 | |
| Location | |
|---|---|
  Crossgates Quarry | |
| Location | Crossgates |
| County | North Yorkshire |
| Country | England |
| Coordinates | 54°14′32″N0°25′30″W / 54.242325°N 0.424996°W |
| Production | |
| Products | Limestone |
Crossgates Quarry is a disused limestone quarry in Crossgates, south of Scarborough, North Yorkshire, England.
The limestone of Crossgates Quarry is of the Corallian Group. It was said in 1892 that "most of [the] species [of Jurassic rock] in former times marked Scarborough have either come from this or Ayton Quarries." [1] Blake and Hudleston described the rock beds of the quarry as 2 feet of coral rag, 8 feet 1 inch of oolite and corals, 2 feet of the coral shell-bed, and 13 feet 2 inches of oolites. [2]
In 1901, J. A. Hargreaves of the Yorkshire Naturalists' Union, commented that "Crossgates quarry lies immediately below the Coral Rag, and although fossils are numerous, it is almost impossible to extract them from the surrounding matrix." [3]
Crossgates Quarry appears on maps as early as 1854, along with 11 lime kilns in the vicinity. [4] In 1857, Anglo-Saxon human remains were found at the quarry and investigated by Lord Londesborough. [5]
The quarry was home to a lime works. In 1932, there was a fire at an engine shed there, which was attended by Scarborough fire brigade and Viscount Downe's private fire brigade from Wykeham Abbey. Scarborough fire brigade did not attempt to put out the fire as they had no agreement to operate outside the borough. [6] Residents near the quarry complained of noise in 1961 when a new plant was being installed. [7]
In 1983, the quarry was mooted as a potential development site for housing, agriculture, or commerce. [8]
Quarries in North Yorkshire | ||
|---|---|---|
| Active quarries in North Yorkshire |  | |
| Inactive quarries in North Yorkshire | ||
| Notes |
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The North York Moors is an upland area in north-eastern Yorkshire, England. It contains one of the largest expanses of heather moorland in the United Kingdom. The area was designated as a National Park in 1952, through the National Parks and Access to the Countryside Act 1949. Covering an area of 554 sq mi (1,430 km2), the National Park has a population of 23,380. It is administered by the North York Moors National Park Authority, which is based in Helmsley.
The Derwent is a river in Yorkshire in the north of England. It flows from Fylingdales Moor in the North York Moors National Park, east then southwards as far as its confluence with the River Hertford then westwards through the Vale of Pickering, south through Kirkham Gorge and the Vale of York, joining the River Ouse at Barmby on the Marsh. The confluence is unusual in that the Derwent converges on the Ouse at a shallow angle in an upstream direction.
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Dorset is a county in South West England on the English Channel coast. Covering an area of 2,653 square kilometres (1,024 sq mi); it borders Devon to the west, Somerset to the north-west, Wiltshire to the north-east, and Hampshire to the east. The great variation in its landscape owes much to the underlying geology, which includes an almost unbroken sequence of rocks from 200 to 40 million years ago (Mya) and superficial deposits from 2 Mya to the present. In general, the oldest rocks appear in the far west of the county, with the most recent (Eocene) in the far east. Jurassic rocks also underlie the Blackmore Vale and comprise much of the coastal cliff in the west and south of the county; although younger Cretaceous rocks crown some of the highpoints in the west, they are mainly to be found in the centre and east of the county.
The Vale of Pickering is a low-lying flat area of land in North Yorkshire, England. It is drained by the River Derwent. The landscape is rural with scattered villages and small market towns. It has been inhabited continuously from the Mesolithic period. The present economy is largely agricultural with light industry and tourism playing an increasing role.
Somerset is a rural county in the southwest of England, covering 4,171 square kilometres (1,610 sq mi). It is bounded on the north-west by the Bristol Channel, on the north by Bristol and Gloucestershire, on the north-east by Wiltshire, on the south-east by Dorset, and on the south west and west by Devon. It has broad central plains with several ranges of low hills. The landscape divides into four main geological sections from the Silurian through the Devonian and Carboniferous to the Permian which influence the landscape, together with water-related features.
Carboniferous Limestone is a collective term for the succession of limestones occurring widely throughout Great Britain and Ireland that were deposited during the Dinantian Epoch of the Carboniferous Period. These rocks formed between 363 and 325 million years ago. Within England and Wales, the entire limestone succession, which includes subordinate mudstones and some thin sandstones, is known as the Carboniferous Limestone Supergroup.
Oswaldkirk is a small village and civil parish 4 miles (6.4 km) south of Helmsley and 20 miles (32 km) north of York in North Yorkshire, England. It is named after the village church of St Oswald, King and Martyr, the Anglo-Saxon King of Northumbria who was slain by the pagan, Penda in 642. There was previously a Catholic church, dedicated to St Aidan, which closed in 2020. The population of the village as taken at the 2011 census was 230.
Seamer is a village and civil parish in the Scarborough district of North Yorkshire, England. It was the location of the Mesolithic Age settlement of Star Carr.
Wilfred Hudleston Hudleston was an English geologist, ornithologist and paleontologist.
Coral rag is a rubbly limestone composed of ancient coral reef material. The term also refers to the building blocks quarried from these strata, which are an important local building material in areas such as the coast of East Africa and the southeastern United States littoral.
Levitt Hagg is an abandoned hamlet in South Yorkshire, located approximately two miles southwest of Doncaster and near Conisbrough Castle. Limestone began to be quarried at the site in ancient times. Levitt Hagg was also the site, along with nearby environs in the Don Gorge, of ancient woodlands rich in yew trees. The old settlement of Levitt Hagg was removed in the 1950s.
The Inferior Oolite is a sequence of Jurassic age sedimentary rocks in Europe. It was deposited during the Middle Jurassic. The Inferior Oolite Group as more recently defined is a Jurassic lithostratigraphic group in southern and eastern England. It has been variously known in the past as the Under Oolite, the Inferior Oolite, the Inferior Oolite Series and the Redbourne Group.
The Hambleton Hills are a range of hills in North Yorkshire, England. They form the western edge of the North York Moors but are separated from the moors by the valley of the River Rye. They are the eastern boundary of the low-lying Vale of Mowbray which they abut with a precipitous escarpment.
Hadspen Quarry is a stone quarry in Somerset, England. It is shown on Ordnance Survey maps for 1888–90, and may have been in operation for a considerable period before that.
The Corallian Group or Corallian Limestone is a geologic group in England. It is predominantly a coralliferous sedimentary rock, laid down in the Oxfordian stage of the Jurassic. It is a hard variety of "coral rag". Building stones from this geological structure tend to be irregular in shape. It is often found close to seams of Portland Limestone. It is a younger limestone than its near-neighbour, the Oolitic, as found in the Cotswolds, in Gloucestershire. It is laterally equivalent to and interfingers with units of the Ancholme Group.
Crossgates is a village in the Borough of Scarborough, North Yorkshire, England, situated between Seamer to the west and Eastfield to the east separating the A64 and the B1261 roads which intersect there. Seamer railway station is situated in Crossgates.
Finedon Top Lodge Quarry, also known as Finedon Gullet is a 0.9-hectare (2.2-acre) geological Site of Special Scientific Interest east of Wellingborough in Northamptonshire. It is a Geological Conservation Review site revealing a sequence of middle Jurassic limestones, sandstones and ironstones, and is the type section for a sequence of sedimentary rocks known as the 'Wellingborough Member'. It was created by quarrying for the underlying ironstone for use at Wellingborough and Corby Steelworks; the ore was transported by the 1,000 mm gauge Wellingborough Tramway.
The Coralline Oolite Formation is a limestone formation of Oxfordian age, found in the Cleveland Basin of North Yorkshire, England.
The geology of the North York Moors National Park in northern England is provided largely by a thick southerly dipping sequence of sedimentary rocks deposited in the Cleveland Basin during the Jurassic Period. A series of ice ages during the Quaternary period has left a variety of glacial deposits, particularly around the margins of the National Park.