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

Data copyright © Historic England unless otherwise stated

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Primary contact

David Bowsher
Director of Research
Museum of London Archaeology
Mortimer Wheeler House
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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

Hewett Character Area

Present Day Form

The Hewett offshore character area is situated in the southern eastern section of the study area in the central area of major gas fields of the Hewett and Leman areas off the northeast coast of Norfolk. The geology of the area comprises Chalk bedrock overlain by glacial till (clay, sand and gravel debris deposited from ice sheets) know as the Boulders Bank Formation. The water depth across the area varies between 15 m and 30 m and the maximum tidal range is 2-3 m. The area has no active aggregate extraction or wind farm industries but is associated with gas extraction from the major gas producing Hewett field with connecting pipelines running through the area.

Sea Use: Present

The Hewett character area dominant character is gas related industry. The Hewett field was discovered in 1966 and started production in 1983. With reserves of 120 billion cubic metres of gas and 1.33 million tons of oil and a peak production of 8.6 billion cubic metres of gas per year it is one of the southern North Sea's major hydrocarbon fields with permanent installations both on the seabed and free standing rigs. The field is connected directly to the Bacton Gas Terminal in Norfolk by two pipelines.

The principal fishing activity in the area is part of the Leman Ground fishing area with trawling in the deeps between the mega ripple shoals for white fish such as cod and whiting and flat fish such as sole and plaice by beam trawlers There is also shrimp fishing for brown and pink shrimp. The fishing in the character area is limited by the number of sea bed obstructions associated with gas exploitation.

Sea Use: Past

The Hewett 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 used this area because of it's proximity to the Outer Dowsing Navigation Channel to the west and 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 the Close's Fisherman's Chart (UKHO 1953) taken from surveys and reports from 1904 to 1925 and 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.

Archaeological Potential

The Hewett 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 areas position makes it a possible Upper Palaeolithic and Mesolithic habitation site. Over the last 6000 years (if not more), humans have used sea faring vessels and this area being close to a navigation channel (see above) has many wrecks. UKHO and NMR data show a total of 8 known wrecks in this area, 6 named. The Wrecks include the Hope sunk in 1811 and the Reinette sunk in 1919. Most of the wrecks, however, are from U Boat action in 1940 and 1941 and include the Paragon, Le Bijou and Success captured and sunk by mines together and other boats such as the Granta and Gardenia both sunk by U Boat action.

Character Perceptions

The area is perceived as an important industrial area as it contains the Hewett production field. It is also an offshore fishing ground with, at present, direct offshore industrial pressures from the gas fields in the area.

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)




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