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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Tel: 020 7410 2285

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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

Indefatigable Banks Character Area

Present Day Form

The Indefatigable Banks is an offshore character area situated in the eastern section of the study area. The geology of the area comprises a complex of Jurassic and Triassic bedrock overlain by glacial till (clay, sand and gravel debris deposited from ice sheets) known as the Elbow Formation. The water depth across the area varies between 15m and 20 m in the deeps and 8m to 10m on the shoals and the maximum tidal range is c 2m. The seabed of the area is characterised by the large sand mega ripple bank which is orientated NW - SE across the area and is part of the series of banks and deeps stretching away to the SW. This makes the area hazardous for navigation where a combination of low tide and high seas can cause breaking waves on the shoals.

Sea Use: Present

The Indefatigable Banks character area's dominant characteristic is navigation as the bank forms a seabed hazard. Commercial shipping tends to avoid the area because of this but fishing vessels cross it in order to fish the extensive grounds in the area. The area contains the gas filed Venture but no pipelines are present. Trawling for white fish, such as cod and whiting, takes place in the deeps between the mega ripple shoals.

Sea Use: Past

The Indefatigable Banks 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. Marine traffic would have historically avoided this area but numerous wrecks will be found here possibly dating from the Roman period onwards. Fishing activity would have been carried out in the area from the medieval period onwards.

As part of the Leman Ground it is a named fishing ground on Close's Fisherman's Chart (UKHO 1953), which describes the area as a good fishing ground in between the shoals. In the south, June to Sept are good months. Fish: Plaice Soles Cod and Dabs. Large lumps of coal are often taken in the nets. The trawling up of coal by fishing vessels suggests that the area has long been a dangerous place for shipping and may suggest that Colliers coming down the coast from the Northeast to London were regularly lost in this area

Archaeological Potential

The Indefatigable Banks 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, especially in the Mesolithic age. Finds dating to the Mesolithic have been found to a depth of 40m so any area of sea bed above that has potential for habitation. Inundation of the North Sea landscapes occurred between 10,000 and 6,000 BP and the most likely evidence for human occupation would be, therefore, Mesolithic in date. Earlier Palaeolithic occupation is less likely to be found and later Neolithic occupation is likely to have been limited to the inshore and very highest of the banks and shoals such as the Dogger Bank.

The area's position makes it a possible Upper Palaeolithic and Mesolithic habitation site as it lies on the edge of a possible palaeochannel to the east which now is the deep water North Sea Transport Route. 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 this area, because of it's dangerous shoals, is a prime area for wrecks and related material that may lie on the sea floor or be buried beneath the sea floor.

Character Perceptions

The area is perceived as a navigation hazard and fishing ground.

References

Close's Fisherman's Chart (UKHO 1953)
Fisheries Sensitivity Maps in British Waters (MAFF 1989)
Scandoil, North Sea Oil and Gas production Fields (Scandoil Oil and Gas Magazine online)

Images

Indefatigable platform

Indefatigable platform
Web: http://www.oilandgas.org.uk/issues/decommissioning/case-studies.cfm




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