Site of Special Scientific Interest | |
Location | Essex |
---|---|
Grid reference | TL 911243 |
Interest | Geological |
Area | 29.5 hectares |
Notification | 1986 |
Location map | Magic Map |
Marks Tey Brickpit is a 29.5-hectare (73-acre) geological Site of Special Scientific Interest in Marks Tey in Essex. [1] [2] It is a Geological Conservation Review site. [3]
This site has a record of pollen throughout the Hoxnian interglacial around 400,000 years ago, and this is the best vegetational record for any British interglacial site. Seasonal layers in lake sediments have made it possible to estimate the duration of the Hoxnian. [1] Clay deposited in the lake is quarried at a brickworks on the site, and this exposes layers above the Hoxnian ones of a later colder period. There is also a Grade II listed early nineteenth-century bottle kiln and brick tile works on the site. [4] [5]
The site is overgrown apart from a small area used for brick making. [4] It is private land with no public access, but a small area, which is now a field, can be seen from Marks Tey railway station car park.
The Essex Wildlife Trust (EWT) is one of 46 wildlife trusts which cover the United Kingdom. The EWT was founded in 1959, and it describes itself as Essex's leading conservation charity, which aims to protect wildlife for the future and the people of the county. As of January 2017, it has over 34,000 members and runs 87 nature reserves, 2 nature parks and 11 visitor centres.
The Hoxnian Stage was a middle Pleistocene stage of the geological history of the British Isles. It was an interglacial which preceded the Wolstonian Stage and followed the Anglian Stage. It is equivalent to Marine Isotope Stage 11. Marine Isotope Stage 11 started 424,000 years ago and ended 374,000 years ago. The Hoxnian is divided into sub-stages Ho I to Ho IV. It is likely equivalent to the Holstein Interglacial in Central Europe.
Hoxne is a village in the Mid Suffolk district of Suffolk, England, about five miles (8 km) east-southeast of Diss, Norfolk and 1⁄2 mile (800 m) south of the River Waveney. The parish is irregularly shaped, covering the villages of Hoxne, Cross Street and Heckfield Green, with a 'tongue' extending southwards to take in part of the former RAF Horham airfield.
Colne Estuary is a 2915 hectare biological and geological Site of Special Scientific Interest near Brightlingsea in Essex. It is also a Nature Conservation Review site, a National Nature Reserve, a Ramsar wetland site of international importance, a Special Protection Area, a Special Area of Conservation, and a Geological Conservation Review site. Three areas in the site are managed by the Essex Wildlife Trust, Colne Point, Fingringhoe Wick and Howlands Marsh.
Swanscombe Skull Site or Swanscombe Heritage Park is a 3.9-hectare (9.6-acre) geological Site of Special Scientific Interest in Swanscombe, north-west Kent, England. It contains two Geological Conservation Review sites and a National Nature Reserve. The park lies in a former gravel quarry, Barnfield Pit, which is the most important site in the Swanscombe complex, alongside several other nearby pits.
Wansunt Pit is a 1.9-hectare (4.7-acre) geological Site of Special Scientific Interest in Dartford Heath between Crayford in the London Borough of Bexley and Dartford in Kent. It is also a Geological Conservation Review site. It is important geologically because it exposes the Dartford Heath Gravel, and the relationship of this exposure to the Swanscombe sequence and the Thames Terraces is a controversial issue in Thames Pleistocene studies. The site is part of Braeburn Park, a nature reserve managed by the London Wildlife Trust.
Oughtonhead Lane is a 0.9-hectare (2.2-acre) geological Site of Special Scientific Interest in Hitchin in Hertfordshire. The local planning authority is North Hertfordshire District Council. The site has been identified as of national importance in the Geological Conservation Review.
Bierton Clay Pit is a 0.07-hectare (0.17-acre) geological Site of Special Scientific Interest in Bierton in Buckinghamshire. It is listed by the Joint Nature Conservation Committee as a Geological Conservation Review site.
Purfleet Chalk Pits is a 10.7-hectare (26-acre) geological Site of Special Scientific Interest in Purfleet in Essex. It is a Geological Conservation Review site.
Purfleet Road, Aveley is a 4 hectare geological Site of Special Scientific Interest in Aveley in Essex.
Ardleigh Gravel Pit is a 1.2-hectare (3.0-acre) geological Site of Special Scientific Interest south of Ardleigh in Essex. It is a Geological Conservation Review site.
Wivenhoe Gravel Pit is a 2.1-hectare (5.2-acre) geological Site of Special Scientific Interest north of Wivenhoe in Essex. It is a Geological Conservation Review site.
Clacton Cliffs and Foreshore is a 26.1-hectare (64-acre) geological Site of Special Scientific Interest in Clacton-on-Sea in Essex. It is a Geological Conservation Review site.
Little Oakley Channel Deposit is a three-hectare geological Site of Special Scientific Interest in Little Oakley in Essex, England. It is a Geological Conservation Review site.
Lofts Farm Pit is a 4.5-hectare (11-acre) geological Site of Special Scientific Interest in Heybridge, a suburb of Maldon in Essex. It is a Geological Conservation Review site.
Newney Green Pit is a 0.07-hectare (0.17-acre) geological Site of Special Scientific Interest west of Writtle in Essex. It is a Geological Conservation Review site.
Hoxne Brick Pit is a 1.3-hectare (3.2-acre) geological Site of Special Scientific Interest in Hoxne in Suffolk, England. It is a Geological Conservation Review site.
Holkham Brick Pit is a 0.5-hectare (1.2-acre) geological Site of Special Scientific Interest west of Wells-next-the-Sea in Norfolk. It is a Geological Conservation Review site, and it is in the Norfolk Coast Area of Outstanding Natural Beauty.
Sugworth is a 0.6-hectare (1.5-acre) geological Site of Special Scientific Interest north of Abingdon-on-Thames in Oxfordshire. It is a Geological Conservation Review site.