Hartlepool Submerged Forest

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Hartlepool Submerged Forest
Image Hartlepoolsubmergedforest.jpg
The site of the submerged forest in 2007
Durham UK relief location map.jpg
Red pog.svg
Location Hartlepool, County Durham, England
Coordinates 54°40′34″N1°11′34″W / 54.67611°N 1.19278°W / 54.67611; -1.19278
Area19.7 ha (49 acres)
Established1988
Governing bodyNatural England
Website Map of site

Hartlepool Submerged Forest (grid reference NZ520315 ) is a 19.7 hectare geological Site of Special Scientific Interest in County Durham, England notified in 1988. The site is located to the south of Hartlepool Docks.

Contents

SSSIs are designated by Natural England, formally English Nature, which uses the 1974–1996 county system. This means there is no grouping of SSSIs by Hartlepool unitary authority, or County Durham which is the relevant ceremonial county . As such Hartlepool Submerged Forest is one of 18 SSSIs in the Cleveland area of search. [1]

A forest stretching for several miles along the Hartlepool coast is thought to have originated around 7,000 years ago. It became submerged as sea levels rose over the next five millennia, but remains preserved to this day as a peaty soil, intermittently revealed on the foreshore by the ebb and flow of the tide. Animal bones, including those of deer and wild boar have been discovered at the site, as well as flint tools and other implements pointing to human activity in the area thousands of years ago. These have been analysed by scientists hoping to understand the environment that existed in the area before the forest was submerged.

The site is also considered to be of significant importance in understanding sea level and environmental changes since the last ice age, and is identified as such in the Geological Conservation Review.

Related Research Articles

Briarcroft Pasture is a 1.76 hectare biological Site of Special Scientific Interest in County Durham, England notified in 2004.

Cowpen Marsh is a 116.8 hectare biological Site of Special Scientific Interest in County Durham, England, notified in 1966. SSSIs are designated by Natural England, formally English Nature, which uses the 1974–1996 county system. This means there is no grouping of SSSIs by Stockton-on-Tees unitary authority, or County Durham which is the relevant ceremonial county. As such Cowpen Marsh is one of 18 SSSIs in the Cleveland area of search.

Hart Bog is a 1.79 hectare biological Site of Special Scientific Interest in County Durham, England notified in 1968.

Seal Sands is a 294.37 hectare biological Site of Special Scientific Interest in County Durham, England, notified in 1966.

<span class="mw-page-title-main">Durham Coast</span>

The Durham Coast is a Site of Special Scientific Interest in County Durham, England. Starting just North of the River Tees estuary it extends, with a few interruptions, northward to the mouth of the River Tyne at South Shields. Notable locations on the Durham Coast include Hartlepool Headland, Seaham, Sunderland Docks and Whitburn Beach.

Whitton Bridge Pasture is a Site of Special Scientific Interest (SSSI) in the unitary authority of Stockton-on-Tees, England. At 3.18 hectares (7.9 acres) it lies to the south of Whitton village and north west of Stockton-on-Tees. SSSIs are chosen by Natural England, and Whitton Bridge Pasture was designated in 2004 because of its biological interest. It is one of 18 SSSIs in the Cleveland area of search.

Seaton Dunes and Common is a 312.1 hectare biological Site of Special Scientific Interest in Hartlepool, County Durham, England notified in 1966. Part of it is a Local Nature Reserve.

Redcar Rocks is a 31.1 hectare biological and geological Site of Special Scientific Interest in North Yorkshire, England notified in 1984.

Tees and Hartlepool Foreshore and Wetlands SSSI is a 255.62-hectare (631.7-acre) biological Site of Special Scientific Interest in County Durham, England notified in 1997.

The geology of County Durham in northeast England consists of a basement of Lower Palaeozoic rocks overlain by a varying thickness of Carboniferous and Permo-Triassic sedimentary rocks which dip generally eastwards towards the North Sea. These have been intruded by a pluton, sills and dykes at various times from the Devonian Period to the Palaeogene. The whole is overlain by a suite of unconsolidated deposits of Quaternary age arising from glaciation and from other processes operating during the post-glacial period to the present. The geological interest of the west of the county was recognised by the designation in 2003 of the North Pennines Area of Outstanding Natural Beauty as a European Geopark.

References

  1. "SSSIs in Cleveland area of search". English Nature. Retrieved 31 January 2007.

Sources