Stoke Lane Slocker | |
---|---|
Location | Stoke St Michael |
Depth | 30m |
Length | 2.18km |
Geology | Limestone |
Hazards | Weils Disease |
Cave survey |
Stoke Lane Slocker (grid reference ST66874745 ) is a cave near Stoke St Michael, in the Carboniferous Limestone of the Mendip Hills, in the English county of Somerset.
It is 2.18 km in length and reaches a depth of 30m. [1]
It was previously known as Stoke Lane Swallet, but now the local name is preferred. The origin of the word "Slocker" is obscure, possibly from "slock" meaning to entice or lure away [2] although the Gaelic word for swallow hole is "sluighaire".
It is believed that the first person to explore the cave in modern times was a Mr Marshall from Stratton-on-the-Fosse around 1905, but major exploration and measurement of this cave really started in 1947 when Sump 1 was reached. That sump was passed the same year and the decorated chambers of Stoke Two discovered. Sumps 2 to 7 were passed over the course of the 1960s. The Bailey-Ward series of chambers was discovered in 1971. [1] [3]
Cases of Weils Disease have been reported in those who have been into the cave. [1] [4]
The submerged entrance to the cave lies near the disused Stoke Lane Quarry, and from it an underground stream emerges into daylight to feed a water-source known as St Dunstan's Well. The cave has been designated as a Site of Special Scientific Interest. [5]
Stoke One (the length of passage between the entrance and Sump 1), is mainly made up of low passageways. However the Bailey-Ward Series of chambers includes Bernard's Rift, which is 20 metres (66 ft) high and contains crystal pools containing calcite-encrusted goniatite snail shells, and cave pearls. [1]
The area between Sumps 1 and 2, Stoke 2, contains a number of highly decorated chambers including the Upper Grotto, Traverse Grotto and the Throne Room which contains a 3 metres (10 ft) high stalactite boss named The King and a second stalactite, 2 metres (7 ft) high, named The Queen after Queen Victoria. The once-spectacular formations in the Princess Grotto have suffered damage since the cave was discovered. When the Bone Chamber, which is not decorated, was found it contained a number of human and animal bones, along with ash and charcoal. [1]
Beyond the second sump is a long stretch of passage containing a further six sumps.
Sump | Length of dive [1] | Notes [1] |
---|---|---|
Sump 1 | 18 inches (46 cm) | Free-divable |
Sump 2 | 10 metres (33 ft) | Fully equipped divers only |
Sump 3 | ? | Can be by-passed |
Sump 4 | 20 metres (66 ft) | Fully equipped divers only |
Sump 5 | ? | Can be by-passed |
Sump 6 | 12 metres (39 ft) | |
Sump 7 | 15 metres (49 ft) | Very tight |
Sump 8 | ? | Boulder-choked; cannot be passed |
Wookey Hole Caves are a series of limestone caverns, a show cave and tourist attraction in the village of Wookey Hole on the southern edge of the Mendip Hills near Wells in Somerset, England. The River Axe flows through the cave. It is a Site of Special Scientific Interest (SSSI) for both biological and geological reasons. Wookey Hole cave is a "solutional cave", one that is formed by a process of weathering in which the natural acid in groundwater dissolves the rocks. Some water originates as rain that flows into streams on impervious rocks on the plateau before sinking at the limestone boundary into cave systems such as Swildon's Hole, Eastwater Cavern and St Cuthbert's Swallet; the rest is rain that percolates directly through the limestone. The temperature in the caves is a constant 11 °C (52 °F).
Swildon's Hole is an extensive cave in Priddy, Somerset. At 9,144 metres (30,000 ft) in length, it is the longest cave on the Mendip Hills. It has been found to be connected to Priddy Green Sink and forms part of the Priddy Caves Site of Special Scientific Interest (SSSI).
The River Axe is a river in South West England. The river is formed by water entering swallets in the limestone and rises from the ground at Wookey Hole Caves in the Mendip Hills in Somerset, and runs through a V-shaped valley. The geology of the area is limestone and the water reaches Wookey Hole in a series of underground channels that have eroded through the soluble limestone. The river mouth is in Weston Bay on the Bristol Channel.
Banwell Caves are a 1.7-hectare geological and biological Site of Special Scientific Interest near the village of Banwell, North Somerset, England notified in 1963.
Lamb Leer is a 14.59 hectare geological Site of Special Scientific Interest between East Harptree and Priddy in the Mendip Hills, Somerset, notified in 1983. The cavern is a fragment of a very ancient major cave system which now contains one of the largest chambers in the Mendip Hills.
St. Dunstan's Well Catchment is a Site of Special Scientific Interest, covering 39.8 hectares near Stoke St Michael in the Mendip Hills, Somerset, England. The site was notified in 1967. It is of both geological and biological significance.
Thrupe Lane Swallet is a 0.5 hectares geological Site of Special Scientific Interest in Somerset, notified in 1992. It is also a Geological Conservation Review site.
Gough's Cave is located in Cheddar Gorge on the Mendip Hills, in Cheddar, Somerset, England. The cave is 115 m (377 ft) deep and is 3.405 km (2.12 mi) long, and contains a variety of large chambers and rock formations. It contains the Cheddar Yeo, the largest underground river system in Britain.
Stoke St Michael is a village and civil parish on the Mendip Hills 4 miles (6.4 km) north east of Shepton Mallet, and 8 miles (12.9 km) west of Frome, in the Mendip district of Somerset, England.
The caves of the Mendip Hills are formed by the particular geology of the Mendip Hills: large areas of limestone worn away by water makes it a national centre for caving. The hills conceal the largest underground river system in Britain.
GB Cave is a cave between Charterhouse and Shipham in the limestone of the Mendip Hills, in Somerset, England.
St Cuthbert's Swallet is the second longest, and most complex, cave on the Mendip Hills, in Somerset, England. It forms a major part of the Priddy Caves system and water entering this swallet re-emerges at Wookey Hole. St Cuthbert's Swallet is part of, and lies underneath, the Priddy Pools Site of Special Scientific Interest.
Shatter Cave is a cave in Fairy Cave Quarry, near Stoke St Michael in the limestone of the Mendip Hills, in Somerset, England. It falls within the St. Dunstan's Well Catchment Site of Special Scientific Interest.
Balch Cave is a cave in Fairy Cave Quarry, near Stoke St Michael in the limestone of the Mendip Hills, in Somerset, England. The cave is part of the complex of passages feeding to St. Dunstan's Well Catchment Site of Special Scientific Interest and an abandoned Bristol Water abstraction point.
Hillier's Cave is a cave in Fairy Cave Quarry, near Stoke St Michael in the limestone of the Mendip Hills, in Somerset, England.
Attborough Swallet is a cave in Chewton Mendip in Somerset, England.
W/L Cave is part of the Fairy Cave Quarry group of caves between Stoke St Michael and Oakhill in the limestone of the Mendip Hills, in Somerset, England.
Charterhouse Cave, on the Mendip Hills in Somerset, is the deepest cave in southern England.
The Cheddar Yeo is a small river in Somerset, England. Beneath the limestone of the Mendip Hills it forms the largest underground river system in Britain. After emerging into Cheddar Gorge it flows through the village of Cheddar, where it has been used in the past to power mills. From the Middle Ages until the 19th century the river had ports for seagoing vessels but is no longer navigable. Some of the water, which is of good quality, is diverted into Cheddar Reservoir to provide drinking water for Bristol.
Reservoir Hole is a cave in Cheddar Gorge in Somerset, southwest England. It contains what is believed to be the largest chamber yet found under the Mendip Hills.