place

Royal Wootton Bassett Town F.C.

1882 establishments in EnglandAssociation football clubs established in 1882Football clubs in EnglandFootball clubs in WiltshireHellenic Football League
Royal Wootton BassettUse British English from June 2015

Royal Wootton Bassett Town Football Club are an English football club based in the town of Royal Wootton Bassett in Wiltshire. The club has two senior men's, one ladies, two veterans, 20 youth and mini soccer and three girls teams and is affiliated to the Wiltshire County Football Association. The record match attendance was 2,103 versus Swindon Town in July 1991. The club's men's first team are currently members of the Hellenic League Premier Division at level nine of the English football league system.

Excerpt from the Wikipedia article Royal Wootton Bassett Town F.C. (License: CC BY-SA 3.0, Authors).

Royal Wootton Bassett Town F.C.
Cricketers Close,

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N 51.545411111111 ° E -1.8962333333333 °
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Cricketers Close

Cricketers Close
SN4 8JD
England, United Kingdom
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Wootton Bassett Mud Spring
Wootton Bassett Mud Spring

Wootton Bassett Mud Spring (grid reference SU078815) is an 8,000-square-metre (9,600 sq yd) geological Site of Special Scientific Interest in Wiltshire, England, notified in 1997. It can be found following a ten-minute walk from the canal car park opposite Templars Way, along the Wilts & Berks Canal cut and then south across agricultural land. The mud springs at Wootton Bassett are oozing springs of cold, grey mud that blister up under a thin layer of vegetation from Ampthill Clay. The water emerging in the mud comes from an aquifer in the Coral Rag Formation beneath the clay and brings to the surface iridescent fossils originating in the mid to late Oxfordian age of the Late Jurassic. The fossils, sometimes with aragonite covering, include foraminifera and ostracoda and are exceptionally well preserved. Also found are many specimens of otoliths, dominated by forms identified as Otolithus (Leptolepididarum).The flow is generally a slow ooze; however, in 1974 workers clearing the nearby stream, Hancock's Water, described a jet of mud rising into the air. In 1990 an attempt was made to fill in the most active spring by putting 100 tonnes (110 tons) of rubble into it. This displaced mud, which ran into Hancock's Water, but the rubble could no longer be seen.In June 1996, the British Microbiological Biodiversity Association (BMBA) sent a team of microbiologists to monitor and sample the springs. They discovered that the springs are more than 120 metres (390 ft) deep and 75 millimetres (3.0 in) in diameter. They emit a steady flow of fluidised mud at a rate of several cubic metres per day. The BMBA scientists were interested in the anaerobic microbiology of the mud flow and the possible links between this source and the deep terrestrial biosphere. They discovered that within the area there are five main sites of mud-spring activity, one of which can be subdivided into three separate mud springs. They also measured the temperature, pH and conductivity of the fluid within the springs.