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
46 Eagle Wharf Road
London
N1 7ED
UK
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

Rough Character Area

Present Day Form

The Rough offshore character area is situated in the north-western section of the study area off the east coast of East Yorkshire. 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 15m and 32m and the maximum tidal range is 2-3m. The seabed is rough gravel and rocks probably derived from the glacial till. The Silver Pit palaeochannel runs through the centre of Rough.

Sea Use: Present

The dominant character of Rough is gas related industry although some fishing does take place in the area. The Rough gas field was discovered in 1968 and started production in 1983. Along with the Mercury and Helvellyn fields it has reserves of some 15 billion cubic metres of gas and a peak production of 1 billion cubic metres of gas per year. It is one of the southern North Sea's larger hydrocarbon fields with permanent installations both on the seabed and free standing rigs. The field is connected directly to the Easington Gas Terminal in East Yorkshire by pipeline. Fishing activity in the area is limited by the rough nature of the sea bed and the gas industry infrastructure. Commercial shipping crosses the area on a regular basis. The fishing in the character area is limited by the number of sea bed obstructions associated with gas exploitation.

Sea Use: Past

The Rough 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 crossed this area on a regular basis from the Roman period onwards utilising the North Sea route from the Humber ports. Fishing activity would have been carried out in the area from the medieval period onwards. The Close's Fisherman's Chart (UKHO 1953) describes the area as mostly foul and very foul off the Humber.

Archaeological Potential

The Rough 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 adjacent to the Silver Pit channel makes it a prime Mesolithic habitation area. Consequently, there is some potential for surviving evidence of human activity within the area along the margins of this channel with less likely survival beyond this.

Over the last 6000 years (if not more), humans have used sea faring vessels and this area and wrecks and related material that may lie on the sea floor or be buried beneath the sea floor. UKHO and NMR data show a total of 15 known wrecks in this area, 5 unnamed and 10 named. Most of these lost vessels relate to World War One and two losses and reflect the large concentration of wrecks found in the sea off the Humber approaches and the importance of Hull and the Humber ports in the war effort. Typical of the losses are the Keynes and English collier sunk by bomb action in 1940, the Jersey an English trawler sunk in 1916 and the Modig a Norwegian collier mined in 1916.

Character Perceptions

The area is perceived as an important industrial area as it contains the Rough, Helvellyn and Mercury production fields. The area is a difficult area for fishing.

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)

NE Diary 1939-45; Incidents (online)




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