Wales is a country, 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, the Bristol Channel to the south, 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, its highest summit; the country has a changeable, maritime climate. Welsh national identity emerged among the Britons after the Roman withdrawal from Britain in the 5th century, Wales is regarded as one of the modern Celtic nations. Llywelyn ap Gruffudd's death in 1282 marked the completion of Edward I of England's conquest of Wales, though Owain Glyndŵr 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 and 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 and the Labour Party.
Welsh national feeling grew over the century. Established under the Government of Wales Act 1998, the National Assembly for Wales holds responsibility for a range of devolved policy matters. At the dawn of the Industrial Revolution, development of the mining and metallurgical industries transformed the country from an agricultural society into an industrial nation. Two-thirds of the population live in South Wales, including Cardiff, Swansea and the nearby valleys. Now that the country's traditional extractive and heavy industries have gone or are in decline, Wales' economy depends on the public sector and service industries and tourism. Although Wales shares its political and social history with the rest of Great Britain, a majority of the population in most areas speaks English as a first language, the country has retained a distinct cultural identity and is bilingual. Over 560,000 Welsh language speakers live in Wales, 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", in part due to the eisteddfod tradition. At many international sporting events, such as the FIFA World Cup, Rugby World Cup and the Commonwealth Games, Wales has its own national teams, though at the Olympic Games, Welsh athletes compete as part of a Great Britain team. Rugby union is seen as an expression of national consciousness; the English words "Wales" and "Welsh" derive from the same Germanic root, itself derived from the name of the Gaulish people known to the Romans as Volcae and which came to refer indiscriminately to all non-Germanic peoples. The Old English-speaking Anglo-Saxons came to use the term Wælisc when referring to the Britons in particular, Wēalas when referring to their lands; the modern names for some Continental European lands and peoples have a similar etymology. In Britain, the words were not restricted to modern Wales or to the Welsh but were used to refer to anything that the Anglo-Saxons associated with the Britons, including other non-Germanic territories in Britain and places in Anglo-Saxon territory associated with Britons, as well as items associated with non-Germanic Europeans, such as the walnut.
The modern Welsh name for themselves is Cymry, Cymru is the Welsh name for Wales. 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, different from other peoples. In particular, the term was not applied to the Cornish or the Breton peoples, who are of similar heritage and language to the Welsh; the word came into use as a self-description before the 7th century. It is attested in a praise poem to Cadwallon ap Cadfan c. 633. In Welsh literature, the word Cymry was used throughout the Middle Ages to describe the Welsh, though the older, more generic term Brythoniaid continued to be used to describe any of the Britonnic peoples and was the more common literary term until c. 1200. 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 these names, Cambrian and Cambria, survive as lesser-used alternative names for Wales and the Welsh people. Examples include the Cambrian Mountains, the newspaper Cambrian News, the organisations Cambrian Airways, Cambrian Railways, Cambrian Archaeological Association and the Royal Cambrian Academy of Art. Outside Wales, a related form survives as the name Cumbria in North West England, once a part of Yr Hen Ogledd; the Cumbric language, thought to
A mountain range or hill range is a series of mountains or hills ranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form and alignment that have arisen from the same cause an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are found on many planetary mass objects in the Solar System and are a feature of most terrestrial planets. Mountain ranges are segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not 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, volcanic landforms resulting in a variety of rock types. Most geologically young mountain ranges on the Earth's land surface are associated with either the Pacific Ring of Fire or the Alpide Belt.
The Pacific Ring of Fire includes the Andes of South America, extends through the North American Cordillera along the Pacific Coast, the Aleutian Range, on through Kamchatka, Taiwan, the Philippines, Papua New Guinea, to New Zealand. The Andes is 7,000 kilometres long and is considered the world's longest mountain system; the Alpide belt includes Indonesia and Southeast Asia, through the Himalaya, Caucasus Mountains, Balkan Mountains fold mountain range, the Alps, ends in the Spanish mountains and the Atlas Mountains. The belt includes other European and Asian mountain ranges; the Himalayas contain the highest mountains in the world, including Mount Everest, 8,848 metres high and traverses the border between China and Nepal. Mountain ranges outside these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Great Dividing Range, the Altai Mountains and the Hijaz Mountains. If the definition of a mountain range is stretched to include underwater mountains the Ocean Ridges form the longest continuous mountain system on Earth, with a length of 65,000 kilometres.
The mountain systems of the earth are characterized by a tree structure, where mountain ranges can contain sub-ranges. The sub-range relationship is 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, the White Mountains and the Blue Ridge Mountains are children of the Appalachians; the parent-child expression extends to the sub-ranges themselves: the Sandwich Range and the Presidential Range are children of the White Mountains, while the Presidential Range is parent to the Northern Presidential Range and Southern Presidential Range. The position of mountains influences climate, such as snow; when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the leeward side, it warms again and is drier, having been stripped of much of its moisture.
A rain shadow will affect the leeward side of a range. Mountain ranges are subjected to erosional forces which work to tear them down; the basins adjacent to an eroding mountain range are filled with sediments which are buried and turned into sedimentary rock. Erosion is at work while the mountains are being uplifted until the mountains are reduced to low hills and plains; the early Cenozoic uplift of the Rocky Mountains of Colorado provides an example. As the uplift was occurring some 10,000 feet of Mesozoic sedimentary strata were removed by erosion over the core of the mountain range and spread as sand and clays across the Great Plains to the east; this mass of rock was removed as the range was undergoing uplift. The removal of such a mass from the core of the range most caused further uplift as the region adjusted isostatically in response to the removed weight. Rivers are traditionally believed to be the principal cause of mountain range erosion, by cutting into bedrock and transporting sediment.
Computer simulation has shown that as mountain belts change from tectonically active to inactive, the rate of erosion drops because there are fewer abrasive particles in the water and fewer landslides. Mountains on other planets and natural satellites of the Solar System are isolated and formed by processes such as impacts, though there are examples of mountain ranges somewhat similar to those on Earth. Saturn's moon Titan and Pluto, in particular exhibit large mountain ranges in chains composed of ices rather than rock. Examples include the Mithrim Montes and Doom Mons on Titan, Tenzing Montes and Hillary Montes on Pluto; some terrestrial planets other than Earth exhibit rocky mountain ranges, such as Maxwell Montes on Venus taller than any on Earth and Tartarus Montes on Mars, Jupiter's moon Io has mountain ranges formed from tectonic processes including Boösaule Montes, Dorian Montes, Hi'iaka Montes and Euboea Montes. Peakbagger Ranges Home Page Bivouac.com
A mountain is a large landform that rises above the surrounding land in a limited area in the form of a peak. A mountain is steeper than a hill. Mountains are formed through tectonic forces or volcanism; these forces can locally raise the surface of the earth. Mountains erode through the action of rivers, weather conditions, glaciers. A few mountains are isolated summits. High elevations on mountains produce colder climates than at sea level; these colder climates affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains tend to be used less for agriculture and more for resource extraction and recreation, such as mountain climbing; the highest mountain on Earth is Mount Everest in the Himalayas of Asia, whose summit is 8,850 m above mean sea level. The highest known mountain on any planet in the Solar System is Olympus Mons on Mars at 21,171 m. There is no universally accepted definition of a mountain.
Elevation, relief, steepness and continuity have been used as criteria for defining a mountain. In the Oxford English Dictionary a mountain is defined as "a natural elevation of the earth surface rising more or less abruptly from the surrounding level and attaining an altitude which to the adjacent elevation, is impressive or notable."Whether a landform is called a mountain may depend on local usage. Mount Scott outside Lawton, Oklahoma, USA, is only 251 m from its base to its highest point. Whittow's Dictionary of Physical Geography states "Some authorities regard eminences above 600 metres as mountains, those below being referred to as hills." In the United Kingdom and the Republic of Ireland, a mountain is defined as any summit at least 2,000 feet high, whilst the official UK government's definition of a mountain, for the purposes of access, is a summit of 600 metres or higher. In addition, some definitions include a topographical prominence requirement 100 or 500 feet. At one time the U.
S. Board on Geographic Names defined a mountain as being 1,000 feet or taller, but has abandoned the definition since the 1970s. Any similar landform lower. However, the United States Geological Survey concludes that these terms do not have technical definitions in the US; the UN Environmental Programme's definition of "mountainous environment" includes any of the following: Elevation of at least 2,500 m. Using these definitions, mountains cover 33% of Eurasia, 19% of South America, 24% of North America, 14% of Africa; as a whole, 24% of the Earth's land mass is mountainous. There are three main types of mountains: volcanic and block. All three types are formed from plate tectonics: when portions of the Earth's crust move and dive. Compressional forces, isostatic uplift and intrusion of igneous matter forces surface rock upward, creating a landform higher than the surrounding features; the height of the feature makes it either a hill or, if steeper, a mountain. Major mountains tend to occur in long linear arcs, indicating tectonic plate boundaries and activity.
Volcanoes are formed when a plate is pushed at a mid-ocean ridge or hotspot. At a depth of around 100 km, melting occurs in rock above the slab, forms magma that reaches the surface; when the magma reaches the surface, it builds a volcanic mountain, such as a shield volcano or a stratovolcano. Examples of volcanoes include Mount Pinatubo in the Philippines; the magma does not have to reach the surface in order to create a mountain: magma that solidifies below ground can still form dome mountains, such as Navajo Mountain in the US. Fold mountains occur when two plates collide: shortening occurs along thrust faults and the crust is overthickened. Since the less dense continental crust "floats" on the denser mantle rocks beneath, the weight of any crustal material forced upward to form hills, plateaus or mountains must be balanced by the buoyancy force of a much greater volume forced downward into the mantle, thus the continental crust is much thicker under mountains, compared to lower lying areas.
Rock can fold either asymmetrically. The upfolds are anticlines and the downfolds are synclines: in asymmetric folding there may be recumbent and overturned folds; the Balkan Mountains and the Jura Mountains are examples of fold mountains. Block mountains are caused by faults in the crust: a plane; when rocks on one side of a fault rise relative to the other, it can form a mountain. The uplifted blocks are block horsts; the intervening dropped blocks are termed graben: these can be small or form extensive rift valley systems. This form of landscape can be seen in East Africa, the Vosges, the Basin and Range Province of Western North America and the Rhine valley; these areas occur when the regional stress is extensional and the crust is thinned. During and following uplift, mountains are subjected to the agents of erosion which wear the uplifted area down. Erosion causes the surface of mountains to be younger than the rocks that form the mountains themselves. Glacial processes produce characteristic landforms, such as pyramidal peaks, knife-edge arêtes, bowl-shaped cirques that can contai
A unitary authority is a type of local authority that has a single tier and is responsible for all local government functions within its area or performs additional functions which elsewhere in the relevant country are performed by national government or a higher level of sub-national government. Unitary authorities cover towns or cities which are large enough to function independently of county or other regional administration. Sometimes they consist of national sub-divisions which are distinguished from others in the same country by having no lower level of administration. In Canada, each province creates its own system of local government, so terminology varies substantially. In certain provinces there is only one level of local government in that province, so no special term is used to describe the situation. British Columbia has only one such municipality, Northern Rockies Regional Municipality, established in 2009. In Ontario the term single-tier municipalities is used, for a similar concept.
Their character varies, while most function as cities with no upper level of government, some function as counties or regional municipalities with no lower municipal subdivisions below them. They exist as individual census divisions, as well as separated municipalities. In Germany, kreisfreie Stadt is the equivalent term for a city with the competences of both the Gemeinde and the Kreis administrative level; the directly elected chief executive officer of a kreisfreie Stadt is called Oberbürgermeister. The British counties have no directly corresponding counterpart in Germany; this German system corresponds in the Czech Republic. Until 1 January 2007, the municipalities of Copenhagen and Bornholm were not a part of a Danish county. In New Zealand, a unitary authority is a territorial authority that performs the functions of a regional council. There are five unitary authorities; the Chatham Islands, located east of the South Island, have a council with its own special legislation, constituted with powers similar to those of a regional authority.
In Poland, a miasto na prawach powiatu, or shortly powiat grodzki is a big, city, responsible for district administrative level, being part of no other powiat. In total, 65 cities in Poland have this status. In the United Kingdom, "unitary authorities" are English local authorities set up in accordance with the Local Government Changes for England Regulations 1994 made under powers conferred by the Local Government Act 1992 to form a single tier of local government in specified areas and which are responsible for all local government functions within such areas. While outwardly appearing to be similar, single-tier authorities formed using older legislation are not Unitary Authorities thus excluding e.g. the Isle of Wight Council or any other single-tier authority formed under the Local Government Act 1972 or older legislation. This is distinct from the two-tier system of local government which still exists in most of England, where local government functions are divided between county councils and district or borough councils.
Until 1996 two-tier systems existed in Scotland and Wales, but these have now been replaced by systems based on a single-tier of local government with some functions shared between groups of adjacent authorities. A single-tier system has existed in Northern Ireland since 1973. For many years the description of the number of tiers in UK local government arrangements has ignored any current or previous bodies at the lowest level of authorities elected by the voters within their area such as parish or community councils. Northern Ireland is divided into 11 districts for local government purposes. In Northern Ireland local councils have no responsibility for road building or housing, their functions include waste and recycling services and community services, building control and local economic and cultural development. Since their reorganisation in 2015 councils in Northern Ireland have taken on responsibility for planning functions; the collection of rates is handled by the Property Services agency.
Category: Subdivisions of Northern Ireland Local authorities in Scotland are unitary in nature but not in name. The Local Government etc. Act 1994 created a single tier of local government throughout Scotland. On 1 April 1996, 32 local government areas, each with a council, replaced the previous two-tier structure, which had regional and district councils. Comhairle nan Eilean Siar uses the alternative Gaelic designation Comhairle; the phrase "unitary authority" is not used in Scottish legislation, although the term is encountered in publications and in use by United Kingdom government departments. Local authorities in Wales are unitary in nature but are described by the Local Government Act 1994 as "principal councils", their areas as principal areas. Various other legislation (e.g. s.9
Moel Fferna is a mountain in Denbighshire and forms part of the Berwyn range. It is the most northern outpost of the range; the summit has a shelter cairn. A trig point has since been destroyed. To the south is Pen Bwlch Llandrillo, followed by Cadair Bronwen
Wrexham County Borough
Wrexham County Borough is a local government principal area centred on the town of Wrexham in northeast Wales. The county borough has a population of nearly 135,000 inhabitants. Around 63,000 of these live either within the town of Wrexham or in the surrounding conurbation of urban villages; the remainder live to the south and east of the town in more rural areas, including the borough's large salient in the Ceiriog Valley. The area has strong links with coal-mining; the county borough was formed on 1 April 1996. Borough status was inherited from the town of Wrexham, granted over 150 years ago. Most of the area was part of the district of Wrexham Maelor – with several communities coming from Glyndŵr – in the county of Clwyd; the area includes a portion of the eastern half of the historic county of Denbighshire, two exclaves of historic Flintshire: English Maelor and the parish of Marford and Hoseley. The region is governed as a unitary authority by Wrexham County Borough Council. Most offices of the council are situated within Wrexham town centre, around Llwyn Isaf and the Civic Centre around Chester Street.
The headquarters of the organisation is at Queens Square. Wrexham County Borough forms part of the Wales constituency, which elects four members to the European Parliament using the d'Hondt method of party-list proportional representation. Top performing Secondary schools in Wrexham County Borough. Percentages are those achieving at least 5 GCSEs at grades A*-C, according to the latest inspection report by Estyn. All schools English medium unless stated: *Incomplete secondary school which does not have a Sixth Form Iserlohn, Germany Racibórz, PolandWrexham is twinned with the German district of Märkischer Kreis and the Polish town of Racibórz; the first twinning was established on 17 March 1970 between the former Kreis Iserlohn and Wrexham Rural District. Its early success ensured that, after local government reorganisation in both countries in the mid-seventies, the twinning was taken over by the new councils of Märkischer Kreis and Wrexham Maelor Borough Council and, in 1996, by Wrexham County Borough Council.
In 2001 Märkischer Kreis entered a twinning arrangement with Racibórz, a county in Poland, part of Silesia, Germany. In September 2002, a delegation from Racibórz visited Wrexham and began discussions about co-operation which led to the signing of Articles of Twinning between Wrexham and Racibórz in March 2004; the Wrexham area has strong historical links with Poland. Following World War II, many service personnel from the Free Polish armed forces, injured received treatment at Penley Polish Hospital. Many of their descendants remain in the area. List of places in Wrexham County Borough for a list of towns and villages Wrexham County Borough at Curlie Wrexham County Borough Council Website Electoral Arrangements Order 1998 – description of Wards Wrexham Council Ward Map Wrexham.com Website North Wales Police Wrexham Ward Map NHS Review of substance misuse including Ward Deprivation Map and detailed population/age group figures
North Wales is a region of Wales. Retail and educational infrastructure are centred on Wrexham, Colwyn Bay and Bangor, it is bordered to the rest of Wales with the counties of Ceredigion and Powys, to the east by the English counties of Shropshire and Cheshire. North Wales was traditionally divided into three regions: Upper Gwynedd, defined as the area north of the River Dyfi and west of the River Conwy); the division with the rest of Wales depends on the particular use being made. For example, the boundary of North Wales Police differs from the boundary of the North Wales area of the Natural Resources Wales and the North Wales Regional Transport Consortium; the historic boundary follows the pre-1996 county boundaries of Merionethshire and Denbighshire which in turn follows the geographic features of the river Dovey to Aran Fawddwy crossing the high moorlands following the watershed until reaching Cadair Berwyn and following the river Rhaeadr and river Tanat to the Shropshire border. Montgomeryshire, one of the historic counties of Wales, is sometimes referred to as being in North Wales.
The region is steeped in history and was for a millennium known as the Kingdom of Gwynedd. The mountainous stronghold of Snowdonia formed the nucleus of that realm and would become the last redoubt of independent Wales — only overcome in 1283. To this day it remains a stronghold of the Welsh language and a centre for Welsh national and cultural identity; the area is home to two of the three UNESCO World Heritage Sites in Wales. These are Pontcysyllte Aqueduct and canal and, the Edwardian castles and town walls of the region which comprise those at Caernarfon, Beaumaris and Harlech, it shares with Powys and Ceredigion the distinction of hosting the only UNESCO Biosphere reserve in Wales, Biosffer Dyfi Biosphere. The region is made up of the following administrative areas: the county borough of Wrexham the county of Flintshire the county of Denbighshire the county borough of Conwy the county of Gwynedd the county of the Isle of Anglesey In addition to the six Local Authority divisions, North Wales is divided into the following preserved counties for various ceremonial purposes: the preserved county of Clwyd the preserved county of Gwynedd North Wales was a European Parliament constituency until 1999.
There is an electoral region for the National Assembly for Wales with the name, which covers the northeast of Wales as well as the northern-most coastal areas of north-western Wales. The area is rural with many mountains and valleys. This, in combination with its coast, means. Farming, once the principal economic force in the area, is now much reduced in importance; the average income per capita of the local population is the lowest in the UK and much of the region has EU Objective 1 status. The eastern part of North Wales contains the most populous areas, with more than 300,000 people living in the areas around Wrexham and Deeside. Wrexham, with a population of 63,084 in 2001 is the largest town; the total population of North Wales is 687,937. The majority of other settlements are along the coast, including some popular resort towns, such as Rhyl, Llandudno and Tywyn; the A55 road links these towns to cities like Manchester and Birmingham and the port of Holyhead for ferries to Ireland. There are two cathedral cities – Bangor and St. Asaph – and a number of mediaeval castles The area of North Wales is about 6,172 square kilometres, making it larger than the country of Brunei, or the island of Bali.
The highest mountain in Wales and Ireland, is Snowdon in northwest Wales. North Wales has a diverse and complex geology with Precambrian schists along the Menai Strait and the great Cambrian dome behind Harlech and underlying much of western Snowdonia. In the Ordovician period much volcanism deposited a range of minerals and rocks over the north western parts of Gwynedd whilst to the east of the River Conwy lies a large area of upland rolling hills underlain by the Silurian mudstones and grits comprising the Denbigh and Migneint Moors. To the east, around Llangollen, to the north on Halkyn Mountain and the Great Orme and in eastern Anglesey are beds of limestone from which metals have been mined since pre-Roman times. Added to all this are the complexities posed by Parys Mountain and the outcrops of unusual minerals such as Jasper and Mona Marble which make the area of special interest to geologists. North Wales has a distinct regional identity, its dialect of the Welsh language differs from that of other regions, such as South Wales, in some ways: for example llefrith is used in most of the North instead of llaeth for "milk".