Stony Furlong Railway Cutting

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Stony Furlong Railway Cutting
Site of Special Scientific Interest
Gloucestershire UK location map.svg
Red pog.svg
Location within Gloucestershire
Area of Search Gloucestershire
Grid reference SP063106
Coordinates 51°47′40″N1°54′34″W / 51.794466°N 1.909329°W / 51.794466; -1.909329 Coordinates: 51°47′40″N1°54′34″W / 51.794466°N 1.909329°W / 51.794466; -1.909329
Interest Geological
Area 2.7 hectare
Notification 1987
Natural England website

Stony Furlong Railway Cutting (grid reference SP063106 ) is a 2.7-hectare (6.7-acre) geological Site of Special Scientific Interest in Gloucestershire, notified in 1987. [1] [2] The site is listed in the 'Cotswold District' Local Plan 2001-2011 (on line) as a Key Wildlife Site (KWS) and a Regionally Important Geological Site (RIGS). [3] [4]

Ordnance Survey National Grid System of geographic grid references used in Great Britain

The Ordnance Survey National Grid reference system is a system of geographic grid references used in Great Britain, distinct from latitude and longitude. It is often called British National Grid (BNG).

Gloucestershire County of England

Gloucestershire is a county in South West England. The county comprises part of the Cotswold Hills, part of the flat fertile valley of the River Severn, and the entire Forest of Dean.

Contents

Location and geology

The site is located in east Gloucestershire, near Chedworth, and is significant as it shows an important section through the White Limestone (Bathonian, Middle Jurassic period). It is unique in the area for exhibition of the Shipton Member. The exposure demonstrates the south west passage of the Hampen Marly Beds. This links with similar exposures in Wiltshire, Oxfordshire and eastern Gloucestershire. [1]

Chedworth village in the United Kingdom

Chedworth is a village and civil parish in Gloucestershire, southwest England, in the Cotswolds and is known as the location of Chedworth Roman Villa, administered since 1924 by the National Trust.

Limestone Sedimentary rocks made of calcium carbonate

Limestone is a sedimentary rock which is often composed of the skeletal fragments of marine organisms such as coral, foraminifera, and molluscs. Its major materials are the minerals calcite and aragonite, which are different crystal forms of calcium carbonate (CaCO3).

The Jurassic was a geologic period and system that spanned 56 million years from the end of the Triassic Period 201.3 million years ago (Mya) to the beginning of the Cretaceous Period 145 Mya. The Jurassic constitutes the middle period of the Mesozoic Era, also known as the Age of Reptiles. The start of the period was marked by the major Triassic–Jurassic extinction event. Two other extinction events occurred during the period: the Pliensbachian-Toarcian extinction in the Early Jurassic, and the Tithonian event at the end; however, neither event ranks among the "Big Five" mass extinctions.

The site has produced significant findings of ammonites and a rarity of the morruisi Zone. [1]

The site is a significant research resource. [1]

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References

SSSI Source