84-593: The Culter Hills , Coulter Fells or variations thereof, are a range of hills, part of the Southern Uplands of Scotland . They are neighboured to the east by the Manor Hills and are split roughly in half by the border between South Lanarkshire and the Scottish Borders . The hills form a roughly southwest–northeast rectangular shape and cover a considerable area, however the ridges within
168-571: A Tuath . The North Sea has provided waterway access for commerce and conquest. Many areas have access to the North Sea because of its long coastline and the European rivers that empty it. There is little documentary evidence concerning the North Sea before the Roman conquest of Britain in 43 CE, however, archaeological evidence reveals the diffusion of cultures and technologies from across or along
252-738: A challenge to their dominance of the North Sea until the 20th century. Tensions in the North Sea were again heightened in 1904 by the Dogger Bank incident . During the Russo-Japanese War , several ships of the Russian Baltic Fleet, which was on its way to the Far East, mistook British fishing boats for Japanese ships and fired on them, and then upon each other, near the Dogger Bank, nearly causing Britain to enter
336-621: A more natural state such as Loch Dee, Loch Enoch , Loch Grannoch and Loch Trool . To the east of Moffat is the largest natural body of water in the Borders Region of the Southern Uplands, St. Mary's Loch together with the adjacent Loch of the Lowes and nearby Loch Skeen . There are several other reservoirs in the vicinity including Megget Reservoir , Talla Reservoir and Fruid Reservoir whilst Daer Reservoir lies among
420-523: A rich source of energy resources, including wind and wave power . The North Sea has featured prominently in geopolitical and military affairs, particularly in Northern Europe , from the Middle Ages to the modern era. It was also important globally through the power northern Europeans projected worldwide during much of the Middle Ages and into the modern era. The North Sea was the centre of
504-717: A vast merchant marine, a large fishing fleet, powerful navy, and sophisticated financial markets made the Dutch the ascendant power in the North Sea, to be challenged by an ambitious England. This rivalry led to the first three Anglo-Dutch Wars between 1652 and 1673, which ended with Dutch victories. After the Glorious Revolution in 1688, the Dutch prince William ascended to the English throne. With unified leadership, commercial, military, and political power began to shift from Amsterdam to London. The British did not face
588-536: A volume of 54,000 cubic kilometres (13,000 cu mi). Around the edges of the North Sea are sizeable islands and archipelagos , including Shetland , Orkney , and the Frisian Islands . The North Sea receives freshwater from a number of European continental watersheds, as well as the British Isles . A large part of the European drainage basin empties into the North Sea, including water from
672-620: Is 17 °C (63 °F) in the summer and 6 °C (43 °F) in the winter. The average temperatures have been trending higher since 1988, which has been attributed to climate change . Air temperatures in January range on average between 0 and 4 °C (32 and 39 °F) and in July between 13 and 18 °C (55 and 64 °F). The winter months see frequent gales and storms. The salinity averages between 34 and 35 grams per litre (129 and 132 g/US gal) of water. The salinity has
756-466: Is a series of asymmetrical trenches between 20 and 30 kilometres (12 and 19 mi) long, one and two kilometres (0.6 and 1.2 mi) wide and up to 230 metres (750 ft) deep. Other areas which are less deep are Cleaver Bank , Fisher Bank and Noordhinder Bank . The International Hydrographic Organization defines the limits of the North Sea as follows: On the Southwest. A line joining
840-526: Is also home to marine mammals. Common seals , grey seals , and harbour porpoises can be found along the coasts, at marine installations, and on islands. The very northern North Sea islands such as the Shetland Islands are occasionally home to a larger variety of pinnipeds including bearded , harp , hooded and ringed seals , and even walrus . North Sea cetaceans include various porpoise , dolphin and whale species. Plant species in
924-780: Is bounded by the Orkney Islands and east coast of Great Britain to the west and the northern and central European mainland to the east and south, including Norway , Denmark , Germany , the Netherlands , Belgium , and France . In the southwest, beyond the Straits of Dover , the North Sea becomes the English Channel connecting to the Atlantic Ocean. In the east, it connects to the Baltic Sea via
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#17327940995031008-699: Is recorded to have killed more than 100,000 people. In 1362, the Second Marcellus Flood , also known as the Grote Manndrenke , hit the entire southern coast of the North Sea. Chronicles of the time again record more than 100,000 deaths, large parts of the coast were lost permanently to the sea, including the now legendary lost city of Rungholt . In the 20th century, the North Sea flood of 1953 flooded several nations' coasts and cost more than 2,000 lives. 315 citizens of Hamburg died in
1092-536: Is the Norwegian trench , which extends parallel to the Norwegian shoreline from Oslo to an area north of Bergen . It is between 20 and 30 kilometres (12 and 19 mi) wide and has a maximum depth of 725 metres (2,379 ft). The Dogger Bank , a vast moraine , or accumulation of unconsolidated glacial debris, rises to a mere 15 to 30 m (50 to 100 ft) below the surface. This feature has produced
1176-518: The Baltic Sea . The largest and most important rivers flowing into the North Sea are the Elbe and the Rhine – Meuse . Around 185 million people live in the catchment area of the rivers discharging into the North Sea encompassing some highly industrialized areas. For the most part, the sea lies on the European continental shelf with a mean depth of 90 metres (300 ft). The only exception
1260-525: The Battle of Heligoland Bight , the Battle of the Dogger Bank , and the Battle of Jutland . World War I also brought the first extensive use of submarine warfare , and a number of submarine actions occurred in the North Sea. The Second World War also saw action in the North Sea, though it was restricted more to aircraft reconnaissance and action by fighter/bomber aircraft, submarines and smaller vessels such as minesweepers and torpedo boats . After
1344-606: The Central Lowlands and the Highlands ). The term is used both to describe the geographical region and to collectively denote the various ranges of hills and mountains within this region. An overwhelmingly rural and agricultural region, the Southern Uplands are partly forested and contain many areas of open moorland - the hill names in the area are congruent with these characteristics. The Southern Uplands consist mainly of Silurian sedimentary deposits deposited in
1428-528: The English Channel was triggered by the earthquake, which in turn caused a tsunami. The tsunami triggered by the 1755 Lisbon earthquake reached Holland, although the waves had lost their destructive power. The largest earthquake ever recorded in the United Kingdom was the 1931 Dogger Bank earthquake , which measured 6.1 on the Richter magnitude scale and caused a small tsunami that flooded parts of
1512-644: The European continental shelf , it connects to the Atlantic Ocean through the English Channel in the south and the Norwegian Sea in the north. It is more than 970 kilometres (600 mi) long and 580 kilometres (360 mi) wide, covering 570,000 square kilometres (220,000 sq mi). It hosts key north European shipping lanes and is a major fishery . The coast is a popular destination for recreation and tourism in bordering countries, and
1596-538: The Galloway hydro-electric power scheme was built between 1930 and 1936. More recently a number of wind farms have been developed on upland sites. Tourism and recreation are of increasing importance: walking, fishing and grouse shooting are traditional pursuits and mountain biking has become popular in recent years. The textile industry employed large numbers in many of the towns of the Scottish Borders in
1680-589: The Iapetus Ocean 420 million years ago. These rocks were pushed up from the sea bed into an accretionary wedge during the Caledonian orogeny , roughly 400 million years ago ( Ma ), when the continents and terranes of Laurentia , Baltica and Avalonia collided. The Caledonian orogeny is named for Caledonia , a Latin name for Scotland . The majority of the rocks are weakly metamorphosed coarse greywacke . The tectonic processes involved in
1764-517: The Last Glacial Maximum when the sea began to flood the European continental shelf. In 2006 a bone fragment was found while drilling for oil in the North Sea. Analysis indicated that it was a Plateosaurus from 199 to 216 million years ago. This was the deepest dinosaur fossil ever found and the first find for Norway. Copepods and other zooplankton are plentiful in the North Sea. These tiny organisms are crucial elements of
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#17327940995031848-965: The Latin names Mare Germanicum and Oceanus Germanicus , and these persisted in use until the First World War. Other common names in use for long periods were the Latin terms Mare Frisicum , as well as the English equivalent, "Frisian Sea". The modern names of the sea in the other local languages are: Danish : Vesterhavet , lit. 'West Sea' [ˈvestɐˌhɛˀvð̩] or Nordsøen [ˈnoɐ̯ˌsøˀn̩] , Dutch : Noordzee , Dutch Low Saxon : Noordzee , French : Mer du Nord , West Frisian : Noardsee , German : Nordsee , Low German : Noordsee , North Frisian : Weestsiie , lit. 'West Sea', Swedish : Nordsjön , Bokmål : Nordsjøen [ˈnûːrˌʂøːn] , Nynorsk : Nordsjøen , Scots : North Sea and Scottish Gaelic : An Cuan
1932-472: The North Sea flood of 1962 . Though rare, the North Sea has been the site of a number of historically documented tsunamis . The Storegga Slides were a series of underwater landslides, in which a piece of the Norwegian continental shelf slid into the Norwegian Sea. The immense landslips occurred between 8150 BCE and 6000 BCE, and caused a tsunami up to 20 metres (66 ft) high that swept through
2016-1016: The Phare de Walde (Walde Lighthouse, in France, 50°59'37"N, 1°54'53"E) and Leathercoat Point (England, 51°10'01.4"N 1°24'07.8"). northeast of Dover. On the Northwest. From Dunnet Head (58°40'20"N, 3°22'30"W) in Scotland to Tor Ness (58°47'N) in the Island of Hoy , thence through this island to the Kame of Hoy (58°55'N) on to Breck Ness on Mainland (58°58'N) through this island to Costa Head (3°14'W) and Inga Ness (59'17'N) in Westray through Westray, to Bow Head, across to Mull Head (North point of Papa Westray ) and on to Seal Skerry (North point of North Ronaldsay ) and thence to Horse Island (South point of
2100-826: The Shetland Islands). On the North. From the North point (Fethaland Point) of the Mainland of the Shetland Islands, across to Graveland Ness (60°39'N) in the Island of Yell , through Yell to Gloup Ness (1°04'W) and across to Spoo Ness (60°45'N) in Unst island, through Unst to Herma Ness (60°51'N), on to the SW point of the Rumblings and to Muckle Flugga ( 60°51′N 0°53′W / 60.850°N 0.883°W / 60.850; -0.883 ) all these being included in
2184-608: The Skagerrak and Kattegat , narrow straits that separate Denmark from Norway and Sweden respectively. In the north it is bordered by the Shetland Islands , and connects with the Norwegian Sea , which is a marginal sea in the Arctic Ocean . The North Sea is more than 970 kilometres (600 mi) long and 580 kilometres (360 mi) wide, with an area of 750,000 square kilometres (290,000 sq mi) and
2268-687: The Southern Uplands Fault line that runs from Ballantrae on the Ayrshire coast northeastwards to Dunbar in East Lothian on the North Sea coast, a distance of some 220 km (140 mi). There are several ranges of hills and mountains within the Southern Uplands. From east to west these are: Although the summits are not as high as many in the Scottish Highlands nor other famous mountain regions, parts of
2352-627: The Vikings' rise . The Hanseatic League , the Dutch Republic , and the British each sought to gain command of the North Sea and access to the world's markets and resources. As Germany's only outlet to the ocean, the North Sea was strategically important through both world wars. The coast has diverse geology and geography. In the north, deep fjords and sheer cliffs mark much of its Norwegian and Scottish coastlines respectively, whereas in
2436-463: The food chain supporting many species of fish. Over 230 species of fish live in the North Sea. Cod , haddock , whiting , saithe , plaice , sole , mackerel , herring , pouting , sprat , and sandeel are all very common and are fished commercially. Due to the various depths of the North Sea trenches and differences in salinity, temperature, and water movement, some fish such as blue-mouth redfish and rabbitfish reside only in small areas of
2520-535: The littoral is low and marshy. The east coast and south-east of the North Sea ( Wadden Sea ) have coastlines that are mainly sandy and straight owing to longshore drift , particularly along Belgium and Denmark. The southern coastal areas were originally flood plains and swampy land. In areas especially vulnerable to storm surges, people settled behind elevated levees and on natural areas of high ground such as spits and geestland . As early as 500 BC, people were constructing artificial dwelling hills higher than
2604-741: The 13th century the Hanseatic League , though centred on the Baltic Sea , started to control most of the trade through important members and outposts on the North Sea. The League lost its dominance in the 16th century, as neighbouring states took control of former Hanseatic cities and outposts. Their internal conflict prevented effective cooperation and defence. As the League lost control of its maritime cities, new trade routes emerged that provided Europe with Asian, American, and African goods. The 17th century Dutch Golden Age saw Dutch maritime power at its zenith. Important overseas colonies,
Culter Hills - Misplaced Pages Continue
2688-473: The 19th and 20th centuries. Stocking frames were introduced in Hawick in 1771 and Galashiels ' first woollen mill was built in 1800, but textile manufacture had a long history in the area: linen production had been a major industry since the Middle Ages. The textile industry declined in the late 20th century, with 7,800 people employed in 1981 and only 4,400 by 1998. However, it continues to be significant both to
2772-474: The Anglo-Scottish border have a troubled and bloody history. They were the scene of many raids, campaigns and battles, including the Battle of Ancrum Moor , the Battle of Nesbit Moor and the Battle of Philiphaugh . The Common Riding festivals of many Southern Upland towns such as Jedburgh , Kelso , Hawick , Peebles , Selkirk and Langholm recall this history, re-enacting the practice of riding
2856-583: The British coast. Shallow epicontinental seas like the current North Sea have since long existed on the European continental shelf . The rifting that formed the northern part of the Atlantic Ocean during the Jurassic and Cretaceous periods, from about 150 million years ago , caused tectonic uplift in the British Isles. Since then, a shallow sea has almost continuously existed between
2940-576: The Carlisle area. Several primary roads run through the Southern Uplands, most of which run north–south, with the most notable exception being the A75. The most significant of these roads is the M74 motorway connecting Scotland and England. These roads include: Five railway lines pass through, or into, the Southern Uplands; all in a roughly north–south direction. These are the: There are no major airports within
3024-524: The Lowther Hills. The area has a wide diversity of species and habitats. The uplands support black and red grouse , mountain hares , golden eagles , hen harriers and some unusual plant species. The western hills are home to red deer , roe deer , feral goats and wild boar . The western forests have one fifth of the Scottish population of red squirrels . Ospreys are present at some of
3108-508: The Middle Ages through the 15th century, the northern European coastal ports exported domestic goods, dyes, linen, salt, metal goods and wine. The Scandinavian and Baltic areas shipped grain, fish, naval necessities, and timber. In turn, the North Sea countries imported high-grade cloths, spices, and fruits from the Mediterranean region. Commerce during this era was mainly conducted by maritime trade due to underdeveloped roadways. In
3192-486: The Netherlands. The North Sea Floods of 1953 and 1962 were the impetus for further raising of the dikes as well as the shortening of the coast line so as to present as little surface area as possible to the punishment of the sea and the storms. Currently, 27% of the Netherlands is below sea level protected by dikes, dunes, and beach flats. Coastal management today consists of several levels. The dike slope reduces
3276-926: The North Sea are home to nature reserves including the Ythan Estuary , Fowlsheugh Nature Preserve, and Farne Islands in the UK and the Wadden Sea National Parks in Denmark, Germany and the Netherlands. These locations provide breeding habitat for dozens of bird species. Tens of millions of birds make use of the North Sea for breeding, feeding, or migratory stopovers every year. Populations of black-legged kittiwakes , Atlantic puffins , northern gannets , northern fulmars , and species of petrels , seaducks , loons (divers), cormorants , gulls , auks , and terns , and many other seabirds make these coasts popular for birdwatching . The North Sea
3360-618: The North Sea area; thence up the meridian of 0°53' West to the parallel of 61°00' North and eastward along this parallel to the coast of Norway, the whole of Viking Bank is thus included in the North Sea. On the East. The Western limit of the Skagerrak [A line joining Hanstholm ( 57°07′N 8°36′E / 57.117°N 8.600°E / 57.117; 8.600 ) and the Naze ( Lindesnes , 58°N 7°E / 58°N 7°E / 58; 7 )]. The average temperature
3444-523: The North Sea during the Migration Period . They made successive invasions of the island from what is now the Netherlands, Denmark, and Germany. The Viking Age began in 793 with the attack on Lindisfarne ; for the next quarter-millennium, the Vikings ruled the North Sea. In their superior longships , they raided, traded, and established colonies and outposts along the coasts of the sea. From
Culter Hills - Misplaced Pages Continue
3528-613: The North Sea include species of wrack , among them bladder wrack , knotted wrack , and serrated wrack. Algae , macroalgal, and kelp , such as oarweed and laminaria hyperboria, and species of maerl are found as well. Eelgrass , formerly common in the entirety of the Wadden Sea, was nearly wiped out in the 20th century by a disease. Similarly, sea grass used to coat huge tracts of ocean floor, but have been damaged by trawling and dredging have diminished its habitat and prevented its return. Invasive Japanese seaweed has spread along
3612-445: The North Sea to Great Britain and Scandinavia and reliance by some prehistoric cultures on fishing, whaling, and seaborne trade on the North Sea. The Romans established organised ports in Britain, which increased shipping and began sustained trade the diffusion of cultures and technologies from across or along the North Sea to Great Britain and Scandinavia and reliance by some prehistoric cultures on fishing, whaling, and seaborne trade on
3696-416: The North Sea until the 20th century, when numbers declined due to overfishing . Other factors like the introduction of non-indigenous species , industrial and agricultural pollution , trawling and dredging , human-induced eutrophication , construction on coastal breeding and feeding grounds, sand and gravel extraction, offshore construction , and heavy shipping traffic have also contributed to
3780-420: The North Sea, having the greatest effect on Scotland and the Faeroe Islands . The Dover Straits earthquake of 1580 is among the first recorded earthquakes in the North Sea measuring between 5.6 and 5.9 on the Richter scale. This event caused extensive damage in Calais both through its tremors and possibly triggered a tsunami , though this has never been confirmed. The theory is a vast underwater landslide in
3864-399: The North Sea. Crustaceans are also commonly found throughout the sea. Norway lobster , deep-water prawns , and brown shrimp are all commercially fished, but other species of lobster , shrimp , oyster , mussels and clams all live in the North Sea. Recently non-indigenous species have become established including the Pacific oyster and Atlantic jackknife clam . The coasts of
3948-399: The North Sea. The Romans established organised ports in Britain, which increased shipping and began sustained trade and many Scandinavian tribes participated in raids and wars against the Romans and Roman coinage and manufacturing were important trade goods. When the Romans abandoned Britain in 410, the Germanic Angles , Frisians , Saxons , and Jutes began the next great migration across
4032-448: The North Sea. The wave continues to travel northward in the Atlantic Ocean, and once past the northern tip of Great Britain, the Kelvin wave turns east and south and once again enters the North Sea. The eastern and western coasts of the North Sea are jagged, formed by glaciers during the ice ages . The coastlines along the southernmost part are covered with the remains of deposited glacial sediment. The Norwegian mountains plunge into
4116-438: The Orkney Islands through the mid-16th century, as both Sable Island and Orkney Islands lay within their normal range. Grey whales also resided in the North Sea but were driven to extinction in the Atlantic in the 17th century Other species have dramatically declined in population, though they are still found. North Atlantic right whales , sturgeon , shad , rays , skates , salmon , and other species were common in
4200-471: The Southern Uplands are covered with forests such as: The amount of forested land cover in the western Southern Uplands increased greatly between the 1940s and the 1980s, from 1% to 23%. The Southern Uplands have always formed a major obstacle to travel between the more heavily populated and industrialised Central Belt of Scotland and England to the south. Major roads and railways follow the east coast route and various valley routes radiating northwards from
4284-424: The Southern Uplands are remote and mountainous, containing about 120 Marilyns , the majority of the Donalds and a substantial number of Corbetts and Grahams . Some of the more notable peaks in the Southern Uplands are: The Southern Uplands are home to the UK's second highest, and Scotland's highest, village, Wanlockhead , 430 m (1,410 ft) above sea level. The region is drained by numerous rivers,
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#17327940995034368-443: The Southern Uplands in several of his prose and verse works (such as The Lay of the Last Minstrel ), as did James Hogg , known as the Ettrick Shepherd. 55°25′N 3°17′W / 55.41°N 3.28°W / 55.41; -3.28 North Sea Download coordinates as: The North Sea lies between Great Britain , Denmark , Norway , Germany , the Netherlands , Belgium and France . An epeiric sea on
4452-422: The Southern Uplands, particularly in the west. The largest is Loch Ken the water lever of the loch was increased in 1936 when the Glenlochar Barrage was installed on the River Dee as well the Water of Ken was dammed to create manmade lochs as part of the Galloway Hydro Scheme. Several other lochs in Galloway are dammed such as Loch Doon , Loch Bradan and Clatteringshaws Loch though many smaller ones remain in
4536-458: The area. The nearest international passenger airports are Glasgow Prestwick International Airport , Glasgow International Airport and Edinburgh Airport . Vehicle ferries operate between Stranraer and Cairnryan in Scotland and Belfast and Larne in Northern Ireland respectively. There are numerous walks through the Southern Uplands. These include the Southern Upland Way , a 212-mile (341 km) coast to coast walk between Portpatrick in
4620-430: The boundaries of the town to enable warning to be given of raids from the south. This violent history is also commemorated in many Border ballads , another common theme of which is the supernatural, as in the ballads of Thomas the Rhymer and Tam Lin . Many Border ballads were collected by Sir Walter Scott in his Minstrelsy of the Scottish Border . Scott also portrayed the social history, folklore and traditions of
4704-435: The coasts of the Netherlands, Belgium, Germany, and Denmark and low-lying areas of eastern England particularly around The Wash and Fens . Storm surges are caused by changes in barometric pressure combined with strong wind created wave action . The first recorded storm tide flood was the Julianenflut , on 17 February 1164. In its wake, the Jadebusen , (a bay on the coast of Germany), began to form. A storm tide in 1228
4788-490: The councils of South Ayrshire , East Ayrshire , South Lanarkshire and East Lothian extend into the region. After local government reorganisation in 1974 and prior to further reorganisation in 1996, the Southern Uplands were administered by the two 'regions' of Dumfries & Galloway and Borders along with the southern margins of the regions of Strathclyde and Lothian. Within each of these regions were districts with their own district councils. Historically, i.e. prior to 1974,
4872-435: The decline. For example, a resident orca pod was lost in the 1960s, presumably due to the peak in PCB pollution in this time period. The OSPAR commission manages the OSPAR convention to counteract the harmful effects of human activity on wildlife in the North Sea, preserve endangered species , and provide environmental protection. All North Sea border states are signatories of the MARPOL 73/78 Accords, which preserve
4956-555: The energy of the incoming sea, so that the dike itself does not receive the full impact. Dikes that lie directly on the sea are especially reinforced. The dikes have, over the years, been repeatedly raised, sometimes up to 9 metres (30 ft) and have been made flatter to better reduce wave erosion. Where the dunes are sufficient to protect the land behind them from the sea, these dunes are planted with beach grass ( Ammophila arenaria ) to protect them from erosion by wind, water, and foot traffic. Storm surges threaten, in particular,
5040-508: The finest fishing location of the North Sea. The Long Forties and the Broad Fourteens are large areas with roughly uniform depth in fathoms (forty fathoms and fourteen fathoms or 73 and 26 m or 240 and 85 ft deep, respectively). These great banks and others make the North Sea particularly hazardous to navigate, which has been alleviated by the implementation of satellite navigation systems . The Devil's Hole lies 320 kilometres (200 mi) east of Dundee , Scotland. The feature
5124-623: The formation of the accretionary wedge, where sediment is scraped off the seafloor as a tectonic plate is subducted , has led to the formation of multiple, major, east–west faults that are now exploited by rivers and define valleys across the Southern Uplands. Levels of deformation associated with these faults is highly variable but is pervasive in the finer-grained sediments. Secondary mineralisation has further altered these Lower Palaeozoic rocks which are hosts for some distinctive springs , some of which have been exploited for tourism, such as those around Moffat . The Southern Uplands lie south of
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#17327940995035208-436: The glen. This can be shortened to head back at Holm Nick, passing by the Coulter reservoir. Another popular option is to begin from Glenkirk farm to the east, also allowing for a circular route. In a roughly clockwise direction, the hills in the range over 2000 ft are: The area is popular with gamekeepers as well as pastoral farming and it is advised to be observant when walking nearby from spring to late summer and heed
5292-420: The highest variability where there is fresh water inflow, such as at the Rhine and Elbe estuaries, the Baltic Sea exit and along the coast of Norway. The main pattern to the flow of water in the North Sea is an anti-clockwise rotation along the edges. The North Sea is an arm of the Atlantic Ocean receiving the majority of ocean current from the northwest opening, and a lesser portion of warm current from
5376-488: The local economy and to that of Scotland in general. Generally, sheep and arable farming are more predominant in the Scottish Borders to the east, while dairy farming is traditionally more important in Dumfries and Galloway , although recent years here have seen a move away from cattle grazing towards sheep farming. Several breeds of livestock have originated in the Southern Uplands, including Galloway cattle , Ayrshire dairy cattle and Cheviot sheep . Large areas of
5460-408: The lochs of the Galloway Forest Park, St Mary's Loch and along the River Tweed . Brown trout are common in many burns and a number of the rivers in the area have populations of sea trout , salmon and Eurasian otters . The two unitary authorities of Dumfries and Galloway in the west and the Scottish Borders in the east cover almost all of the Southern Uplands. Along its northern margins,
5544-431: The marine environment by preventing pollution from ships. Germany, Denmark, and the Netherlands also have a trilateral agreement for the protection of the Wadden Sea , or mudflats , which run along the coasts of the three countries on the southern edge of the North Sea. The North Sea has had various names throughout history. One of the earliest recorded names was Septentrionalis Oceanus , or "Northern Ocean", which
5628-415: The most important of which are Scotland's third and fourth longest, the River Clyde at 106 mi (171 km) and the River Tweed at 97 mi (156 km) respectively. Several significant rivers drain southwards into the Solway Firth and Irish Sea including (from west to east) the River Cree , River Dee , River Urr , River Nith , River Annan and the River Esk . There are numerous lochs in
5712-434: The prevailing flood levels. It was only around the beginning of the High Middle Ages , in 1200 AD, that inhabitants began to connect single ring dikes into a dike line along the entire coast, thereby turning amphibious regions between the land and the sea into permanent solid ground. The modern form of the dikes supplemented by overflow and lateral diversion channels, began to appear in the 17th and 18th centuries, built in
5796-411: The range do not follow a common direction. The highest summit, Culter Fell, at 748m, is the highest point in South Lanarkshire and indeed the whole of Lanarkshire . Walks in the area frequently follow a popular round which begins in the Culter Glen, follows an ascent from the north up Culter Fell, down and up to Glenwhappen Rig to Gathersnow Hill followed by a long, flat walk to Hudderstone and back into
5880-433: The region comprised the counties of Wigtown , Kirkcudbright , Dumfries , Roxburgh , Peebles , Selkirk and Berwick together with parts of Ayrshire , Lanarkshire, Midlothian and East Lothian . The geography of the region has caused it to be sparsely populated, a characteristic shared with the Highlands but in contrast to the Central Lowlands. Although the political and geographical borders do not precisely coincide,
5964-410: The sea creating deep fjords and archipelagos . South of Stavanger, the coast softens, the islands become fewer. The eastern Scottish coast is similar, though less severe than Norway. From north east of England , the cliffs become lower and are composed of less resistant moraine , which erodes more easily, so that the coasts have more rounded contours. In the Netherlands, Belgium and in East Anglia
6048-413: The shores of the sea clogging harbours and inlets and has become a nuisance. Due to the heavy human populations and high level of industrialization along its shores, the wildlife of the North Sea has suffered from pollution, overhunting, and overfishing. Flamingos and pelicans were once found along the southern shores of the North Sea, but became extinct over the second millennium. Walruses frequented
6132-471: The smaller opening at the English Channel. These tidal currents leave along the Norwegian coast. Surface and deep water currents may move in different directions. Low salinity surface coastal waters move offshore, and deeper, denser high salinity waters move inshore. The North Sea located on the continental shelf has different waves from those in deep ocean water. The wave speeds are diminished and
6216-501: The south of Scotland, from the heart of the Scottish Borders to Dumfries and Galloway. They are on Forestry Commission land and along with schemes in Wales are regarded as the benchmark by which further trails in the UK should be developed. They are known as the 7stanes because each venue features a 'stane' ( Scots for stone) somewhere along the forest trails. The Seven Stanes: The Southern Uplands and especially those areas adjacent to
6300-557: The south, the coast consists mainly of sandy beaches, estuaries of long rivers and wide mudflats . Due to the dense population, heavy industrialisation , and intense use of the sea and the area surrounding it, various environmental issues affect the sea's ecosystems. Adverse environmental issues – commonly including overfishing , industrial and agricultural runoff , dredging , and dumping, among others – have led to several efforts to prevent degradation and to safeguard long-term economic benefits. The North Sea
6384-501: The two southern local authority areas have a combined population of around 265,000 across 4,314 square miles (11,170 km ), fewer inhabitants than five of the areas within the Central Lowlands, for example North Lanarkshire is home to 340,000 across 184 square miles (480 km ). Agriculture and forestry are the main forms of land use in the Southern Uplands. Sustainable power has been in production for several decades:
6468-825: The uplands of the Fennoscandian Shield and the British Isles. This precursor of the current North Sea has grown and shrunk with the rise and fall of the eustatic sea level during geologic time. Sometimes it was connected with other shallow seas, such as the sea above the Paris Basin to the south-west, the Paratethys Sea to the south-east, or the Tethys Ocean to the south. During the Late Cretaceous, about 85 million years ago , all of modern mainland Europe except for Scandinavia
6552-568: The war on the side of Japan. During the First World War , Great Britain's Grand Fleet and Germany's Kaiserliche Marine faced each other in the North Sea, which became the main theatre of the war for surface action. Britain's larger fleet and North Sea Mine Barrage were able to establish an effective blockade for most of the war, which restricted the Central Powers ' access to many crucial resources. Major battles included
6636-500: The warnings of any landowners. The area has a predominantly Scots influence. 'Coulter' is also a toponymic surname , likely derived from the village Coulter to the north. The word may derive from Scottish Gaelic cùl tir (back land) or Scots cootyre (safe place to store cows). Southern Uplands The Southern Uplands ( Scottish Gaelic : Na Monaidhean a Deas ) are the southernmost and least populous of mainland Scotland 's three major geographic areas (the others being
6720-406: The wave amplitudes are increased. In the North Sea there are two amphidromic systems and a third incomplete amphidromic system. In the North Sea the average tide difference in wave amplitude is between zero and eight metres (26 ft). The Kelvin tide of the Atlantic Ocean is a semidiurnal wave that travels northward. Some of the energy from this wave travels through the English Channel into
6804-500: The west and Cockburnspath in the east. There is some good rock climbing in the Southern Uplands, particularly in the western portion, the Galloway Hills. The majority of the climbing is on good quality granite, often slabby and sometimes a bit broken in nature. In cold winters there is good ice climbing on the hills of Craignaw , Merrick and Cairnsmore of Fleet . The 7stanes are seven mountain biking centres spanning
6888-532: Was a scattering of islands. By the Early Oligocene , 34 to 28 million years ago , the emergence of Western and Central Europe had almost completely separated the North Sea from the Tethys Ocean, which gradually shrank to become the Mediterranean as Southern Europe and South West Asia became dry land. The North Sea was cut off from the English Channel by a narrow land bridge until that
6972-566: Was breached by at least two catastrophic floods between 450,000 and 180,000 years ago. Since the start of the Quaternary period about 2.6 million years ago , the eustatic sea level has fallen during each glacial period and then risen again. Every time the ice sheet reached its greatest extent, the North Sea became almost completely dry, the dry landmass being known as Doggerland , whose northern regions were themselves known to have been glaciated. The present-day coastline formed after
7056-632: Was cited by Pliny . He also noted that the Cimbri called it Morimarusa – "Dead Sea". The name "North Sea" probably came into English, however, via the Dutch Noordzee , who named it thus either in contrast with the Zuiderzee ("South Sea"), located south of Frisia , or because the sea is generally to the north of the Netherlands. Before the adoption of "North Sea", the names used in English were "German Sea" or "German Ocean", referred to as
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