Misplaced Pages

#908091

101-631: Black Rock Gorge is a deep and narrow cleft in Old Red Sandstone conglomerate through which the Allt Graad (also known as the 'River Glass') flows in Easter Ross , Scotland . It was caused by rapids heavily burdened with sediment being carried upwards as part of the great Post-glacial rebound . It lies a few kilometres from Evanton , at the edge of the Evanton Wood in the traditional territory of

202-794: A Celtic nation . The South West is known for Cheddar cheese , which originated in the Somerset village of Cheddar ; Devon cream teas , crabs , Cornish pasties , and cider . It is home to the Eden Project , Aardman Animations , the Glastonbury Festival , the Bristol International Balloon Fiesta , trip hop music and Cornwall's surfing beaches. The region has also been home to some of Britain's most renowned writers, including Daphne du Maurier , Agatha Christie and Enid Blyton , all of whom set many of their works here, and

303-632: A Local Transport Plan (LTP) which outlines their strategies, policies and implementation programme. The most recent LTP is that for the period 2006–11. In the South West region the following transport authorities have published their LTP online: Bournemouth U.A., Cornwall U.A., Devon , Dorset , Gloucestershire , Plymouth U.A., Somerset , Swindon U. A., Torbay U. A. and Wiltshire unitary authority . The transport authorities of Bath and North East Somerset U. A., Bristol U. A., North Somerset U. A. and South Gloucestershire U. A. publish

404-514: A boat trip from Dunglass Burn east along the coast with the geologist Sir James Hall of Dunglass and at Siccar Point found what Hutton called "a beautiful picture of this junction washed bare by the sea", where 345-million-year-old Old Red Sandstone overlies 425-million-year-old Silurian greywacke . In the early 19th century, the paleontology of the formation was studied intensively by Hugh Miller , Henry Thomas De la Beche , Roderick Murchison , and Adam Sedgwick —Sedgwick's interpretation

505-560: A combination of dunes , and sediments that may have been laid down in lakes , river , estuaries, and possibly other coastal environments. The Old Red Sandstone was long thought to have been deposited mostly in freshwater, but more recent studies have discovered marine fossils (such as brachiopods ) in some locations, its vertebrate fauna also occurs in typically marine environments, and an isotopic study also found significant marine influence in mineralised tissues of its vertebrates. Thus, at least some strata appear to have been deposited on

606-515: A cultural and historic unity or identity of itself, which has led to criticism of it as an "artificial" construct. The large area of the region, stretching as it does from the Isles of Scilly to Gloucestershire, encompasses diverse areas which have little more in common with each other than they do with other areas of England. The region has several TV stations and newspapers based in different areas, and no single acknowledged regional "capital". Many people in

707-417: A few of whom appear to have been descended from pre-Conquest families. In 1140, during the civil war of King Stephen 's reign, the castles of Plympton and Exeter were held against the king by Baldwin de Redvers and this gave rise to the defensive castles at Corfe Castle , Powerstock , Wareham and Shaftesbury . The period saw the growth of towns such as Truro , Totnes , Okehampton and Plympton in

808-823: A higher proportion of people live in such areas than in any other English region. There are two major regional cities in terms of population, which are Bristol and Plymouth (although Bristol is larger by some consideration), and two major conurbations which are the South East Dorset Conurbation (Bournemouth, Christchurch and Poole) and the Bristol Metropolitan Conurbation (which includes the City of Bristol and areas of South Gloucestershire). Cities and Towns with specific tourist and cultural sites of interest include Bath, Bristol, Salisbury, Plymouth, Exeter, Cheltenham, Gloucester and Weston-super-Mare, as well as

909-757: A military road, or Herepath , to allow his army to cover Viking movements at sea. The Herepath has a characteristic form which is familiar on the Quantocks: a regulation 20 m wide track between avenues of trees growing from hedge laying embankments. A peace treaty with the Danes was signed at Wedmore and the Danish king Guthrum the Old was baptised at Aller . Burhs (fortified places) had been set up by 919, such as Lyng . The Alfred Jewel , an object about 2.5-inch (64 mm) long, made of filigree gold, cloisonné -enamelled and with

1010-507: A narrow zone from Dulas Bay on Anglesey's northeast coast, southwards to the town of Llangefni . In 1787 James Hutton noted what is now known as Hutton's Unconformity at Inchbonny, Jedburgh , and in early 1788 he set off with John Playfair to the Berwickshire coast and found more examples of this sequence in the valleys of the Tower and Pease Burns near Cockburnspath . They then took

1111-582: A number of distinct sedimentary basins throughout Britain has been established. The Orcadian Basin extends over a wide area of North East Scotland and the neighbouring seas. It encompasses the Moray Firth and adjoining land areas, Caithness, Orkney and parts of Shetland . South of the Moray Firth, two distinct sub-basins are recognized at Turriff and at Rhynie . The sequence is more than 4 kilometres (13,000 ft) thick in parts of Shetland. The main basin

SECTION 10

#1732872734909

1212-499: A rock crystal covering, was found in 1693 at Petherton Park , North Petherton . This is believed to have been owned by King Alfred. Monasteries and minster churches were set up all over Somerset, with daughter churches of the minsters in manors. There was a royal palace at Cheddar , which was used at times in the 10th century to host the Witenagemot . In the late pre-Norman period, the east coast of modern-day England came under

1313-531: A single Joint Local Transport Plan as part of the West of England Partnership . There is evidence from flint artefacts in a quarry at Westbury-sub-Mendip that an ancestor of modern man, possibly Homo heidelbergensis , was present in the future Somerset from around 500,000 years ago. There is some evidence of human occupation of southern England before the last ice age , such as at Kents Cavern in Devon, but largely in

1414-533: A temporary Roman occupation. The massacre at Cadbury Castle seems to have been associated with the later Boudiccan Revolt of AD 60–61. The Roman invasion, and possibly the preceding period of involvement in the internal affairs of the south of England, was inspired in part by the lead mines of the Mendip Hills , which also offered the potential for the extraction of silver. Forts were set up at Bath and Ilchester . The lead and silver mines at Charterhouse in

1515-605: A yearly tribute or danegeld to Sweyn and later Canute, all three areas retained their autonomy from the Danes. Ultimately, the Danes lost control of Wessex in 1042 on the death of both of Canute's sons. Edward the Confessor retook Wessex for the Saxons. In 1016 Edmund Ironside was crowned king at Glastonbury. After the Norman Conquest the region was controlled by various Norman as well as Breton lords and later by local gentry,

1616-512: Is a stub . You can help Misplaced Pages by expanding it . Old Red Sandstone The Old Red Sandstone describes a group of sedimentary rocks deposited in a variety of environments in the late Silurian , through the Devonian and into the earliest part of the Carboniferous . The body of rock , or facies , is dominated by terrigenous deposits and conglomerates at its base, and progresses to

1717-969: Is a continuous outcrop along the Highland Boundary Fault from Stonehaven on the North Sea coast to Helensburgh and beyond to Arran . A more disconnected series of outcrops occur along the line of the Southern Uplands Fault from Edinburgh to Girvan . Old Red Sandstone often occurs in conjunction with conglomerate formations, one such noteworthy cliffside exposure being the Fowlsheugh Nature Reserve , Kincardineshire . A series of outcrops occur from East Lothian southwards through Berwickshire . Hutton's famous unconformity at Siccar Point occurs within this basin - see History of study below. This relatively large basin extends across much of South Wales from southern Pembrokeshire in

1818-568: Is classed as oceanic ( Cfb ) according to the Köppen climate classification . The oceanic climate typically experiences cool winters with warmer summers and precipitation all year round, with more experienced in winter. Annual rainfall is about 1,000 millimetres (39 in) and up to 2,000 millimetres (79 in) on higher ground. Summer maxima averages range from 18 °C (64 °F) to 22 °C (72 °F) and winter minimum averages range from 1 °C (34 °F) to 4 °C (39 °F) across

1919-700: Is considered to be an intramontane basin resulting from crustal rifting associated with post-Caledonian extension , possibly accompanied by strike-slip faulting along the Great Glen Fault system. There are a scatter of exposures of the Old Red Sandstone around Oban and the Isle of Kerrera on the West Highland coast, this unit is sometimes referred to as the Kerrera Sandstone Formation. The unit

2020-644: Is currently the only county in the region where there are electric trains, though the Great Western Main Line and the South Wales Main Line in Wiltshire, Somerset, Greater Bristol and Gloucestershire is being electrified . SWR operate services to and from London Waterloo and serves every county in the region except Gloucestershire and Cornwall. GWR serves all counties in the region and operate to various destinations, some of which run to South Wales and

2121-466: Is generally considered that Cornwall came fully under the dominion of the English Crown in the time of Athelstan 's rule, i.e. 924–939. In the absence of any specific documentation to record this event, supporters of Cornwall's English status presume that it then became part of England. However, in 944, within a mere five years of Athelstan's death, King Edmund issued a charter styling himself "King of

SECTION 20

#1732872734909

2222-431: Is merely an erosional contact incorporating debris of the slate in a basal conglomerate. The ORS deposits around Oban are considered latest Silurian ( Pridoli ) to earliest Devonian in age. They are interpreted as alluvial fans which filled a depositional basin from the east and northeast. Small outliers occur near Taynuilt and either side of Loch Avich . The deposits are especially obvious on Kerrera where they form

2323-698: Is represented by the Gupton and West Angle formations. The Freshwater East Formation, and corresponding Red Cliff Formation of north Pembrokeshire, are both late Silurian in age. A small and separate basin exists here where both alluvial and lacustrine deposits are recorded. Both the middle and upper ORS are missing but the lower ORS is represented, in ascending order, by the Bodafon, Traeth Bach, Porth y Mor and Traeth Lligwy formations. Calcretes are also recorded representing carbonate-rich soils developed between periods of sediment deposition. The present day outcrop occupies

2424-475: Is up to 128m thick in its type area and consists of green and red sandstones and conglomerates, typically containing large (10–30 cm or 4–12 in across) elliptical well rounded clasts, accompanied by siltstones, mudstones and limestones. On Kerrera a conglomerate of andesite boulders rests unconformably on Dalradian black, pyritic slates ( Easdale Slate) of the Easdale Subgroup . At Oban there

2525-512: The Battle of Lose-coat Field . The organisation of the region remained based on the shires and Church estates, which were largely unchanged throughout the period. Some of the most important nobles in the South West included the Courtenays Earl of Devon, William Bonville, 1st Baron Bonville , and Humphrey Stafford, earl of Devon whose wider influence stretched from Cornwall to Wiltshire. After 1485,

2626-512: The Clan Munro . The Black Rock Gorge is approximately 1.5 km in length as shown on 1:50 000 Ordnance Survey mapping and reaches 36 metres (120 feet) in depth. It attracts a substantial amount of tourism, and there is a camping site nearby. The gorge is the subject of local Gaelic myth, in which a local noblewoman, the Lady of Balconie , is lured into its depths by a mysterious man, thought to be

2727-673: The Danelaw . Sweyn ruled Wessex, along with his other realms, from 1013 onwards, followed by his son Canute the Great . But Cornwall was not part of his realm of Wessex. A map by the American historian called "The Dominions of Canute" (pictured just above) shows that Cornwall, like Wales and Scotland, was part neither of Sweyn Forkbeard's nor of Canute's Danish empire. Neither Sweyn Forkbeard nor Canute conquered or controlled Scotland, Wales or Cornwall; but these areas were "client nations": subject to payment of

2828-598: The Devil . Ever since, it is said, the cries which she utters can be heard from the top. In April 2004, ten days of filming took place in the area for the movie Harry Potter and the Goblet of Fire and the gorge is the setting for one scene. Also James Robertson's 2006 novel The Testament of Gideon Mack is inspired by Black Rock Gorge. 57°40′0″N 4°22′12″W  /  57.66667°N 4.37000°W  / 57.66667; -4.37000 This Highland location article

2929-612: The Devon border to the mouth of the River Axe . Historically, the main port on the river was at Bridgwater; the river being bridged at this point, with the first bridge being constructed in 1200. Quays were built in 1424; with another quay, the Langport slip , being built in 1488 upstream of the Town Bridge. In Bristol the port began to develop in the 11th century. By the 12th century Bristol

3030-620: The Frome Hoard , one of the largest ever hoards of Roman coins discovered in Britain, was found by a metal detectorist. The hoard of 52,500 coins dated from the 3rd century AD and was found buried in a field near Frome , in a jar 14 inches (36 cm) below the surface. The coins were excavated by archaeologists from the Portable Antiquities Scheme . After the Romans left at the start of

3131-482: The Mendip Hills . The human bone fragments it contained, from about 21 different individuals, are thought to be roughly between 10,200 and 10,400 years old. During this time the tundra gave way to birch forests and grassland and evidence for human settlement appears at Salisbury Plain , Wiltshire and Hengistbury Head , Dorset. At the end of the last Ice Age the Bristol Channel was dry land, but subsequently

Black Rock Gorge - Misplaced Pages Continue

3232-669: The New Forest is also within the region); and four World Heritage Sites : Stonehenge , the Cornwall and West Devon Mining Landscape , the Jurassic Coast and the City of Bath . The northern part of Gloucestershire, near Chipping Campden , is as close to the Scottish border as it is to the tip of Cornwall. The region has by far the longest coastline of any English region. Following the abolition of

3333-778: The Pagans Hill Roman Temple at Chew Stoke . In October 2001 the West Bagborough Hoard of 4th-century Roman silver was discovered in West Bagborough . The 681 coins included two denarii from the early 2nd century and 8 miliarensia and 671 siliquae all dating from AD 337 to 367. The majority were struck in the reigns of emperors Constantius II and Julian and derive from a range of mints including Arles and Lyons in France, Trier in Germany, and Rome. In April 2010,

3434-708: The Plateau Beds Formation is unconformably overlain by the Grey Grits Formation though further east these divisions are replaced by the Quartz Conglomerate Group which is itself subdivided into a variety of different formations. The sequence in Pembrokeshire differs from that of the main part of the basin and falls into two parts. In North Pembrokeshire to the north of the Ritec Fault , both

3535-530: The Purbeck Hills . These downs are the principal area of arable agriculture in the region. Limestone is also found in the region, at the Cotswolds , Quantock Hills and Mendip Hills , where they support sheep farming. All of the principal rock types can be seen on the Jurassic Coast of Dorset and East Devon, where they document the entire Mesozoic era from west to east. The climate of South West England

3636-492: The Roman baths . Excavations carried out before the flooding of Chew Valley Lake also uncovered Roman remains, indicating agricultural and industrial activity from the second half of the 1st century until the 3rd century AD. The finds included a moderately large villa at Chew Park, where wooden writing tablets (the first in the UK) with ink writing were found. There is also evidence from

3737-557: The South West Regional Assembly in 2008 and Government Office in 2011, South West Councils provide local government coordination in the region. Bristol , South Gloucestershire , and Bath and North East Somerset are part of the West of England Combined Authority . The region is known for its rich folklore , including the legend of King Arthur and Glastonbury Tor , as well as its traditions and customs. Cornwall has its own language, Cornish , and some regard it as

3838-510: The West Midlands through Gloucestershire, Bristol and Somerset to Exeter. The A38 serves as a western extension to Plymouth. There are three other smaller motorways in the region, all in the Bristol area . Passenger airports in the region include Bristol , Exeter , Newquay and Bournemouth . Within the region the local transport authorities carry out transport planning through the use of

3939-456: The science of stratigraphy 's early debates were about the Old Red Sandstone. In older geological works predating theories of plate tectonics , the United States' Catskill Delta formation is sometimes referred to as part of the Old Red Sandstone. In the modern day it is recognized that the two are not stratigraphically continuous but are very similar due to being formed at approximately

4040-464: The south east . The British mainland was connected to the continent during the ice age and humans may have repeatedly migrated into and out of the region as the climate fluctuated. There is evidence of human habitation in the caves at Cheddar Gorge 11,000–10,000 years BC, during a partial thaw in the ice age. The earliest scientifically dated cemetery in Great Britain was found at Aveline's Hole in

4141-471: The 1930s for civil defence administration and subsequently used for various statistical analyses. The region is also similar to that used in the 17th-century Rule of the Major-Generals under Cromwell . (For further information, see Historical and alternative regions of England ). By the 1960s, the South West region (including Dorset, which for some previous purposes had been included in a Southern region),

Black Rock Gorge - Misplaced Pages Continue

4242-560: The 5th century AD, the region split into several Brittonic kingdoms, including Dumnonia , centred around the old tribal territory of the Dumnonii . The upper Thames area soon came under Anglo-Saxon control but the remainder of the region was in British control until the 6th century. Bokerley Dyke , a large defensive ditch on Cranborne Chase dated to 367, delayed the Saxon conquest of Dorset, with

4343-460: The 9th century. Viking raids took place for instance in 987 and 997 at Watchet and the Battle of Cynwit . King Alfred was driven to seek refuge from the Danes at Athelney before defeating them in 878 at the Battle of Ethandun , usually considered to be near Edington, Wiltshire , but possibly the village of Edington in Somerset. Alfred established a series of forts and lookout posts linked by

4444-616: The Chancellor of King Henry I , converted the bishop's hall in Taunton into Taunton Castle . It passed to the king in 1233 and in 1245 repairs were ordered to its motte and towers. During the 11th-century Second Barons' War against Henry III , Bridgwater was held by the barons against the King. During the Middle Ages sheep farming for the wool trade came to dominate the economy of Exmoor . The wool

4545-664: The Durotriges, "water dwellers", whose main settlement is represented by Maiden Castle . Ptolemy stated that Bath was in the territory of the Belgae , but this may be a mistake. The Celtic gods were worshipped at the temple of Sulis at Bath and possibly the temple on Brean Down . Iron Age sites on the Quantock Hills include major hill forts at Dowsborough and Ruborough , as well as smaller earthwork enclosures, such as Trendle Ring , Elworthy Barrows and Plainsfield Camp . At

4646-473: The Earl of Devon, Henry VII's chamberlain, Giles Daubeney, 1st Baron Daubeney and Robert Willoughby, 1st Baron Willoughby de Broke were also influential. In 1497, early in Henry VII 's reign, the royal pretender Perkin Warbeck , besieged Exeter. The Cornish Rebellion of 1497 led by An Gof and Thomas Flamank ended in a march to Blackheath in London where the Cornish forces were massacred. Great disturbances throughout both Cornwall and Devon followed

4747-410: The Elder built similarly at Barnstaple and Totnes . But sporadic Viking incursions continued until the Norman Conquest , including the disastrous defeat of the Devonians at the Battle of Pinhoe . In 876 King Alfred the Great trapped a Danish fleet at Arne and then drove it out; 120 ships were wrecked at Studland . Although King Alfred had lands in Cornwall, it continued to have a British king. It

4848-405: The English and ruler of this province of the Britons ". Thus we can see that then the "province" was a territorial possession, which has long claimed a special relationship to the English Crown. Corfe Castle in 978 saw the murder of King Edward the Martyr , whose body was taken first to Wareham and then to Shaftesbury . Somerset played an important part in stopping the spread of the Danes in

4949-473: The Mendip Hills were run by the military. The Romans established a defensive boundary along the new military road known the Fosse Way (from the Latin fossa meaning "ditch"). The Fosse Way ran through Bath , Shepton Mallet , Ilchester and south-west towards Axminster . The road from Dorchester ran through Yeovil to meet the Fosse Way at Ilchester. Salt was produced on the Somerset Levels near Highbridge and quarrying took place near Bath, named after

5050-419: The Raglan Mudstone is marked by a well-developed calcrete , the Bishop's Frome Limestone . The lowermost Devonian formation is the St Maughans Formation , itself overlain by the Brownstones Formation though with an intervening Senni Formation over much of the area. The Upper Devonian sequence is rather thinner and comprises a series of formations which are more laterally restricted. In the Brecon Beacons ,

5151-463: The Romano-British remaining in Dorset for 200 years after the withdrawal of the Roman legions. The Western Wandsdyke earthwork was probably built during the 5th or 6th century. This area became the border between the Romano-British Celts and the West Saxons following the Battle of Deorham in 577. The Anglo-Saxons then gained control of the Cotswold area; but most of Somerset, Dorset and Devon (as well as Cornwall) remained in British hands until

SECTION 50

#1732872734909

5252-461: The South West is also the location of Thomas Hardy's Wessex , the setting for many of his best-known novels. Most of the region is located on the South West Peninsula , between the English Channel and Bristol Channel . It has the longest coastline of all the English regions, totalling over 700 miles (1,130 km). Much of the coast is now protected from further substantial development because of its environmental importance, which contributes to

5353-401: The Temeside, Raglan Mudstone and St Maughans formations of the central and eastern part of the basin. In south Pembrokeshire to the south of the Ritec Fault, the lower ORS is represented by, in ascending order, the Freshwater East, Moors Cliff and Freshwater West formations. These are unconformably overlain by the Ridgeway Conglomerate Formation. The middle ORS is missing whilst the Upper ORS

5454-411: The United Kingdom. Three major roads enter the region from the east. The M4 motorway from London to South Wales via Bristol is the busiest. The A303 cuts through the centre of the region from Salisbury to Honiton , where it merges with the A30 to continue past Exeter to the west of Cornwall. The A31 , an extension of the M27 , serves Poole and Bournemouth and the Dorset coast. The M5 runs from

5555-408: The Upper Devonian, the contact between the two being unconformable and representing the complete omission of any Middle Devonian sequence. The lowermost formations are of upper Silurian age, these being the Downton Castle Sandstone Formation and the overlying Raglan Mudstone Formation except in Pembrokeshire where a more complex series of formations is recognized. In the east of the basin, the top of

5656-399: The West Midlands, though almost all intercity trains operated by GWR run through the region. Transport for Wales also operates services between Maesteg and Cheltenham Spa . West Midlands Railway operated a parliamentary train between Birmingham New Street and Gloucester via Worcester Shrub Hill , which was withdrawn in 2019 (there was once a regular service on the route, but this

5757-416: The area sometimes called Greater Bristol , which includes parts of South Gloucestershire ; and the South East Dorset conurbation , covering Bournemouth, Poole and Christchurch . The population of the South West in 2009 was about five million. The region lies on several main line railways . The Great Western Main Line runs from London Paddington to Bristol , Exeter , Plymouth , and Penzance in

5858-476: The area. The highest point of the region is High Willhays , at 2,038 feet (621 m), on Dartmoor . In North Devon the slates of the west and limestones of the east meet at Exmoor National Park. The variety of rocks of similar ages seen has led to the county's name being given to that of the Devonian period. The east of the region is characterised by wide, flat clay vales , and chalk and limestone downland . The vales, with good irrigation, are home to

5959-534: The bedrock across half of the island. These are conformably overlain by peperite and the basaltic and andesitic Lorne plateau lavas . The ORS on Kerrera and isolated localities around Oban are known for their fossils, particularly fish. The Midland Valley graben defined by the Highland Boundary Fault in the north and the Southern Uplands Fault in the south harbours not only a considerable amount of Old Red Sandstone sedimentary rocks but also igneous rocks of this age associated with extensive volcanism . There

6060-409: The coast, probably in marginal marine environments. The familiar red colour of these rocks arises from the presence of iron oxide , but not all the Old Red Sandstone is red or sandstone – the sequence also includes conglomerates, mudstones , siltstones and thin limestones and colours can range from grey and green through to red and purple. These deposits are closely associated with

6161-465: The coast. Snowfalls are more frequent in comparison to the coast, but less so in comparison to higher ground. It experiences the lowest wind speeds and sunshine total in between that of the coast and the moors. The climate of inland areas is more noticeable the further north-east into the region. In comparison to inland areas, the coast experiences high minimum temperatures, especially in winter, and it experiences slightly lower maximum temperatures during

SECTION 60

#1732872734909

6262-676: The county of Cornwall on a widespread scale. The region is home to six universities: University of Bristol, University of The West of England (UWE), University of Exeter, University of Plymouth, Plymouth Marjon University, University of Gloucestershire (Gloucester and Cheltenham), and Falmouth University (Cornwall). The largest cities and towns in order of population are: Bristol (700,000) Plymouth (300,000) Bournemouth (250,000) Swindon (230,000) Poole (180,000) Gloucester (180,000) Exeter (160,000) Cheltenham (150,000) Torbay (150,000) Bath (130,000) Weston-super-Mare (80,000) Taunton (70,000) Salisbury (50,000) Weymouth (50,000). The largest conurbations are

6363-490: The east seems to have been halted by battles between the British and Saxons, for example at the siege of Badon Mons Badonicus (which may have been in the Bath district, perhaps at Solsbury Hill ), or Bathampton Down . The Battle of Bedwyn was fought in 675 between Escuin , a West Saxon nobleman who had seized the throne of Queen Saxburga , and King Wulfhere of Mercia . The earliest fortification of Taunton started for King Ine of Wessex and Æthelburg , in or about

6464-435: The end of the ice age; however, it is unclear whether the region was continuously inhabited during the previous 4000 years, or if humans returned to the gorge after a final cold spell. A Palaeolithic flint tool found in West Sedgemoor is the earliest indication of human presence on the Somerset Levels. During the 7th millennium BC the sea level rose and flooded the valleys, so the Mesolithic people occupied seasonal camps on

6565-470: The erosion of the Caledonian Mountain chain which was thrown up by the collision of the former continents of Avalonia , Baltica and Laurentia to form the Old Red Sandstone Continent - an event known as the Caledonian Orogeny . Many fossils are found within the rocks, including early fishes, arthropods and plants. As is typical with terrestrial red beds , the vast majority of the rock is not fossil-bearing; however there are isolated, localized beds within

6666-490: The eve of the Black Death of 1348–49. The plague resulted in a prolonged pause in the growth of Bristol's population, with numbers remaining at 10,000–12,000 through most of the 15th and 16th centuries. During the Wars of the Roses , there were frequent skirmishes between the Lancastrian Thomas Courtenay, Earl of Devon and Yorkist William, Lord Bonville . In 1470, Edward IV pursued Richard Neville, Earl of Warwick and George, Duke of Clarence as far as Exeter after

6767-400: The far west of Cornwall. The South West Main Line runs from London Waterloo and Southampton to Bournemouth , Poole and Weymouth in Dorset. The West of England Main Line runs from London Waterloo to Exeter via south Wiltshire, north Dorset and south Somerset. The Wessex Main Line runs from Bristol to Salisbury and on to Southampton. The Heart of Wessex Line runs from Bristol in

6868-405: The former Brecknockshire (now south Powys) of south Wales. South West England South West England , or the South West of England , is one of the nine official regions of England in the United Kingdom . It consists of the counties of Cornwall (including the Isles of Scilly ), Dorset , Devon , Bristol , Gloucestershire , Somerset and Wiltshire . Cities and large towns in

6969-399: The government of the western counties of England. It was analogous in form to the Council of the North . The council was established in March 1539, with Lord Russell as its Lord President. Members included Thomas Derby, Sir Piers Edgcumbe, Sir Richard Pollard and John Rowe. However, the fall of Thomas Cromwell , the chief political supporter of government by Councils, and the tranquillity of

7070-411: The growing sway of the Norsemen . Eventually England came to be ruled by Norse monarchs, and the Anglo-Saxon kingdoms fell one by one, Wessex being conquered in 1013 by King Sweyn Forkbeard . Sweyn's realms included Denmark and Norway , and parts of England such as Mercia (an Anglian kingdom roughly coinciding with the English Midlands ), much of which, along with northern England, fell under

7171-430: The higher ground, indicated by scatters of flints. The Neolithic people continued to exploit the reed swamps for their natural resources and started to construct wooden trackways. These included the Post Track and the Sweet Track . The Sweet Track, dating from the 39th century BC, is thought to be the world's oldest timber trackway and was once thought to be the world's oldest engineered roadway. The Levels were also

7272-469: The introduction of Edward VI 's Book of Common Prayer . The day after Whit Sunday 1549, a priest at Sampford Courtenay was persuaded to read the old mass . This insubordination spread swiftly into serious revolt. The Cornish quickly joined the men of Devon in the Prayer Book Rebellion and Exeter was besieged until relieved by Lord Russell. The Cornish had a particular motivation for opposing

7373-787: The late 7th century. According to the Anglo-Saxon Chronicle , the Saxon Cenwalh achieved a breakthrough against the British Celtic tribes, with victories at Bradford-on-Avon (in the Avon Gap in the Wansdyke) in 652, and further south at the Battle of Peonnum (at Penselwood ) in 658, followed by an advance west through the Polden Hills to the River Parrett . The Saxon advance from

7474-721: The location of the Glastonbury Lake Village as well as two lake villages at Meare . Stonehenge , Avebury and Stanton Drew are perhaps the most famous Neolithic sites in the UK. The region was heavily populated during the Neolithic, Bronze Age and Iron Age periods. Many monuments, barrows and trackways exist. Coin evidence shows that the region was split between the Durotriges , Dobunni and Dumnonii . The Iron Age tribe in Dorset were

7575-454: The middle and upper ORS are missing with only the lower ORS present; this is divided into an earlier Milford Haven Group comprising in ascending order, the Red Cliff, Sandy Haven and Gelliswick Bay formations and a later Cosheston Group with, again in ascending order, its constituent Llanstadwell, Burton Cliff, Mill Bay, Lawrenny Cliff and New Shipping formations. These respectively equate with

7676-699: The new English language prayer book, as there were still many monoglot Cornish speakers in West Cornwall. The Cornish language declined rapidly afterwards and the Dissolution of the Monasteries resulted in the eventual loss of the Cornish language as a primary language. By the end of the 18th century it was no longer a first language. The Council of the West was a short-lived administrative body established by Henry VIII for

7777-487: The north of the region to Weymouth on the south Dorset coast via Westbury , Castle Cary and Yeovil , with most services starting at Gloucester . The vast majority of trains in the region are operated by CrossCountry , Great Western Railway (GWR) and South Western Railway (SWR). GWR is the key operator for all counties in the region except Dorset where SWR is the key operator. CrossCountry operates services to Manchester Piccadilly , Glasgow and Aberdeen . Dorset

7878-440: The peninsula where the status of being from the region is less equivocal. In particular, Cornwall 's inclusion in the region is disputed by Cornish nationalists. The cross-party Cornish Constitutional Convention and Cornish nationalist party Mebyon Kernow have campaigned for a Cornish Assembly ever since the idea of regional devolution was put forward. The South West region is largely rural, with small towns and villages;

7979-574: The period, including the remains at Bath. The area of Somerset was part of the Roman Empire from AD 47 to about AD 409. The empire disintegrated gradually, and elements of Romanitas lingered on for perhaps a century. In AD 47, Somerset was invaded from the south-east by the Second Legion Augusta , under the future emperor Vespasian . The hillforts of the Durotriges at Ham Hill and Cadbury Castle were captured. Ham Hill probably had

8080-504: The region have some level of a "South West" or "West Country" regional identity, although this may not necessarily correspond to an identification with the official government-defined region . It is common for people in the region to identify at a national level (whether English , British , Cornish or a county, city or town level). Identifying as being from 'the Westcountry', amorphous though it is, tends to be more predominant further into

8181-538: The region include Bath , Bristol , Bournemouth , Cheltenham , Exeter , Gloucester , Plymouth and Swindon . It is geographically the largest of the nine regions of England with a land area of 9,203 square miles (23,836 km ), but the third-least populous, with an estimated 5,764,881 residents in 2022. The region includes the West Country and much of the ancient kingdom of Wessex . It includes two entire national parks , Dartmoor and Exmoor (a small part of

8282-500: The region's attractiveness to tourists and residents. Geologically the region is divided into the largely igneous and metamorphic west and sedimentary east, the dividing line slightly to the west of the River Exe . Cornwall and West Devon's landscape is of rocky coastline and high moorland, notably at Bodmin Moor and Dartmoor . These are due to the granite and slate that underlie

8383-569: The region's dairy agriculture. The Blackmore Vale was Thomas Hardy 's "Vale of the Little Dairies"; another, the Somerset Levels was created by reclaiming wetlands. The Southern England Chalk Formation extends into the region, creating a series of high, sparsely populated and archaeologically rich downs, most famously Salisbury Plain , but also Cranborne Chase , the Dorset Downs and

8484-420: The rest of the southwest (approximately twice as much rainfall as lowland areas), because of their high altitude. Both of these factors also cause it to experience the highest levels of snowfall and the lowest levels of sunshine. Exposed areas of the moors are windier than lowlands and can be almost as windy as the coast. The boundaries of the South West region are based upon those devised by central government in

8585-490: The rock that do contain fossils. Rocks of this age were also laid down in South West England (hence the name 'Devonian'; from Devon ) though these are of true marine origin and are not included within the Old Red Sandstone. Since the Old Red Sandstone consists predominantly of rocks of terrestrial origin, it does not generally contain marine fossils which would otherwise prove useful in correlating one occurrence of

8686-519: The rock with another, both between and within individual sedimentary basins . Accordingly, local stage names were devised and these remain in use to some extent today though there is an increasing use of international stage names. Thus in the Anglo-Welsh Basin, there are frequent references to the Downtonian , Dittonian , Breconian and Farlovian stages in the literature. The existence of

8787-522: The same time by the same processes. The Old Red Sandstone has been widely used as a building stone across those regions where it outcrops. Notable examples of its use can be found in the area surrounding Stirling , Stonehaven , Perth and Tayside . The inhabitants of Caithness at the northeastern tip of Scotland also used the stone to a considerable extent. Old Red Sandstone has also frequently been used in buildings in Herefordshire, Monmouthshire and

8888-462: The sea level rose, resulting in major coastal changes. The Somerset Levels were flooded, but the dry points such as Glastonbury and Brent Knoll are known to have been occupied by Mesolithic hunters. The landscape at this time was tundra . Britain's oldest complete skeleton, Cheddar Man , lived at Cheddar Gorge around 7150 BC (in the Upper Palaeolithic or Old Stone Age), shortly after

8989-481: The south-west. It is the second windiest area of the United Kingdom, the majority of winds coming from the south-west and north-east. Government organisations predict the region to rise in temperature and become the hottest region in the United Kingdom. Inland areas of low altitude experience the least amount of precipitation. They experience the highest summer maxima temperatures, but winter minima are colder than

9090-407: The summer. Rainfall is the lowest at the coast and snowfall is rarer than the rest of the region. Coastal areas are the windiest parts of the peninsula and they receive the most sunshine. The general coastal climate is more typical the further south-west into the region. Areas of moorland inland such as: Bodmin Moor , Dartmoor and Exmoor experience lower temperatures and more precipitation than

9191-517: The time of the Roman invasion , the inhabitants of the entire area spoke a Brythonic Celtic language. Its descendant languages are still spoken to a greater or lesser extent in Cornwall , Wales, and Brittany . During the Roman era , the east of the region, particularly the Cotswolds and eastern Somerset, was heavily Romanised but Devon and Cornwall were much less so, though Exeter was a regional capital. There are villas, farms and temples dating from

9292-549: The west of the region, but these were small compared with the established wealth of ancient cathedral cities in the east of the region such as Exeter , Bath and Wells . Wealth grew from sheep farming in the east of the region: church controlled estates such as Glastonbury Abbey and Wells became among the richest in England, while tin and silver mining was important in Devon and Cornwall; Stannary Parliaments with semi-autonomous powers were established. Farming prospered until it

9393-459: The west through Carmarthenshire into Powys and Monmouthshire and through the southern Welsh Marches , notably into Herefordshire , Worcestershire and Gloucestershire . Outliers in Somerset and north Devon complete the extent of this basin. With the exception of south Pembrokeshire, all parts of the basin are represented by a range of lithologies assigned to the Lower Devonian and to

9494-532: The year 710. However, according to the Anglo-Saxon Chronicle this was destroyed 12 years later. Alfred the Great refortified Exeter as a defensive burh , followed by new erections at Lydford , Halwell and Pilton , although these fortifications were small compared to burhs further east, suggesting that they were protection for the elite only. The English defeated a combined Cornish and Danish force at Hingston Down (near Gunnislake) in 838. Edward

9595-449: Was an important port, handling much of England's trade with Ireland. During this period Bristol also became a centre of shipbuilding and manufacturing. Bristol was the starting point for many important voyages, notably John Cabot 's 1497 voyage of exploration to North America. By the 14th century Bristol was one of England's three largest medieval towns after London, along with York and Norwich , with perhaps 15,000–20,000 inhabitants on

9696-706: Was severely hit by the Black Death which arrived in Dorset in 1348 and quickly spread through Somerset, causing widespread death, with mortality rates perhaps as high as 50% in places. The resulting labour shortage led to changes in feudal practices. Crafts and industries also flourished; the Somerset woollen industry was then one of the largest in England. Coal mining in the Mendips was an important source of wealth while quarrying also took place. Many parish churches were rebuilt in this period. Between 1107 and 1129 William Giffard ,

9797-563: Was sold off in 1818. Where conditions were suitable, coastal villages and ports had an economy based on fishing. The larger ports such as Fowey contributed vessels to the naval enterprises of the King and were subject to attack from the French in return. Bridgwater was part of the Port of Bristol until the Port of Bridgwater was created in 1348, covering 80 miles (130 km) of the Somerset coast line, from

9898-465: Was spun into thread on isolated farms and collected by merchants to be woven, fulled, dyed and finished in thriving towns such as Dunster . The land started to be enclosed and from the 17th century onwards larger estates developed, leading to establishment of areas of large regular shaped fields. During this period a royal forest and hunting ground was established, administered by the Warden. The royal forest

9999-547: Was the one that placed it in the Devonian : he coined the name of that period. The term 'Old Red Sandstone' was originally used in 1821 by Scottish naturalist and mineralogist Robert Jameson to refer to the red rocks which underlay the 'Mountain Limestone' i.e. the Carboniferous Limestone. They were thought at that time to be the British version of Germany's Rotliegendes , which is in fact of Permian age. Many of

10100-403: Was widely recognised for government administration and statistics. The boundaries were carried forward into the 1990s when regional administrations were formally established as Government Office Regions. A regional assembly and regional development agency were created in 1999, then abolished in 2008 and 2012 respectively. It has been argued that the official South West region does not possess

10201-576: Was withdrawn in 2009). It has been proposed that the former London & South Western Railway Exeter to Plymouth railway be reopened to connect Cornwall and Plymouth as an alternative to the route via the Dawlish seawall that is susceptible to closure in bad weather. Local bus services are primarily operated by FirstGroup , Go-Ahead Group and Stagecoach subsidiaries as well as independent operators. Megabus and National Express operate long-distance services from South West England to all parts of

#908091