The Scottish Borders is one of 32 council areas of Scotland. It borders the City of Edinburgh and Galloway, East Lothian, South Lanarkshire, West Lothian and, to the south-west and east, the English counties of Cumbria and Northumberland; the administrative centre of the area is Newtown St Boswells. The term Scottish Borders is used to designate the areas of southern Scotland and northern England that bound the Anglo-Scottish border; the Scottish Borders are in the eastern part of the Southern Uplands. The region is hilly and rural, with the River Tweed flowing west to east through it. In the east of the region, the area that borders the River Tweed is flat and is known as'The Merse'; the Tweed and its tributaries drain the entire region with the river flowing into the North Sea at Berwick-upon-Tweed, forming the border with England for the last twenty miles or so of its length. The term Central Borders refers to the area in which the majority of the main towns of Galashiels, Hawick, Earlston, Newtown St. Boswells, St Boswells, Peebles and Tweedbank are located.
Two of Scotland's 40 national scenic areas lie within the region: The Eildon and Leaderfoot National Scenic Area covers the scenery surrounding Eildon Hill, extends to include the town of Melrose and Leaderfoot Viaduct. The Upper Tweeddale National Scenic Area covers the scenery surrounding the upper part of the River Tweed between Broughton and Peebles. 2011 Galashiels: 14,994 Hawick: 14,294 Peebles: 8,376 Selkirk: 5,784 Kelso: 5,639 Jedburgh: 4,030 Eyemouth: 3,546 Innerleithen: 3,031 Duns: 2,753 Melrose: 2,307 Coldstream: 1,946 Earlston: 1,779 The term Borders has a wider meaning, referring to all of the counties adjoining the English border including Dumfriesshire and Kirkcudbrightshire – as well as Northumberland and Westmorland in England. Roxburghshire and Berwickshire bore the brunt of the conflicts with England, both during declared wars such as the Wars of Scottish Independence, armed raids which took place in the times of the Border Reivers. Thus, across the region are to be seen the ruins of many castles and towns.
The council area was created in 1975, by merging the historic counties of Berwickshire, Peeblesshire and Selkirkshire and part of Midlothian, as a two-tier region with the districts of Berwickshire and Lauderdale, Tweeddale within it. In 1996 the region became the districts were wound up; the region was created with the name Borders. Following the election of a shadow area council in 1995 the name was changed to Scottish Borders with effect from 1996. Although there is evidence of some Scottish Gaelic in the origins of place names such as Innerleithen and Longformacus, which contain identifiably Goidelic rather than Brythonic Celtic elements and are an indication of at least a Gaelic-speaking elite in the area, the main languages in the area since the 5th century appear to have been Brythonic and Old English, the latter of which developed into its modern forms of English and Scots. There are two British Parliamentary constituencies in the Borders. Berwickshire and Selkirk covers most of the region and is represented by John Lamont of the Conservatives.
The western Tweeddale area is included in the Dumfriesshire, Clydesdale & Tweeddale constituency and is represented by David Mundell of the Conservatives. At Scottish Parliament level, there are two seats; the eastern constituency is Ettrick and Berwickshire, represented by Conservative Rachael Hamilton. The western constituency is Midlothian South and Lauderdale and is represented by SNP Christine Grahame. Following the 2012 local elections, the council administration was a coalition of Independents, Scottish National Party and Liberal Democrats. Prior to the election a coalition of Conservatives, Liberal Democrats and Independents ruled; the Conservatives were the biggest party on the council with 10 seats, the Liberal Democrats had six. The SNP had nine seats and the Independents had seven. Two councillors form the Borders Party. Following the 2017 local elections, the council is now a coalition of Independents and Conservatives; the Conservatives became the largest party on the council with 15, an increase of 5.
At the Census held on 27 March 2011, the population of the region was 114,000, an increase of 6.78% from the 106,764 enumerated at the previous Census. The region had until September 2015 no working railway stations. Although the area was well connected to the Victorian railway system, the branch lines that supplied it were closed in the decades following the Second World War. A bill was passed by the Scottish Parliament to extend the Waverley Line, which aimed to re-introduce a commuter service from Edinburgh to Stow and Tweedbank; this section of the route re-opened on 6 September 2015, under the Borders Railway branding. The other railway route running through the region is the East Coast Main Line, with Edinburgh Waverley and Berwick being the nearest stations on that line, all of which are outwith the Borders. Since 2014 there has been discussion of re-opening the station at Reston, within the region and would serve Eyemouth. To the west, Carlisle and Lockerbie are the nearest stations on the West Coast Main Line.
The area is served by buses. Express bus services link the main towns with rail stations at Edinburgh and
Otterburn Training Area
The Otterburn Army Training Estate is a military training area near Otterburn, Northumberland, in northern England. It is owned by the UK's Ministry of Defence and operated by Landmarc on contract from the MoD's Defence Infrastructure Organisation; the is used for training up to 30,000 soldiers per year. The site was established in 1911 and covers about 242 square kilometres of the southern Cheviot Hills. Otterburn is the UK's largest firing range, is in frequent use: artillery can be heard from Lindisfarne to the northeast and Fontburn to the south; the ranges are used by M270 Multiple Launch Rocket Systems. The training area accounts for 23% of the Northumberland National Park; because of the danger posed by live fire exercises, recreational use of the area is restricted, although it is possible for the public access use some parts of the estate subject to the relevant bylaws. The MoD publishes Walks on Ministry of Defence Lands, which offers advice on this matter. DTE Otterburn - Public information leaflet, Defence Estates, Ministry of Defence Otterburn firing times, Defence Infrastructure Organisation, Ministry of Defence
Hedgehope Hill is a mountain in the Cheviot Hills of north Northumberland in northeast England, categorised as a Hewitt. At a height of 714 metres and a distance of about 3 miles from the Scottish border, it is best climbed from Langleeford in the Harthope Valley, over which it looms; the Harthope valley is accessible by a minor road from near Wooler to the northeast. A gentler climb, though a longer distance, is from Linhope in the Breamish valley, approaching from the south east. An alternative route to the summit could involve a long day's climb of both the Cheviot and Hedgehope Hill and finishing at Langleeford, it is a steep climb from any approach, best reserved for fitter walkers though the steepest inclines are not long in distance. Hedgehope has steeper sides than the taller but flatter-topped Cheviot and affords excellent views on all sides. On a clear day, views stretch to Blyth down the coastline up to 40 miles away
England is a country, part of the United Kingdom. It shares land borders with Wales to Scotland to the north-northwest; the Irish Sea lies west of England and the Celtic Sea lies to the southwest. England is separated from continental Europe by the North Sea to the east and the English Channel to the south; the country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Palaeolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century, since the Age of Discovery, which began during the 15th century, has had a significant cultural and legal impact on the wider world; the English language, the Anglican Church, English law – the basis for the common law legal systems of many other countries around the world – developed in England, the country's parliamentary system of government has been adopted by other nations.
The Industrial Revolution began in 18th-century England, transforming its society into the world's first industrialised nation. England's terrain is chiefly low hills and plains in central and southern England. However, there is upland and mountainous terrain in the west; the capital is London, which has the largest metropolitan area in both the United Kingdom and the European Union. England's population of over 55 million comprises 84% of the population of the United Kingdom concentrated around London, the South East, conurbations in the Midlands, the North West, the North East, Yorkshire, which each developed as major industrial regions during the 19th century; the Kingdom of England – which after 1535 included Wales – ceased being a separate sovereign state on 1 May 1707, when the Acts of Union put into effect the terms agreed in the Treaty of Union the previous year, resulting in a political union with the Kingdom of Scotland to create the Kingdom of Great Britain. In 1801, Great Britain was united with the Kingdom of Ireland 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 and Northern Ireland. 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 Anglia peninsula in the Bay of Kiel area of the Baltic Sea; the earliest recorded use of the term, as "Engla londe", is in the late-ninth-century translation into Old English of Bede's Ecclesiastical History of the English People. The term was used in a different sense to the modern one, meaning "the land inhabited by the English", it included English people in what is now south-east Scotland but was part of the English kingdom of Northumbria; the Anglo-Saxon Chronicle recorded that the Domesday Book of 1086 covered the whole of England, meaning the English kingdom, but a few years the Chronicle stated that King Malcolm III went "out of Scotlande into Lothian in Englaland", thus using it in the more ancient sense.
According to the Oxford English Dictionary, its modern spelling was first used in 1538. The earliest attested reference to the Angles occurs in the 1st-century work by Tacitus, Germania, in which the Latin word Anglii is used; the etymology of the tribal name itself is disputed by scholars. How and why a term derived from the name of a tribe, less significant than others, such as the Saxons, came to be used for the entire country and its people is not known, but it seems this is related to the custom of calling the Germanic people in Britain Angli Saxones or English Saxons to distinguish them from continental Saxons of Old Saxony between the Weser and Eider rivers in Northern Germany. In Scottish Gaelic, another language which developed on the island of Great Britain, the Saxon tribe gave their name to the word for England. An alternative name for England is Albion; the name Albion referred to the entire island of Great Britain. The nominally earliest record of the name appears in the Aristotelian Corpus the 4th-century BC De Mundo: "Beyond the Pillars of Hercules is the ocean that flows round the earth.
In it are two large islands called Britannia. But modern scholarly consensus ascribes De Mundo not to Aristotle but to Pseudo-Aristotle, i.e. it was written in the Graeco-Roman period or afterwards. The word Albion or insula Albionum has two possible origins, it either derives from a cognate of the Latin albus meaning white, a reference to the white cliffs of Dover or from the phrase the "island of the Albiones" in the now lost Massaliote Periplus, attested through Avienus' Ora Maritima to which the former served as a source. Albion is now applied to England in a more poetic capacity. Another romantic name for England is Loegria, related to the Welsh word for England and made popular by its use in Arthurian legend; the earliest known evidence of human presence in the area now known as England was that of Homo antecessor, dating to approximate
The River Tyne is a river in North East England and its length is 73 miles. It is formed by the confluence of two rivers: the South Tyne; these two rivers converge at Warden Rock near Hexham in Northumberland at a place dubbed'The Meeting of the Waters'. The Tyne Rivers Trust measure the whole Tyne catchment as 2,936 square kilometres, containing around 4,399 kilometres of waterways; the North Tyne rises on the Scottish border, north of Kielder Water. It flows through Kielder Forest, in and out of the border, it passes through the village of Bellingham before reaching Hexham. The South Tyne rises on Alston Moor and flows through the towns of Haltwhistle and Haydon Bridge, in a valley called the Tyne Gap. Hadrian's Wall lies to the north of the Tyne Gap. Coincidentally the source of the South Tyne is close to the sources of the other two great rivers of the industrial north east namely the Tees and the Wear; the South Tyne Valley falls within the North Pennines Area of Outstanding Natural Beauty - the second largest of the 40 AONBs in England and Wales.
The combined Tyne flows from the convergence point at Warden Rock just to the north west of Hexham, the area where the river's now thriving barbel stocks were first introduced in the mid-1980s, through Corbridge in Northumberland. It enters the county of Tyne and Wear between Clara Vale and Tyne Riverside Country Park and continues to divide Newcastle and Gateshead for 13 miles, in the course of which it is spanned by 10 bridges. To the east of Gateshead and Newcastle, the Tyne divides Hebburn and Jarrow on the south bank from Walker and Wallsend on the north bank. Jarrow and Wallsend are linked underneath the river by the Tyne Tunnel, it flows between South Shields and Tynemouth into the North Sea. The late Thomas John Taylor supposed that the main course of the river anciently flowed through what is now Team Valley, its outlet into the tidal river being by a waterfall at Bill Point, his theory is not far from the truth, as there is evidence that prior to the last Ice Age, the River Wear did once follow the current route of the lower River Team, merging with the Tyne at Dunston.
Ice diverted the course of the Wear to its current location, flowing east the course of the Tyne) and joining the North Sea at Sunderland. The River Tyne is believed to be around 30 million years old; the conservation of the Tyne has been handled by various bodies over the past 500 years. Conservation bodies have included: Newcastle Trinity House, the Tyne Improvement Commission; the Tyne Improvement Commission conservation lasted from 1850 until 1968. The 1850-1950 era was the worst period for pollution of the river; the Tyne Improvement Commission laid the foundations for what has become the modern day Port of Tyne. Under the management of the Tyne Improvement Commissioners, over a period of the first 70 years the Tyne was deepened from 1.83 to 9.14 meters and had 150 million tonnes dredged from it. Inside these 70 years, the two Tyne piers were built; this infrastructure enabled millions of tonnes of cargo to be handled by the Port by 1910. As of 2019 the tidal river is now managed by the Port of Tyne Authority, has been managed by the Port of Tyne Authority since 1968.
With its proximity to surrounding coalfields, the Tyne was a major route for the export of coal from the 13th century until the decline of the coal mining industry in North East England in the second half of the 20th century. The largest coal staithes were located at Dunston in Gateshead and Tyne Dock, South Shields; the dramatic wooden staithes at Dunston, built in 1890, have been preserved, although they were destroyed by fire in 2006. In 2016, Tyne Dock, South Shields was still involved with coal, importing 2 million tonnes of shipments a year; the lower reaches of the Tyne were, in the late 19th and early 20th centuries, one of the world's most important centres of shipbuilding, there are still shipyards in South Shields and Hebburn to the south of the river. To support the shipbuilding and export industries of Tyneside, the lower reaches of the river were extensively remodelled during the second half of the 19th century, with islands removed and meanders in the river straightened. Nothing definite is known of the origin of the designation Tyne, nor is the river known by that name until the Saxon period: Tynemouth is recorded in Anglo-Saxon as Tinanmuðe.
There is a theory that *tīn was a word that meant "river" in the local Celtic language or in a language spoken in England before the Celts came: compare Tardebigge. There is a river Tyne that rises in Midlothian in Scotland and flows through East Lothian into the North Sea; the River Vedra on the Roman map of Britain may be the River Wear. A supposed pre-Celtic root *tei, meaning'to melt, to flow' has been proposed as an etymological explanation of the Tyne and similarly-named rivers, as has a Brittonic derivative of Indo-European *teihx, meaning'to be dirty'. Shields Ferry New Tyne Tunnel Old Tyne Tunnel Tyne Pedestrian & Cycle Tunnel Gateshead Millennium Bridge Tyne Bridge Swing Bridge High Level Bridge Queen Elizabeth II Metro Bridge King Edward VII Bridge Redheugh Bridge Scotswood Bridge Scotswood Railway Bridge (disused rail, now carries water and gas ma
Quaternary is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy. It follows the Neogene Period and spans from 2.588 ± 0.005 million years ago to the present. The Quaternary Period is divided into two epochs: the Holocene; the informal term "Late Quaternary" refers to the past 0.5–1.0 million years. The Quaternary Period is defined by the cyclic growth and decay of continental ice sheets associated with Milankovitch cycles and the associated climate and environmental changes that occurred. In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders"; the term "quaternary" was introduced by Jules Desnoyers in 1829 for sediments of France's Seine Basin that seemed to be younger than Tertiary Period rocks. The Quaternary Period extends to the present; the Quaternary covers the time span of glaciations classified as the Pleistocene, includes the present interglacial time-period, the Holocene.
This places the start of the Quaternary at the onset of Northern Hemisphere glaciation 2.6 million years ago. Prior to 2009, the Pleistocene was defined to be from 1.805 million years ago to the present, so the current definition of the Pleistocene includes a portion of what was, prior to 2009, defined as the Pliocene. Quaternary stratigraphers worked with regional subdivisions. From the 1970s, the International Commission on Stratigraphy tried to make a single geologic time scale based on GSSP's, which could be used internationally; the Quaternary subdivisions were defined based on biostratigraphy instead of paleoclimate. This led to the problem that the proposed base of the Pleistocene was at 1.805 Mya, long after the start of the major glaciations of the northern hemisphere. The ICS proposed to abolish use of the name Quaternary altogether, which appeared unacceptable to the International Union for Quaternary Research. In 2009, it was decided to make the Quaternary the youngest period of the Cenozoic Era with its base at 2.588 Mya and including the Gelasian stage, considered part of the Neogene Period and Pliocene Epoch.
The Anthropocene has been proposed as a third epoch as a mark of the anthropogenic impact on the global environment starting with the Industrial Revolution, or about 200 years ago. The Anthropocene is not designated by the ICS, but a working group has been working on a proposal for the creation of an epoch or sub-period; the 2.6 million years of the Quaternary represents the time during which recognizable humans existed. Over this geologically short time period, there has been little change in the distribution of the continents due to plate tectonics; the Quaternary geological record is preserved in greater detail than that for earlier periods. The major geographical changes during this time period included the emergence of the Strait of Bosphorus and Skagerrak during glacial epochs, which turned the Black Sea and Baltic Sea into fresh water, followed by their flooding by rising sea level; the current extent of Hudson Bay, the Great Lakes and other major lakes of North America are a consequence of the Canadian Shield's readjustment since the last ice age.
The climate was one of periodic glaciations with continental glaciers moving as far from the poles as 40 degrees latitude. There was a major extinction of large mammals in Northern areas at the end of the Pleistocene Epoch. Many forms such as saber-toothed cats, mastodons, etc. became extinct worldwide. Others, including horses and American cheetahs became extinct in North America. Glaciation took place during the Quaternary Ice Age – a term coined by Schimper in 1839 that began with the start of the Quaternary about 2.58 Mya and continues to the present day. In 1821, a Swiss engineer, Ignaz Venetz, presented an article in which he suggested the presence of traces of the passage of a glacier at a considerable distance from the Alps; this idea was disputed by another Swiss scientist, Louis Agassiz, but when he undertook to disprove it, he ended up affirming his colleague's hypothesis. A year Agassiz raised the hypothesis of a great glacial period that would have had long-reaching general effects.
This idea led to the establishment of the Glacial Theory. In time, thanks to the refinement of geology, it has been demonstrated that there were several periods of glacial advance and retreat and that past temperatures on Earth were different from today. In particular, the Milankovitch cycles of Milutin Milankovitch are based on the premise that variations in incoming solar radiation are a fundamental factor controlling Earth's climate. During this time, substantial glaciers advanced and retreated over much of North America and Europe, parts of South America and Asia, all of Antarctica; the Great Lakes formed and giant mammals thrived in parts of North America and Eurasia not covered in ice. These mammals became extinct. Modern humans evolved about 315,000 years ago. During the Quaternary Period, flowering plants, insects dominated