

The county of Somerset is in South West England, bordered by the Bristol Channel and the counties of Bristol and Gloucestershire to the north, and Wiltshire to the east, Dorset to the south, and Devon to the west. The climate, influenced by its proximity to the Atlantic Ocean and the prevailing westerly winds, tends to be mild, damp and windy.

Finedon Top Lodge Quarry

Finedon Top Lodge Quarry, also known as Finedon Gullet is a 0.9 hectare geological Site of Special Scientific Interest east of Wellingborough in Northamptonshire. It is a Geological Conservation Review site revealing a sequence of middle Jurassic limestones, sandstones and ironstones, and is the type section for a sequence of sedimentary rocks known as the 'Wellingborough Member'. It was created by quarrying for the underlying ironstone for use at Wellingborough and Corby Steelworks; the ore was transported by the 1,000 mm gauge Wellingborough Tramway.

References

  1. 1 2 "Wurt Pit And Devil's Punchbowl" (PDF). English Nature. Retrieved 11 July 2006.