Pocklington Beck

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Pocklington Beck
Beck between Millington and Pocklington (geograph 5744458).jpg
Beck between Millington and Pocklington
East Riding of Yorkshire UK relief location map.jpg
Red pog.svg
Location
County East Riding of Yorkshire
CountryEngland
Physical characteristics
SourceMillington Springs
 • location Millington
 • coordinates 53°58′07″N0°42′59″W / 53.9686°N 0.7164°W / 53.9686; -0.7164
 • elevation289 feet (88 m)
Mouth Cottingwith Lock
 • location
 Cottingwith
 • coordinates
 53°52′33″N0°56′12″W / 53.8757°N 0.9366°W / 53.8757; -0.9366
 • elevation
16 feet (5 m)
Basin size23,300 acres (9,431 ha)
Basin features
River system River Derwent

Pocklington Beck is a watercourse that flows westwards from Pocklington in the East Riding of Yorkshire, and empties into the River Derwent at East Cottingwith. The beck is known for being culverted through the town of Pocklington, and for being susceptible to flooding. Historically the beck supported the villages along the route by providing water-power for several corn mills.

Contents

Course

The beck has two feeder streams which are to the north of Pocklington, including Millington Springs which feed Millington Beck, an affluent of Pocklington Beck. [1] [2] [3] Further downstream, the beck acquires different names such as Bielby Beck and simply just The Beck on mapping, but the Environment Agency lists it as Pocklington Beck until it reaches the River Derwent. [4] [5] The beck flows south-westwards across the low-lying edge of the Vale of York, and is the chief watercourse for drainage in the area. [6]

As the beck runs through Pocklington, the streets and road run parallel to the beck, akin to the situation in Driffield. [7] Various building schemes and civic improvements have left the beck largely culverted through the town of Pocklington, though accumulation of silt and gravel adds to the beck being flooded during high rainfall. [8] To the south of Pocklington, a mill dam used to extend from just under the railway line to feed White Mill. After the old mill site, is a permanently flooded area which provides a haven for wildlife. [9] Further south, the Pocklington Canal parallels the course of the beck all the way to the River Derwent, however, all the drainage channels still feed into the beck, not the canal. [10] [11] As it meanders through the land, the beck is the natural dividing line between the parishes, with Allerthorpe to the north of the beck, and Harswell and Seaton Ross to the south. [12]

The beck flows into the Pocklington Canal at Cottingwith at a height of 16 feet (5 m) above sea level, and then the combined waters empty into the River Derwent. [13] [14] The beck has many tributaries and all told, drains an area covering 9,431 hectares (23,300 acres). [4] [5]

Hydrology

Despite the land being underlain by the Pocklington Gravel Formation, which should drain away the excess water, the area surrounding the beck is fairly low-lying (at most it is 50 feet (15 m) above sea level apart from Millington Springs) and the beck is prone to flooding. [15] Documents from the 1320s describe flooding in the small valley that the beck flows through due to the drains being overwhelmed, and the road crossing the beck at Walbut water mill being difficult to pass during periods of high rainfall. [16]

Water from the beck was diverted south of Pocklington in 1818 to feed the Pocklington Canal. [17] When this canal fell into disuse, neither waterway was maintained which led to flooding on both waterways. [18] Flooding remains an issue on the beck, and in the 21st century the beck has flooded the town of Pocklington in 2007, 2012 and in 2015. [19] [20] During the period of the Boxing Day Floods of 2015, Pocklington was not as severely affected as other locations in Northern England, the beck did record its highest level at 2 feet 5 inches (0.73 m). [21] Flooding through the town is partly due to fact that the beck has been culverted through the town, and silt and gravel have built up in the culverts. Work was undertaken in 2010 to remove debris, silt and gravel from the beck. [22] [23] Historical floods have occurred in December 1927, when snow-melt and heavy rain resulted in numerous streets within Pocklington being inundated, [24] December 1954 when several streets were flooded to a depth of 2 feet (0.61 m), [25] October 1968, when 1.31 inches (33 mm) of rain fell in one day (the area normally receives an average of 24 inches (610 mm) of rain per year), [26] and December 1996 when Chapmangate was flooded. [27]

In 1995, sewage spilled into Pocklington Beck which then flowed into the Pocklington Canal through the canal had which is fed from Pocklington Beck. Many fish were suffocated due to the sewage removing the oxygen from the water. The National Rivers Authority (precursor of the Environment Agency) spent time pumping oxygen into the canal. [28]

In 2016, a proposal was put forward to build a flood alleviation dam upstream of the town of Pocklington which was approved at a cost of £4.6 million in October 2017. [29] Work commenced in 2018 and the dam was completed in 2019 and cost £4.7 million. The dam consists of a bund 5 metres (16 ft) high, 600 metres (2,000 ft) long, and 45 metres (148 ft) wide, located at SE808499 . [30]

The spring at Millington used to be a source of public water supply, at a rate of 590,000 imperial gallons; 710,000 US gallons (2,700,000 L) per day, but it was closed in the 1970s when rising nitrate levels within the water became an issue. [31] In 2024, Yorkshire Water stated that they would be investing £7.3 million in upgraded the wastewater treatment works at Pocklington to prevent discharge into the beck during periods of heavy or prolonged rainfall, and that phosphorus pollution would be reduced. [32]

Flora and fauna

The beck is known to have species of brown trout, rainbow trout, minnow, stickleback and crayfish along its length. [33] The native white-clawed crayfish was found to be living in the culverts under Pocklington town when action was being taken to remove gravel and silt from the beck. [34] Further downstream is the Melbourne and Thornton Ings SSSI, which supports several plants including reed grass, bladder sedge, reed sweetgrass, marsh stitchwort and tubular water-dropwort. It is also host to a variety of birdlife such as pintail, garganey and gadwall. Otters are also known to visit the site. [35]

Industry

The beck supported several watermills, with some still working up until the middle of the 20th century. The development of the town of Pocklington was due to the "fast-flowing beck", which allowed for several mills to be constructed and the mills were "crucial to the town's development." [15]

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References

  1. ↑ "Pocklington water supply". The Yorkshire Herald and the York Herald. No. 12, 764. 3 May 1892. p. 6. OCLC   751480479.
  2. ↑ Gale, I. N.; Rutter, H. K.; Adams, B. (2006). The Chalk aquifer of Yorkshire. Keyworth, Nottingham: British Geological Survey. p. 50. ISBN   0-85272-480-2.
  3. 1 2 3 Nottingham & Bellingham 2011, p. 3.
  4. 1 2 "Pocklington Beck from Source to Bielby beck | Catchment Data Explorer | Catchment Data Explorer". environment.data.gov.uk. Retrieved 5 September 2024.
  5. 1 2 "Pocklington Beck from Bielby Bk to River Derwent | Catchment Data Explorer | Catchment Data Explorer". environment.data.gov.uk. Retrieved 5 September 2024.
  6. ↑ Allison 1976a, p. 179.
  7. ↑ Allison, Keith John (1976). The East Riding of Yorkshire Landscape. London: Hodder & Stoughton. p. 225. ISBN   0-3401-5821-2.
  8. ↑ Bagshaw, Mike (2018) [2014]. Slow travel; North York Moors and Yorkshire Wolds (2 ed.). Chalford St Peter: Bradt. p. 162. ISBN   978-1-78477-075-4.
  9. ↑ Nottingham & Bellingham 2011, p. 22–23.
  10. ↑ Sheppard, June A. (1966). The draining of the marshlands of South Holderness and the Vale of York. York: East Yorkshire Local History Society. p. 23. OCLC   4336055.
  11. ↑ Crackles, F. E.; Arnett, Roger R. (1990). Flora of the East Riding of Yorkshire. Hull: Hull University Press : Humberside County Council. p. 5. ISBN   0859584879.
  12. ↑ Allison 1976a, p. 133.
  13. ↑ Historic England. "Pocklington Canal Cottingwith Lock (Grade II) (1162005)". National Heritage List for England . Retrieved 27 September 2024. Map shows contours
  14. ↑ Phillips, John (1853). The rivers, mountains, and seacoast of Yorkshire. With essays on the climate, scenery, and ancient inhabitants of the county. London: Murray. p. 92. OCLC   957204471.
  15. 1 2 Gannon, Barrie (2019). "Pocklington Neighbourhood Development Plan Townscape Character Assessment" (PDF). pocklington.gov.uk. p. 5. Retrieved 13 October 2024.
  16. ↑ Allison 1976a, p. 181.
  17. ↑ Duckham, Baron F. (1972). The inland waterways of East Yorkshire, 1700-1900. York: East Yorkshire Local History Society. p. 64. ISBN   0900349298.
  18. ↑ Allison, Keith John (1976). The East Riding of Yorkshire Landscape. London: Hodder & Stoughton. p. 171. ISBN   0-3401-5821-2.
  19. ↑ "Calls for better flood protection in Pocklington". BBC News. 3 May 2012. Retrieved 1 September 2024.
  20. ↑ "York floods 2015: How the devastating floods unfolded and how York rallied superbly". York Press. 28 July 2016. Retrieved 5 September 2024.
  21. ↑ "Pocklington Beck level at Pocklington - GOV.UK". check-for-flooding.service.gov.uk. Retrieved 5 September 2024.
  22. ↑ "Work begins to clean up town watercourse - ProQuest" . Hull Daily Mail. 8 March 2010. ProQuest   333726984 . Retrieved 2 September 2024.
  23. ↑ Gannon, Barrie (2019). "Pocklington Neighbourhood Development Plan Townscape Character Assessment" (PDF). pocklington.gov.uk. p. 6. Retrieved 13 October 2024.
  24. ↑ "Pocklington flooded". Hull Daily Mail. No. 13, 170. 22 December 1927. p. 7. ISSN   1741-3419.
  25. ↑ "Raging Torrent". Hull Daily Mail. No. 21, 508. 9 December 1954. p. 9. ISSN   1741-3419.
  26. ↑ "Its mopping-up day for Wolds towns". Hull Daily Mail. No. 25, 818. 29 October 1968. p. 7. ISSN   1741-3419.
  27. ↑ "20 years ago". The York Press. 20 December 2016. p. 11. ISSN   1757-3289.
  28. ↑ Morris, Allison (29 July 1995). "Race against time to save canal fish". Hull Daily Mail. p. 7. ISSN   1741-3419.
  29. ↑ Willers, Daniel (16 October 2017). "£4.6m flood bank plan is approved". The York Press. p. 14. ISSN   1757-3289.
  30. ↑ "Flood Risk Strategy Pocklington Flood Alleviation Scheme (POCFAS)". eastriding.gov.uk. Retrieved 2 September 2024. Expand the "What flood alleviation schemes are being undertaken in my area?"
  31. ↑ Gale, I. N.; Rutter, H. K.; Adams, B. (2006). The Chalk aquifer of Yorkshire. Keyworth, Nottingham: British Geological Survey. pp. vii, 51. ISBN   0-85272-480-2.
  32. ↑ Booth, Harry (14 October 2024). "'Incredibly important' £7.3 million project to improve North Yorkshire waterway". Gazette & Herald. Retrieved 14 October 2024.
  33. ↑ "Hundreds of fish die during bridge repairs". Hull Daily Mail. 29 July 1994. p. 12. ISSN   1741-3419.
  34. ↑ Campbell, James (18 May 2010). "Crayfish claw their way back; endangered species discovered in beck- ProQuest" . Hull Daily Mail. ProQuest   288382549 . Retrieved 2 September 2024.
  35. ↑ "Melbourne and Thornton Ings" (PDF). designatedsites.naturalengland.org.uk. Retrieved 5 September 2024.
  36. ↑ Allison 1975, p. 40.
  37. ↑ Historic England. "Bielby Mill (Grade II) (1084125)". National Heritage List for England . Retrieved 1 September 2024.
  38. ↑ Historic England. "Devonshire Mill (Grade II) (1162000)". National Heritage List for England . Retrieved 5 September 2024.
  39. ↑ Plumptre, George (15 February 2020). "Small and white, clean and bright". The Daily Telegraph. No. 51, 241. Saturday. p. 18. ISSN   0307-1235.
  40. ↑ Allison 1975, p. 45.
  41. ↑ Historic England. "Ousethorpe medieval settlement, moat and mill 310m south of Ousethorpe Farm (1018406)". National Heritage List for England . Retrieved 2 September 2024.
  42. ↑ Allison 1975, p. 48.
  43. ↑ Sheppard, June A. (1966). The draining of the marshlands of South Holderness and the Vale of York. York: East Yorkshire Local History Society. p. 17. OCLC   4336055.
  44. ↑ "On the History Trail: The mills of Pocklington - ProQuest" . The Pocklington Post. 11 November 2013. ProQuest   1449810463 . Retrieved 13 October 2024.

Sources

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