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Somerset is a rural county in the southwest of Englandcovering 4, square kilometres 1, sq mi. It is bounded on the north-west Web cam singles in Kilve the Bristol Channelon the north by Bristol and Gloucestershireon the north-east by Wiltshireon the south-east by Dorsetand 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.

The low-lying areas of the North Somerset Levels and Somerset Levels have been subject to thousands of years of flooding and man's attempts to control the flow of water. In the north of the county the Limestone of the Mendip Hills dominates the landscape, while in the south the Blackdown and Quantock Hills rise out of the levels.

The highest areas are on Exmoor. The wide variety of landscapes has led to several areas being deated as Sites of Special Scientific Interest for geological reasons, and support a range of flora and fauna as can be seen from the List of Sites of Special Scientific Interest in Somerset. The oldest rocks are of Silurian age — million years agothe most southerly known outcrop of rocks of this age in Britain.

They make up a sequence of lavastuffs volcanic ashshales and mudstones in a narrow outcrop to the northeast of Shepton Malletin the eastern Mendip Hills. Rocks from the Devonian — million years ago are found across much of Exmoor[2] the Quantocks including Hangman Sandstone and Cockercombe tuffand in the cores of the folded masses of the Mendip Hills.

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Carboniferous Period — million years ago rocks are represented by the Carboniferous Limestone that forms the Mendip Hills, rising abruptly out of the flat landscape of the Somerset Levels and Moors. The limestones are very fossiliferous, and contain evidence of the abundant marine life that existed at the time of their creation, including fossil crinoids sea-liliescorals and brachiopods.

At the end of the Permian — million years ago and Triassic periods, the Variscan orogeny resulted in the formation of several mountainous areas including Dartmoor in the south, Exmoor and the Quantocks, and the Mendips. In the Taunton area Permian — million years ago red sandstones and breccia outcrop, although rocks of Triassic age — million years ago underlie much of Somerset and form the solid geology of the Somerset Moors and Levels.

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The Triassic rocks consist of red marls, sandstones, breccias and conglomerates which spread over the older rocks. The Dolomitic Conglomerate is an old shingle beach of Keuper Marl age.

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The Rhaetic Beds are full of fossils due to invasion of the Jurassic Sea. The Lias consists of clays and limestones, the latter being quarried and are famous for their fossils. Blue Lias was burnt locally to provide a source of lime for making lime mortar. It is still used as a decorative building stone. Blue Lias is believed to have been quarried on the Polden Hills as early as the 15th century and was quarried in Puriton from the early 19th century untilwhen the local cement works closed.

Above the Lias is the Lower Oolite Series which are chiefly clays and oolitic limestone. The famous Bath Stone is obtained from the Great Oolite bed. Alluvial flats and peat bogs occupy much of the centre of Somerset. In prehistoric times the coastline of Somerset was very different from the present one, the sea level at the last glacial maximum being several hundred feet lower than today so that the Bristol Channel was almost non-existent.

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The Bristol Channel has one of the largest tidal ranges in the world, up to 12 metres 39 ft at Burnham-on-Sea for example, [8] behind only the Bay of Fundy and Ungava Bay [9] in Canada. Thus the present coastline is partly due to a belt of marine clay at the coast and partly due to seawalls built to reclaim areas ly flooded at high tide.

The main valleys between the hills are filled with alluvial deposits from the hills or sea. The county has many small riversmost of which flow into the Bristol Channel.

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Many of the latter rivers now have clysts the local name for a sluice [18] on them to control the sea, but formerly they were tidal for some way inland. The main exception to this is the River Parrettwhich still has a tidal bore. The courses of the rivers ParrettSomerset AxeBrue and Cary run across the Somerset Levels and have generally been changed to improve the flow.

The River Brue rises at Brewhamclose to the county border with Wiltshire.

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It flows through Bruton and is ed by the rivers Pitt and Alham. It flows south-west through Cary Moor to Cary Fitzpaine. It then used to turn south to the Parrett but now passes through Somerton Moor and crosses Kings Sedgemoor in an artificial channel, the King's Sedgemoor Draining the Parrett at Dunball north of Bridgwater. It enters Somerset at Haselbury Plucknett where it is ed by the Broad river. It flows south into Clatworthy reservoir and then to Greenham [25] where it changes course to go north-east to Taunton.

It then flows south to Exebridge where it meets the Barle and passes into Devon. Because of the nature of the Levels and Moors, the Poldens have a ificant visual impact. The Somerset Levels run from the coast up to 30 kilometres 19 mi inland.

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These wetlands cover square kilometres sq mimost of which is no higher than 8 metres 26 ft above sea level. The water levels in the moors and levels are controlled by a series of small narrow canals called rhynes known as 'rhines' in Avonmouth and Gloucestershire - both are pronounced 'reens'.

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The area is mainly used for grazing but some peat extraction is carried out. This is the area between the River Avon to the north and the Axe valley. The north of Somerset is dominated by the tableland of the Mendip Hillsan area of outstanding natural beautystretching from Frome in the east to Crook Peak in the west, with outliers of Bleadon Hill and Brean Down as well as Steep Holm in the Bristol Channel.

The highest point is Black Down at metres 1, ft. To the north of Bath are Lansdown, Langridge and Solsbury hills. These are outliers of the Cotswolds. The Old Red Sandstone is a series of red sandstonesmarls and conglomerates. It rises as an anticline in the Mendips and appears in the Avon Gorge and at Portishead. Carboniferous Limestoneof marine origin, covers the sandstone and appears in the Avon Gorge and at Weston-super-Mare where it contains volcanic rocks.

The main geological component of the Mendips is Carboniferous Limestone.

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It represents the remnants of a much higher range of hills that existed hundreds of millions years ago. Further east there are Silurian volcanoesCarboniferous Limestone outcrops, Variscan thrust tectonicsPermo-Triassic conglomerates, sediment-filled fissures, a classic unconformity, Jurassic clays and limestones, Cretaceous Greensand and chalk topped with Tertiary remnants including Sarsen Stones.

These sediments have yielded a fairly rich fossil fauna of brachiopods and trilobites indicating that they were deposited in a shallow marine sea into which the lavas were extruded.

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Coal measures appear in the Rtock district, and surrounding Somerset Coalfield largely concealed by Triassic and newer rocks. Locally the beds are folded and faulted. There were mines in the Rtock and Nailsea areas but these have closed. This was one of the first areas in the world to undergo systematic geological study and mapping by John Strachey and William Smith in the 18th century. The Mendips were mined for leadsilvercoalochrefuller's earth and zinc but this has finished.

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To the south of Somerset there is an upland with a series of rolling valleys and scarps, from Penselwood in the east to the Blackdown Hillsanother deated Area of Outstanding Natural Beauty, in the west. The Blackdowns are on the south-west border of Somerset, extending into Devon. They are composed of Upper Greensand. There is an open plateau, which is not as high as the Mendips.

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The Quantock Hills are a 20 kilometres 12 mi long broad ridge from the coast near Watchet in the north to near Taunton in the south. They reach metres 1, ft high at Wills Neck and are separated from Exmoor and the Brendons by a rift valley.

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The Quantocks and the Brendon Hills at the eastern end of Exmoor are formed by thick sequences of slates and sandstones of Devonian age that were deposited by large deltas that built out into a shallow sea. The Quantock Hills are largely formed by rocks of the Devonian Period, which consist of sediments originally laid down under a shallow sea and slowly compressed into solid rock.

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In the higher north western areas older Early Devonian rocks, known as Hangman Grits, [51] predominate, and can be seen in the exposed rock at West Quantoxhead quarry, which were worked for road building. These include sandstone and limestone, which have been quarried near Aisholt. The west side is cut by combes with broad valleys on the east.

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The hill tops are open heathland with woods on the slopes. Several areas have outcrops of slates and between St Audries and Kilveyounger rocks of the Jurassic Period can be found. Exmoor is a dissected plateau of Devonian sedimentary rock, rising to metres 1, ft at Dunkery Beacon. It extends into Devon but the majority of the area is in Somerset. Much of the area is a National Park. Because of high rainfall there are boggy areas and the part by the Chains is a Geological Conservation Review site recognised as being nationally important for its south-western lowland heath communities and for transitions from ancient semi-natural woodland through upland heath to blanket mire.

The Chains provides palynological record of a mid to late Flandrian vegetation history on Exmoor. The pollen sequence in the peat is calibrated by radiocarbon dating.

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As this area of Britain was not subject to glaciationthe plateau remains as a remarkably old landform. Exmoor has 55 kilometres 34 mi of coastline, including the highest cliffs in England, which reach a height of 1, feet m at Culbone Hill. If a cliff is defined as having a slope greater than 60 degrees, the highest cliff on mainland Britain is Great Hangman near Combe Martin at metres 1, ft high, with a cliff face of metres ft.

Exmoor's woodlands sometimes reach the shoreline, [67] especially between Porlock and The Forelandwhere they form the single longest stretch of coastal woodland in England and Wales. The high ground forms the catchment area for numerous rivers and streams.

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There are about miles km of named rivers on Exmoor. The river and the Barle Valley are both deated as biological sites of Special Scientific Interest. Another tributary, the River Haddeoflows from the Wimbleball Lake. The action of streams has cut combes through the hills down to the sea, which are now wooded, although much of Exmoor is open heathland.

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There is an outlier of Exmoor at North Hill near Minehead. Iron working was formerly carried out, probably from the Roman period onward. Because Exmoor was a royal foresti.

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