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River Sid
The River Sid, situated in East Devon, is often claimed to be the shortest complete river in England. It flows for southwards from a source in Crowpits Covert (OSGB36 Grid reference SY138963) at a height of 206 metres above sea level. Thsourceis at the head of a goyle or small ravine. The underlying geology is impermeable silty mudstones and sandstones of the Triassic Keuper marl, overlain with permeable Greensand and clay-with-flints. The junction between the Greensand and Keuper Marl forms a spring line. The river flows through Sidbury and Sidford to Sidmouth Sidmouth () is a town on the English Channel in Devon, South West England, southeast of Exeter. With a population of 12,569 in 2011, it is a tourist resort and a gateway to the Jurassic Coast World Heritage Site. A large part of the town h ... and is fed by springs flowing from East Hill and water from the Roncombe Stream, the Snod Brook and the Woolbrook. In Sidmouth the river outflows at the Ham through a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greensand
Greensand or green sand is a sand or sandstone which has a greenish color. This term is specifically applied to shallow marine sediment that contains noticeable quantities of rounded greenish grains. These grains are called ''glauconies'' and consist of a mixture of mixed-layer clay minerals, such as smectite and glauconite. Greensand is also loosely applied to any glauconitic sediment. Formation Greensand forms in anoxic marine environments that are rich in organic detritus and low in sedimentary input. Having accumulated in marine environments, greensands can be fossil-rich, such as in the late-Cretaceous deposits of New Jersey. Occurrence Important exposures are known from both northern and western Europe, North America, southeastern Brazil and north Africa. Well known and important greensands are the Upper and Lower Greensands of England and occur within Eocene and Cretaceous sedimentary strata underlying the coastal plains of New Jersey and Delaware. Although greensand ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sid Vale Association
The Sid Vale Association (SVA) is a voluntary conservation charity. It is headquartered in the coastal town of Sidmouth in the English county of Devon. Following the government's restructuring of the legal framework for charities the SVA was registered as CIO No 1154749 on 26 November 2013. It was the first Civic Society in Britain, founded in 1846 by John Carslake. It focuses on preserving and enhancing the civic fabric and the countryside of the Sid valley and encouraging public enjoyment of facilities in the valley. The Society owns over of the countryside surrounding Sidmouth and has done extensive work within and around the town especially around 'The Byes Walk' that runs from Sidford to Sidmouth Sidmouth () is a town on the English Channel in Devon, South West England, southeast of Exeter. With a population of 12,569 in 2011, it is a tourist resort and a gateway to the Jurassic Coast World Heritage Site. A large part of the town h .... Some of the association's ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sidmouth
Sidmouth () is a town on the English Channel in Devon, South West England, southeast of Exeter. With a population of 12,569 in 2011, it is a tourist resort and a gateway to the Jurassic Coast World Heritage Site. A large part of the town has been designated a conservation area. History The origins of Sidmouth pre-date recorded history. The Sid valley has been in human occupation since at least the Iron Age as attested by the presence of Sidbury Castle, and possibly earlier given the presence of Bronze Age burial mounds on Gittisham Hill and Broad Down. The village of Sidbury itself is known to be Saxon in origin with the Church crypt dating to the seventh century. However, the Sid Valley was divided into two ecclesiastical land holdings, with Sidbury and Salcombe Regis being gifted by King Athelstan to Exeter Cathedral, and Sidmouth, which was part of the manor of Otterton, was gifted by Gytha Thorkelsdóttir (the mother of King Harold Godwinson) to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sidford
Sidford is a small village in the civil parish of and on the outskirts of the town of Sidmouth in the England, English county of Devon. It has a population of just over 2,100 people according to the United Kingdom Census 2001, 2001 Census. The Church of England Church (building), Church, St Peter's, is part of the Sid Valley Mission. It gets its name from being on the River Sid, which runs for four miles into Lyme Bay at Sidmouth. One can walk along the river down the Byes into Sidmouth and to the sea. There is a 12th-century packhorse bridge over the river that was the site of a 1644 skirmish in the English Civil War. In the village centre there is a small Spar supermarket with a post office, a fish and chip shop, Bloaters. There is also a hairdresser, a sports injury clinic, a pub called the Rising Sun and a veterinary surgery. The Salty Monk opposite the Church is a sixteenth century building operated as a bed and breakfast. In sport, there is the Sidford Tennis Club, and Si ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sidbury
Sidbury is a large village north of Sidmouth on the A375 road in Devon, England. In 2011 the built-up area had a population of 457. In 1951 the civil parish had a population of 2,507. It is situated on the River Sid, which rises at Crowpits Covert (OSGB36 grid reference ) and runs for to Lyme Bay at Sidmouth. Above the village is Sidbury Castle, the site of an Iron Age hill fort. Sidbury is mentioned in the Domesday Book as the manor of Sideberia, held by Bishop Osbern of Exeter. The Church of St Peter and St Giles has a Norman tower topped with a spire, a Saxon crypt, a gunpowder storage room dating from the Napoleonic era and a 500-year-old font. The tower has eight bells, the earliest dating from 1662 and 1663. Six more were hung in 1712, 1750, 1752, 1776 and two in 1947 to complete the present eight. Both the tower and the rest of the church are Norman but the tower was accurately rebuilt in 1884. The north aisle is possibly 13th century and the south porch Perpendi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring Line Settlement
Spring line settlements occur where a ridge of permeable rock lies over impermeable rock, resulting in a line of springs along the contact between the two layers. Spring line (or springline) settlements will sometimes form around these springs, becoming villages. In each case to build higher up the hill would have meant difficulties with water supply; to build lower would have taken the settlement further away from useful grazing land or nearer to the floodplain. Spring line villages are often the principal settlements in strip parishes, with long, narrow parish boundaries stretching up to the top of the ridge and down to the river but being narrow in the direction of adjacent spring line villages. Some examples in England * to the north and south of the Howardian Hills in the North Riding of Yorkshire. * to the west and east of the ridge that stretches south from Lincoln and on top of which is the Roman road Ermine Street. The western line (which includes Boothby Graffoe and Na ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clay-with-flints
In geology, clay-with-flints was the name given by William Whitaker in 1861 to a peculiar deposit of stiff red, brown or yellow clay containing unworn whole flints as well as angular shattered fragments, also with a variable admixture of rounded flint, quartz, quartzite and other pebbles. Occurrence The Formation is associated with deposits of the Chalk Group, subsequent Palaeogene and Neogene strata, and occasionally Upper Greensand. It occurs in sheets or patches of various sizes over a large area in the south of England, from Hertfordshire on the north to Sussex on the south, and from Kent on the east to Devon on the west. It almost always lies on the surface of the Upper Chalk, but in Dorset Dorset ( ; archaically: Dorsetshire , ) is a county in South West England on the English Channel coast. The ceremonial county comprises the unitary authority areas of Bournemouth, Christchurch and Poole and Dorset. Covering an area of , ... it passes on to the Middle an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keuper Marl
Keuper marl is a former and now deprecated term for multiple layers of mudstone and siltstone of Triassic age which occur beneath parts of the English Midlands and neighbouring areas e.g. Cheshire, Nottinghamshire, Devon, eastern Worcestershire and northern Yorkshire. Typically red, or occasionally green or grey, these strata are generally featureless and contain few fossils. In basin formations, thick halite-bearing layers, or rock salt deposits, are sometimes present at the base of the marl. In modern nomenclature, Keuper marl is included within the Mercia Mudstone Group The Mercia Mudstone Group is an early Triassic lithostratigraphic group (a sequence of rock strata) which is widespread in Britain, especially in the English Midlands – the name is derived from the ancient kingdom of Mercia which corresponds to t .... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devon River Sid Weir
Devon ( , historically known as Devonshire , ) is a ceremonial and non-metropolitan county in South West England. The most populous settlement in Devon is the city of Plymouth, followed by Devon's county town, the city of Exeter. Devon is a coastal county with cliffs and sandy beaches. Home to the largest open space in southern England, Dartmoor (), the county is predominately rural and has a relatively low population density for an English county. The county is bordered by Somerset to the north east, Dorset to the east, and Cornwall to the west. The county is split into the non-metropolitan districts of East Devon, Mid Devon, North Devon, South Hams, Teignbridge, Torridge, West Devon, Exeter, and the unitary authority areas of Plymouth, and Torbay. Combined as a ceremonial county, Devon's area is and its population is about 1.2 million. Devon derives its name from Dumnonia (the shift from ''m'' to ''v'' is a typical Celtic consonant shift). During the B ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system (stratigraphy), system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago (Year#Abbreviations yr and ya, Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic, Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vert ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstones
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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