England's Historic Seascapes: Withernsea to Skegness

Museum of London Archaeology, 2010. https://doi.org/10.5284/1000104. How to cite using this DOI

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https://doi.org/10.5284/1000104
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Museum of London Archaeology (2010) England's Historic Seascapes: Withernsea to Skegness [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1000104

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David Bowsher
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Museum of London Archaeology
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Resource identifiers

Digital Object Identifiers

Digital Object Identifiers (DOIs) are persistent identifiers which can be used to consistently and accurately reference digital objects and/or content. The DOIs provide a way for the ADS resources to be cited in a similar fashion to traditional scholarly materials. More information on DOIs at the ADS can be found on our help page.

Citing this DOI

The updated Crossref DOI Display guidelines recommend that DOIs should be displayed in the following format:

https://doi.org/10.5284/1000104
Sample Citation for this DOI

Museum of London Archaeology (2010) England's Historic Seascapes: Withernsea to Skegness [data-set]. York: Archaeology Data Service [distributor] https://doi.org/10.5284/1000104

Lynn Character Area

Present Day Form

The Lynn character area is situated at the southern end of the study area immediately offshore from the Skegness and Mablethorpe coastal waters character area. The geology of the area comprises chalk bedrock overlain by glacial till (clay, sand and gravel debris deposited from ice sheets) known as the Boulders Bank formation. The water depth across the area varies between 6m and 13m and the maximum tidal range is 6m. The seabed of the area consists of a shallow sloping thin bed of sand, gravel and shells.

Sea Use: Present

The character area contains a licensed area for an offshore wind farm. The proposed site for this extends over an area of 2.5 km by 4 km (1.35 nautical miles by 2.15 nautical miles) orientated approximately east-west. The shortest distance between any turbine and the nearest point on the coast is 5 km.

The principal fishing activity in the area is long-lining and some netting for cod, roker, sole and brill, trawling for white fish by beam trawlers, crab and lobster potting and shrimp fishing for brown and pink shrimp. The area is not the most intensively fished of the inshore area between the Humber and The Wash, but is locally important, particularly for smaller vessels and for vessels following the more mobile fisheries. The area has spawning areas of Dover sole and lemon sole and is within nursery areas used by lemon sole and plaice, but is offshore of the main Dover sole and cod nursery areas.

Sea Use: Past

The Lynn Character area has been shaped by thousands of years of dynamic sea level changes and erosion and deposition. The relatively shallow nature of the sea bed means that the area was dry land almost certainly in the Upper Palaeolithic, Mesolithic and probably in the Neolithic periods.

Marine traffic would have crossed this area on a regular basis from the Roman period onwards but especially in the medieval period when Wainfleet St Mary was a busy port. Its access to the sea gradually silted up and Wainfleet Haven was established nearer the coast to carry on the maritime trade. Continued silting and dune formation resulted in the last commercial vessels using the port in the1920's. Fishing activity would have been carried out in the area from the medieval period onwards.

Archaeological Potential

The Lynn character area has potential for the presence of drowned land surfaces resulting from the fact that sea level has fluctuated between -120 metres and +10 metres over the past 500,000 years. From the period 500,000 BP to 22,000 BP (before present), human population levels were low, and little more than stray finds may be expected, although these may still be of considerable archaeological importance.

From 22,000 BP to 2100 BP parts of the North Sea were dry land and human population levels were higher. The area's position adjacent to the Ouse/Nene palaeochannel makes it prime habitation site. Consequently, there is some potential for surviving evidence of human activity within the area. Over the last 6000 years (if not more), humans have used sea faring vessels and so wrecks and related material may lie on the sea floor or be buried beneath the sea floor.

Character Perceptions

Along the coast there are a number of seaside resorts at Skegness, Ingoldmells and Mablethorpe. The area is perceived as an inshore fishing ground and also as an immediate offshore area to an important recreational area around Skegness and the National Nature Reserve at Gibraltar Point.

References

http://www.amec.com/uploadfiles/LynnNTS.pdf Lynn offshore Wind Farm Non -Technical summary

BGS (British Geological Survey), 2001 North Sea Geology. Technical Report TR_008 for Strategic Environmental Assessment (SEA2)

Images

Leman Field

Lynn Windfarm
Web: www.flickr.com/photos/electropod/3087010838/




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