Sign warning of the risk of entrapment in the Mud Springs

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.[1] 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[1][2] and brings to the surface iridescent fossils originating in the mid to late Oxfordian age of the Late Jurassic.[3] 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).[4]

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.[5] In 1990 an attempt was made to fill in the most active spring by putting 100 tonnes (110 tons) of rubble into it.[6] This displaced mud, which ran into Hancock's Water, but the rubble could no longer be seen.[3]

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.[7]

References

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  1. 1 2 "SSSI citation sheet for Wootton Bassett Mud Spring" (PDF). Natural England. Retrieved 25 May 2023.
  2. ↑ Bristow, C.R.; Gale, I.N.; Fellman, E. (2000). "The lithostratigraphy, biostratigraphy and hydrogeological significance of the mud springs at Templars Firs, Wootton Bassett, Wiltshire". Proceedings of the Geologists' Association. 111 (3): 231–245. doi:10.1016/S0016-7878(00)80016-4.
  3. 1 2 Baird, Bill (2002). "The mud springs of Wootton Bassett, Wiltshire". The Edinburgh Geologist (38): 30.
  4. ↑ Hart, M.B.; Henderson, A.S.; Frayling, T.; Adair, T. (2006). "Microfossils from the Wootton Bassett Mud Springs (Wiltshire, UK)". Geoscience in South-west England. 11: 199–204.
  5. ↑ Leighton, Barry (28 October 2015). "It's mud, mud, inglorious mud". Swindon Advertiser. Retrieved 3 September 2016.
  6. ↑ Snelling, Andrew A. "A "165 Million Year" Surprise". Answers in Genesis. Retrieved 3 September 2016.
  7. ↑ Atkinson, Tony; Cowan, Don; Danson, Mike; Hough, David; Raven, Neil; Poole, Debbie; O'Flaherty, Peter; Riley, Paul; Atkinson, Max; Hill, Sue; Atkinson, Maureen; Montagu, David. "Wootton Bassett Mud Springs Expedition". British Microbial Biodiversity Association. Archived from the original on 4 February 2017. Retrieved 14 February 2020.

51°31′58″N 1°53′22″W / 51.53277°N 1.88952°W / 51.53277; -1.88952

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