1.
Summit
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A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. Mathematically, a summit is a maximum in elevation. The topographic terms acme, apex, peak, and zenith are synonymous, the UIAA definition is that a summit is independent if it has a prominence of 30 metres or more, it is a mountain if it has a prominence of at least 300 metres. This can be summarised as follows, A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top, Summit may also refer to the highest point along a line, trail, or route. In many parts of the western United States, the term refers to the highest point along a road, highway. For example, the highest point along Interstate 80 in California is referred to as Donner Summit while the highest point on Interstate 5 is Siskiyou Mountain Summit, geoid Hill List of highest mountains Maxima and minima Nadir Summit accordance Peak finder
2.
Staffordshire
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Staffordshire is a landlocked county in the West Midlands of England. It adjoins Cheshire to the north west, Derbyshire and Leicestershire to the east, Warwickshire to the south east, West Midlands and Worcestershire to the south, and Shropshire to the west. The largest city in Staffordshire is Stoke-on-Trent, which is administered separately from the rest of the county as an independent unitary authority, Lichfield also has city status, although this is a considerably smaller cathedral city. Major towns include Stafford, Burton upon Trent, Cannock, Newcastle-under-Lyme, Leek, smaller towns include Stone, Uttoxeter, and Rugeley, and large villages Eccleshall, Wombourne, Kinver, Penkridge, Tutbury and Stretton. Cannock Chase AONB is within the county as well as parts of the National Forest, Wolverhampton, Walsall, West Bromwich, and Smethwick were historic Staffordshire towns until local government reorganisation created the West Midlands county in 1974. Historically, Staffordshire was divided into the five hundreds of Cuttlestone, Offlow, Pirehill, Seisdon, the historic boundaries of Staffordshire cover much of what is now the metropolitan county of West Midlands. The Act also saw the towns of Tamworth and Burton upon Trent united entirely in Staffordshire, in 1553 Queen Mary made Lichfield a county separate from the rest of Staffordshire. Handsworth and Perry Barr became part of the county borough of Birmingham in the early 20th century, Burton, in the east of the county, became a county borough in 1901, and was followed by Smethwick, another town in the Black Country in 1907. In 1910 the six towns of the Staffordshire Potteries, including Hanley, a major reorganisation in the Black Country in 1966, under the recommendation of the Local Government Commission for England led to the creation of an area of contiguous county boroughs. Meanwhile, the county borough of Dudley, historically a part of Worcestershire, expanded. County boroughs were abolished, with Stoke becoming a district in Staffordshire. On 1 April 1997, under a recommendation of the Banham Commission, in July 2009 the largest hoard of Anglo-Saxon gold ever found in Britain was discovered in a field near Lichfield. The artefacts, known as The Staffordshire Hoard have tentatively dated to the 7th or 8th centuries. Some nationally and internationally known companies have their base in Staffordshire. They include the Britannia Building Society which is based in Leek, JCB is based in Rocester near Uttoxeter and bet365 based in Stoke-on-Trent. The theme park Alton Towers is in the Staffordshire Moorlands and several of the worlds largest pottery manufacturers are based in Stoke-on-Trent, Staffordshire has a completely comprehensive system with eight independent schools. Most secondary schools are from 11–16 or 18, but two in Staffordshire Moorlands and South Staffordshire are from 13–18, there are two universities in the county, Keele University in Newcastle-under-Lyme and Staffordshire University, which has campuses in Stoke-on-Trent, Stafford, Lichfield and Shrewsbury. The modern county of Staffordshire currently has three football clubs – Stoke City and Port Vale, both from Stoke-on-Trent, and Burton Albion, who play in Burton upon Trent. They were among the 12 founder members of the Football League in 1888, in 1972, the club finally won a major trophy when they lifted the Football League Cup, but after relegation from the First Division in 1985 they would not experience top flight football for 23 years
3.
England
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England is a country that is part of the United Kingdom. It shares land borders with Scotland to the north and Wales to the west, the Irish Sea lies northwest of England and the Celtic Sea lies to the southwest. England is separated from continental Europe by the North Sea to the east, the country covers five-eighths of the island of Great Britain in its centre and south, and includes over 100 smaller islands such as the Isles of Scilly, and the Isle of Wight. England became a state in the 10th century, and since the Age of Discovery. The Industrial Revolution began in 18th-century England, transforming its society into the worlds first industrialised nation, Englands terrain mostly comprises low hills and plains, especially in central and southern England. However, there are uplands in the north and in the southwest, the capital is London, which is the largest metropolitan area in both the United Kingdom and the European Union. In 1801, Great Britain was united with the Kingdom of Ireland through another Act of Union to become the United Kingdom of Great Britain and Ireland. In 1922 the Irish Free State seceded from the United Kingdom, leading to the latter being renamed the United Kingdom of Great Britain, the name England is derived from the Old English name Englaland, which means land of the Angles. The Angles were one of the Germanic tribes that settled in Great Britain during the Early Middle Ages, the Angles came from the Angeln peninsula in the Bay of Kiel area of the Baltic Sea. The earliest recorded use of the term, as Engla londe, is in the ninth century translation into Old English of Bedes Ecclesiastical History of the English People. According to the Oxford English Dictionary, its spelling was first used in 1538. The earliest attested reference to the Angles occurs in the 1st-century work by Tacitus, Germania, the etymology of the tribal name itself is disputed by scholars, it has been suggested that it derives from the shape of the Angeln peninsula, an angular shape. An alternative name for England is Albion, the name Albion originally referred to the entire island of Great Britain. The nominally earliest record of the name appears in the Aristotelian Corpus, specifically the 4th century BC De Mundo, in it are two very large islands called Britannia, these are Albion and Ierne. But modern scholarly consensus ascribes De Mundo not to Aristotle but to Pseudo-Aristotle, the word Albion or insula Albionum has two possible origins. Albion is now applied to England in a poetic capacity. Another romantic name for England is Loegria, related to the Welsh word for England, Lloegr, the earliest known evidence of human presence in the area now known as England was that of Homo antecessor, dating to approximately 780,000 years ago. The oldest proto-human bones discovered in England date from 500,000 years ago, Modern humans are known to have inhabited the area during the Upper Paleolithic period, though permanent settlements were only established within the last 6,000 years
4.
Mountain range
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A mountain range is a geographic area containing numerous geologically related mountains. A mountain system or system of ranges, sometimes is used to combine several geological features that are geographically related. Mountain ranges are usually segmented by highlands or mountain passes and valleys, individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, most geologically young mountain ranges on the Earths land surface are associated with either the Pacific Ring of Fire or the Alpide Belt. The Andes is 7,000 kilometres long and is considered the worlds longest mountain system. The Alpide belt includes Indonesia and southeast Asia, through the Himalaya, the belt also includes other European and Asian mountain ranges. The Himalayas contain the highest mountains in the world, including Mount Everest, mountain ranges outside of these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Altai Mountains and the Hijaz Mountains. If the definition of a range is stretched to include underwater mountains. The mountain systems of the earth are characterized by a tree structure, the sub-range relationship is often expressed as a parent-child relationship. For example, the White Mountains of New Hampshire and the Blue Ridge Mountains are sub-ranges of the Appalachian Mountains, equivalently, the Appalachians are the parent of the White Mountains and Blue Ridge Mountains, and the White Mountains and the Blue Ridge Mountains are children of the Appalachians. The position of mountains influences climate, such as rain or snow, when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the side, it warms again and is drier. Often, a shadow will affect the leeward side of a range. Mountain ranges are constantly subjected to forces which work to tear them down. Erosion is at work while the mountains are being uplifted and long after until the mountains are reduced to low hills, rivers are traditionally believed to be the principle erosive factor on mountain ranges, with their ability of bedrock incision and sediment transport. The rugged topography of a range is the product of erosion. The basins adjacent to a mountain range are filled with sediments which are buried and turned into sedimentary rock. The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example and this mass of rock was removed as the range was actively undergoing uplift
5.
Peak District
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The Peak District is an upland area in England at the southern end of the Pennines. It is mostly in northern Derbyshire, but also parts of Cheshire, Greater Manchester. The Peak District National Park became the first national park in the United Kingdom in 1951, with its proximity to the cities of Manchester, Stoke-on-Trent, Derby and Sheffield and easy access by road and rail, it attracts millions of visitors every year. The Peak District forms the end of the Pennines and much of the area is uplands above 1,000 feet. Despite its name, the landscape generally lacks sharp peaks, being characterised by rounded hills, the area is surrounded by major conurbations, including Huddersfield, Manchester, Sheffield, Derby and Stoke-on-Trent. The National Park covers 555 square miles of Derbyshire, Staffordshire, Cheshire, Greater Manchester and South and West Yorkshire, including the majority of the area commonly referred to as the Peak. Its northern limits lie along the A62 road between Marsden and Meltham, north east of Oldham, while its southernmost point is on the A52 road on the outskirts of Ashbourne in Derbyshire. The town of Bakewell and numerous villages are included within the boundaries, as of 2010, it is the fifth largest National Park in England and Wales. 12% of the Peak District National Park is owned by the National Trust and it does not receive government funding. The Peak District National Park Authority directly owns around 5%, the Peak District is formed almost exclusively from sedimentary rocks dating from the Carboniferous period. They comprise the Carboniferous Limestone, the overlying Gritstone and finally the Coal Measures, in addition there are infrequent outcrops of igneous rocks including lavas, tuffs and volcanic vent agglomerates. The general geological structure of the Peak District is that of a broad dome, the southern edge of the dome is overlain by sandstones of Triassic age though these barely impinge upon the National Park. Earth movements after the Carboniferous period resulted in the up-doming of the area and, particularly in the west, the region was raised in a north–south line which resulted in this dome-like shape and the shale and sandstone were worn away until limestone was exposed. At the end of period, the Earths crust sank here which led to the area being covered by sea. Some time after its deposition, mineral veins were formed in the limestone and these veins and rakes have been mined for lead since Roman times. The Peak District was covered by ice during at least one of the ice ages of the last 2 million years as evidenced by the patches of glacial till or boulder clay that can be found across the area. It was not covered by ice during the last glacial period, a mix of Irish Sea and Lake District ice abutted against its western margins. Glacial meltwaters eroded a complex of channels along this margin of the Peak District during this period
6.
Ordnance Survey
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Ordnance Survey is a non-ministerial government department which acts as the national mapping agency for Great Britain and is one of the worlds largest producers of maps. Since 1 April 2015 it has operated as Ordnance Survey Ltd, the Ordnance Survey Board remain accountable to the Secretary of State for Business, Energy and Industrial Strategy. It is also a member of the Public Data Group, the agencys name indicates its original military purpose, mapping Scotland in the wake of the Jacobite rebellion in 1745. There was also a general and nationwide need in light of the potential threat of invasion during the Napoleonic Wars. Ordnance Survey mapping is usually classified as either large-scale or small-scale, the Surveys large-scale mapping comprises maps at six inches to the mile or more and was available as sheets until the 1980s, when it was digitised. Small-scale mapping comprises maps at less than six inches to the mile, such as the one inch to the mile leisure maps. These are still available in sheet form. Ordnance Survey maps remain in copyright for fifty years after their publication, some of the Copyright Libraries hold complete or near-complete collections of pre-digital OS mapping. The origins of the Ordnance Survey lie in the aftermath of the last Jacobite rising which was defeated by forces loyal to the government at the Battle of Culloden in 1746. In 1747, Lieutenant-colonel David Watson proposed the compilation of a map of the Highlands to facilitate the subjugation of clans, in response, King George II charged Watson with making a military survey of the Highlands under the command of the Duke of Cumberland. Among Watsons assistants were William Roy, Paul Sandby and John Manson, the survey was produced at a scale of 1 inch to 1000 yards and included the Duke of Cumberlands Map now held in the British Library. This work was the point of the Principal Triangulation of Great Britain. Roys technical skills and leadership set the standard for which Ordnance Survey became known. Work was begun in earnest in 1790 under Roys supervision, when the Board of Ordnance began a military survey starting with the south coast of England. A set of stamps, featuring maps of the Kentish village of Hamstreet, was issued in 1991 to mark the bicentenary. In 1801, the first one-inch-to-the-mile map was published, detailing the county of Kent, during the next twenty years, roughly a third of England and Wales was mapped at the same scale under the direction of William Mudge, as other military matters took precedence. It took until 1823 to re-establish a relationship with the French survey made by Roy in 1787, by 1810, one inch to the mile maps of most of the south of England were completed, but were withdrawn from sale between 1811 and 1816 because of security fears. It was gruelling work, major Thomas Colby, later the longest serving director general of Ordnance Survey, in 1824, Colby and most of his staff moved to Ireland to work on a six-inches-to-the-mile valuation survey
7.
Leek, Staffordshire
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Leek is a market town and civil parish in the county of Staffordshire, England, on the River Churnet. It is situated about 10 miles north east of Stoke-on-Trent and it is an ancient borough and was granted its royal charter in 1214. It is the centre for the Staffordshire Moorlands District Council. King John granted Ranulph de Blondeville, 6th Earl of Chester, the right to hold a weekly Wednesday market, leeks coat of arms is made up of a Saltire Shield. On the top is the Stafford Knot, either side is the Leek Double Sunset, the crest is a mural crown with three Mulberry leaves on a Mount of Heather on top of which a Moorcock is resting his claw on a small-weave Shuttle. The motto ARTE FAVENTE NIL DESPERANDUM translates to, Our skill assisting us, the town had a regular cattle market for hundreds of years, reflecting its role as a centre of local farming. Following the Industrial Revolution it was a producer of textiles. However, this industry has now ceased, the mills from the towns textile era remain and many have now been converted into housing. Britannia, the former Building Society, has its headquarters in the town and was a local employer. Most of the town is at or above 600 feet and is surrounded by the countryside of the Staffordshire Moorlands which is situated on the southern uplands of the Pennines. Leek is built on the slope and crown of a hill which is situated just a few south of the Roaches. Many Victorian period, and older, buildings stand in the town. In 1849 William Sugden came to Leek and he was an architect and his work on the design of the railway stations for the Churnet Valley Railway brought him to the area. In the following year William’s son, Larner Sugden, was born, the firm had offices in Derby Street. The building still survives, the ground floor now being occupied by Boots the Chemist, Larner was a great supporter of the Society for the Protection of Ancient Buildings, and so Leek’s development was in sympathetic hands. The architectural output from Sugden & Son was both prolific and varied and this last was probably the last joint venture of the father-and-son team because William Sugden died in 1892. The Sugden masterpiece was, perhaps, the Nicholson Institute, built in the Queen Anne style, the fact that this building is tucked away behind the 17th century ‘Greystones’ is a further indication of Larner’s regard for old buildings. Larner would not countenance demolition of the old building, and so, as the Nicholsons owned the land to the rear, in 1899 came the Technical Schools and the Co-operative Society Hall
8.
Hiking
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Hiking is the preferred term, in Canada and the United States, for a long, vigorous walk, usually on trails, in the countryside, while the word walking is used for shorter, particularly urban walks. On the other hand, in the United Kingdom, and the Republic of Ireland, the word hiking is also often used in the UK, along with rambling, hillwalking, and fell walking. The term bushwalking is endemic to Australia, having been adopted by the Sydney Bush Walkers club in 1927, in New Zealand a long, vigorous walk or hike is called tramping. It is an activity with numerous hiking organizations worldwide. In the United States, Canada, the Republic of Ireland, a day hike refers to a hike that can be completed in a single day. However, in the United Kingdom, the walking is also used, as well as rambling. In Northern England, Including the Lake District and Yorkshire Dales, fellwalking describes hill or mountain walks, hiking sometimes involves bushwhacking and is sometimes referred to as such. This specifically refers to walking through dense forest, undergrowth, or bushes. In extreme cases of bushwhacking, where the vegetation is so dense that human passage is impeded, the Australian term bushwalking refers to both on and off-trail hiking. Common terms for hiking used by New Zealanders are tramping, walking or bushwalking, trekking is the preferred word used to describe multi-day hiking in the mountainous regions of India, Pakistan, Nepal, North America, South America, Iran and in the highlands of East Africa. Hiking a long-distance trail from end-to-end is also referred to as trekking, in North America, multi-day hikes, usually with camping, are referred to as backpacking. The idea of taking a walk in the countryside for pleasure developed in the 18th-century, in earlier times walking generally indicated poverty and was also associated with vagrancy. Thomas West, an English priest, popularized the idea of walking for pleasure in his guide to the Lake District of 1778. To this end he included various stations or viewpoints around the lakes, published in 1778 the book was a major success. Another famous early exponent of walking for pleasure, was the English poet William Wordsworth, in 1790 he embarked on an extended tour of France, Switzerland, and Germany, a journey subsequently recorded in his long autobiographical poem The Prelude. His famous poem Tintern Abbey was inspired by a visit to the Wye Valley made during a tour of Wales in 1798 with his sister Dorothy Wordsworth. Wordsworths friend Coleridge was another keen walker and in the autumn of 1799, he and Wordsworth undertook a three weeks tour of the Lake District. John Keats, who belonged to the generation of Romantic poets began, in June 1818, a walking tour of Scotland, Ireland
9.
Rock climbing
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Rock climbing is an activity in which participants climb up, down or across natural rock formations or artificial rock walls. The goal is to reach the summit of a formation or the endpoint of a usually pre-defined route without falling. Due to the length and extended endurance required and because accidents are likely to happen on descent than ascent. It is very rare for a climber to downclimb, especially on the larger multiple pitches, professional Rock climbing competitions have the objectives of either completing the route in the quickest possible time or attaining the farthest point on an increasingly difficult route. Scrambling, another activity involving the scaling of hills and similar formations, is similar to rock climbing, however, rock climbing is generally differentiated by its sustained use of hands to support the climbers weight as well as to provide balance. Rock climbing is a physically and mentally demanding sport, one that often tests a climbers strength, endurance, agility and it can be a dangerous activity and knowledge of proper climbing techniques and usage of specialized climbing equipment is crucial for the safe completion of routes. Because of the range and variety of rock formations around the world. Paintings dating from 200 BC show Chinese men rock climbing China woop woop, in early America, the cliff-dwelling Anasazi in the 12th century were thought to be excellent climbers. Early European climbers used rock climbing techniques as a required to reach the summit in their mountaineering exploits. In the 1880s, European rock climbing become an independent pursuit outside of mountain climbing, Rock climbing evolved gradually from an alpine necessity to a distinct athletic activity. However, climbing techniques, equipment and ethical considerations have evolved steadily, today, free climbing, climbing using holds made entirely of natural rock while using gear solely for protection and not for upward movement, is the most popular form of the sport. Free climbing has since divided into several sub-styles of climbing dependent on belay configuration. Over time, grading systems have also created in order to compare more accurately the relative difficulties of the rock climbs. In How to Rock Climb, John Long notes that for moderately skilled climbers simply getting to the top of a route is not enough, in rock climbing, style refers to the method of ascending the cliff. There are three styles of climbing, on-sight, flash, and redpoint. To on-sight a route is to ascend the wall without aid or any foreknowledge and it is considered the way to climb with the most style. Flashing is similar to on-sighting, except that the climber has previous information about the route including talking about the beta with other climbers, redpointing means to make a free ascent of the route after having first tried it. Free climbing is typically divided into styles that differ from one another depending on the choice of equipment used
10.
Cheshire
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Cheshire is a county in North West England, bordering Merseyside and Greater Manchester to the north, Derbyshire to the east, Staffordshire and Shropshire to the south and Wales to the west. Cheshires county town is Chester, the largest town is Warrington, other major towns include Congleton, Crewe, Ellesmere Port, Macclesfield, Northwich, Runcorn, Widnes, Wilmslow, and Winsford. The county covers 905 square miles and has a population of around 1 million and it is mostly rural, with a number of small towns and villages supporting the agricultural and other industries which produce Cheshire cheese, salt, chemicals and silk. Cheshires name was derived from an early name for Chester. Although the name first appears in 980, it is thought that the county was created by Edward the Elder around 920, in the Domesday Book, Chester was recorded as having the name Cestrescir, derived from the name for Chester at the time. A series of changes occurred as English itself changed, together with some simplifications and elision, resulted in the name Cheshire. Because of the close links with the land bordering Cheshire to the west. The Domesday Book records Cheshire as having two complete Hundreds that later became the part of Flintshire. Additionally, another portion of the Duddestan Hundred later became known as Maelor Saesneg when it was transferred to North Wales. For this and other reasons, the Welsh name for Cheshire is sometimes used within Wales, after the Norman conquest of 1066 by William I, dissent and resistance continued for many years after the invasion. In 1069 local resistance in Cheshire was finally put down using draconian measures as part of the Harrying of the North, the ferocity of the campaign against the English populace was enough to end all future resistance. Examples were made of major landowners such as Earl Edwin of Mercia, William I made Cheshire a county palatine and gave Gerbod the Fleming the new title of Earl of Chester. When Gerbod returned to Normandy in about 1070, the king used his absence to declare the earldom forfeit, due to Cheshires strategic location on Welsh Marches, the Earl had complete autonomous powers to rule on behalf of the king in the county palatine. Cheshire in the Domesday Book is recorded as a larger county than it is today. It included two hundreds, Atiscross and Exestan, that became part of North Wales. At the time of the Domesday Book, it included as part of Duddestan Hundred the area of land later known as English Maelor in Wales. The area between the Mersey and Ribble formed part of the returns for Cheshire, an example is the barony of Halton. One of Hugh dAvranches barons has been identified as Robert Nicholls, Baron of Halton, in 1182 the land north of the Mersey became administered as part of the new county of Lancashire, thus resolving any uncertainty about the county in which the land Inter Ripam et Mersam was
11.
Snowdon
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Snowdon is the highest mountain in Wales, at an elevation of 1,085 metres above sea level, and the highest point in the British Isles south of the Scottish Highlands. It is located in Snowdonia National Park in Gwynedd, and has described as probably the busiest mountain in Britain. It is designated as a nature reserve for its rare flora. The cliff faces on Snowdon, including Clogwyn Dur Arddu, are significant for rock climbing, the summit also houses a cafe called Hafod Eryri, open only when the railway is operating and opened in 2009 to replace one built in the 1930s. The railway generally operates to the station from Whitsun to October. The daily running schedule depends on weather and customer demand, as well as other figures from Arthurian legend, the mountain is linked to a legendary afanc and the Tylwyth Teg. A1682 survey estimated that the summit of Snowdon was at a height of 3,720 feet, in 1773, Thomas Pennant quoted a later estimate of 3,568 ft above sea level at Caernarfon. Recent surveys give the height of the summit as 1,085 m, making Snowdon the highest mountain in Wales, Snowdon is one of three mountains climbed as part of the National Three Peaks Challenge. The unique environment of Snowdon, particularly its rare plants, has led to its designation as a nature reserve. In addition to plants that are widespread in Snowdonia, Snowdon is home to some plants rarely found elsewhere in Britain, Snowdon lies in the northern part of Snowdonia National Park, which has also provided some legal protection since the parks establishment in 1951. The rocks which make up Snowdon and its neighbouring mountains were formed in the Ordovician Period. At that time, most of modern-day Wales was near the edge of Avalonia, in the Soudleyan stage of the Caradoc age, a volcanic caldera formed, and produced ash flows of rhyolitic tuff, which formed deposits up to 500 metres thick. The current summit is near the edge of the ancient caldera, the calderas full extent is unclear. Snowdon and its surrounding peaks have been described as examples of Alpine topography. The summits of Snowdon and Garnedd Ugain are surrounded by cwms, erosion by glaciers in adjacent cwms caused the characteristic arêtes of Crib Goch, Crib y Ddysgl and Y Lliwedd, and the pyramidal peak of Snowdon itself. Other glacial landforms that can be seen around Snowdon include roches moutonnées, glacial erratics, the English name Snowdon comes from the Old English snaw dun, meaning snow hill, as Snowdon often has a covering of snow. Although the amount of snow on Snowdon in winter varies significantly, the slopes of Snowdon have one of the wettest climates in Great Britain, receiving an annual average of more than 200 inches of precipitation. A number of lakes are found in the various cwms of the Snowdon range, Llyn Llydaw –1,430 feet high,110 acres – lies in Cwm Dyli, Snowdons eastern cwm, and is one of Snowdonias deepest lakes, at up to 190 ft deep
12.
Wales
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Wales is a country that is part of the United Kingdom and the island of Great Britain. It is bordered by England to the east, the Irish Sea to the north and west, and it had a population in 2011 of 3,063,456 and has a total area of 20,779 km2. Wales has over 1,680 miles of coastline and is mountainous, with its higher peaks in the north and central areas, including Snowdon. The country lies within the temperate zone and has a changeable. Welsh national identity emerged among the Celtic Britons after the Roman withdrawal from Britain in the 5th century, Llywelyn ap Gruffudds death in 1282 marked the completion of Edward I of Englands conquest of Wales, though Owain Glyndŵr briefly restored independence to Wales in the early 15th century. The whole of Wales was annexed by England and incorporated within the English legal system under the Laws in Wales Acts 1535–1542, distinctive Welsh politics developed in the 19th century. Welsh Liberalism, exemplified in the early 20th century by Lloyd George, was displaced by the growth of socialism, Welsh national feeling grew over the century, Plaid Cymru was formed in 1925 and the Welsh Language Society in 1962. Established under the Government of Wales Act 1998, the National Assembly for Wales holds responsibility for a range of devolved policy matters, two-thirds of the population live in south Wales, mainly in and around Cardiff, Swansea and Newport, and in the nearby valleys. Now that the countrys traditional extractive and heavy industries have gone or are in decline, Wales economy depends on the sector, light and service industries. Wales 2010 gross value added was £45.5 billion, over 560,000 Welsh language speakers live in Wales, and the language is spoken by a majority of the population in parts of the north and west. From the late 19th century onwards, Wales acquired its popular image as the land of song, Rugby union is seen as a symbol of Welsh identity and an expression of national consciousness. The Old English-speaking Anglo-Saxons came to use the term Wælisc when referring to the Celtic Britons in particular, the modern names for some Continental European lands and peoples have a similar etymology. The modern Welsh name for themselves is Cymry, and Cymru is the Welsh name for Wales and these words are descended from the Brythonic word combrogi, meaning fellow-countrymen. The use of the word Cymry as a self-designation derives from the location in the post-Roman Era of the Welsh people in modern Wales as well as in northern England and southern Scotland. It emphasised that the Welsh in modern Wales and in the Hen Ogledd were one people, in particular, the term was not applied to the Cornish or the Breton peoples, who are of similar heritage, culture, and language to the Welsh. The word came into use as a self-description probably before the 7th century and it is attested in a praise poem to Cadwallon ap Cadfan c. 633. Thereafter Cymry prevailed as a reference to the Welsh, until c.1560 the word was spelt Kymry or Cymry, regardless of whether it referred to the people or their homeland. The Latinised forms of names, Cambrian, Cambric and Cambria, survive as lesser-used alternative names for Wales, Welsh
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