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Jed Water
The Jed Water is a river and a tributary of the River Teviot in the Borders region of Scotland. In total the Jed Water is over long and it falls . It flows into the Teviot near Jedfoot Bridge () two miles north of Jedburgh. Jed Water rises from a source on Carlin Tooth in the Cheviot Hills where it is first known as Raven Burn. Description The river in past times was the main source of water for the monks living in Jedburgh Abbey. It also powered a watermill in the town of Jedburgh although this no longer exists. It gives its name to Jedburgh and Jedforest. In the 1800s it had trout in the river. The Ordnance gazetteer said Jed Water "in the parts immediately above the town of Jedburgh ... more of the elements of fine landscape than during a whole day's ride in the most favourite Scottish haunts of tourists." The guide drew attention to the pure waters, the brisk currents, the steep landscapes and the contrasts which it thought picturesque. The name Jed is of obscure origi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jedburgh
Jedburgh (; gd, Deadard; sco, Jeddart or ) is a town and former royal burgh in the Scottish Borders and the traditional county town of the historic county of Roxburghshire, the name of which was randomly chosen for Operation Jedburgh in support of the D-Day invasion. Location Jedburgh lies on the Jed Water, a tributary of the River Teviot. It is from the border with England, and is dominated by the substantial ruins of Jedburgh Abbey. Other notable buildings in the town include Queen Mary's House, Jedburgh Castle Jail, now a museum, and the Jedburgh Library. Other places nearby are Ancrum, Bairnkine, Bonjedward, Camptown, Crailing, Edgerston, Ferniehirst Castle, Nisbet and Oxnam. History Jedburgh began as ''Jedworð'', the "worth" or enclosed settlement on the Jed. Later the more familiar word "burgh" was substituted for this, though the original name survives as Jeddart/Jethart. Bishop Ecgred of Lindisfarne founded a church at Jedburgh in the 9th centur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Back-formation
In etymology, back-formation is the process or result of creating a new word via inflection, typically by removing or substituting actual or supposed affixes from a lexical item, in a way that expands the number of lexemes associated with the corresponding root word.Crystal, David. ''A Dictionary of Linguistics and Phonetics, Sixth Edition'', Blackwell Publishers, 2008. The resulting is called a ''back-formation'', a term coined by James Murray in 1889. ('' Oxford English Dictionary Online'' preserves its first use of 'back-formation' from 1889 in the definition of ''to burgle''; from ''burglar''.) For example, the noun ''resurrection'' was borrowed from Latin, and the verb ''resurrect'' was then back-formed hundreds of years later from it by removing the ''-ion'' suffix. This segmentation of ''resurrection'' into ''resurrect'' + ''ion'' was possible because English had examples of Latin words in the form of verb and verb+''-ion'' pairs, such as ''opine/opinion''. These bec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of The Scottish Borders
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Places In Scotland
This list of places in Scotland is a complete collection of lists of places in Scotland. * List of burghs in Scotland * List of census localities in Scotland *List of islands of Scotland ** List of Shetland islands ** List of Orkney islands ** List of Inner Hebrides **List of Outer Hebrides ** List of outlying islands of Scotland **List of freshwater islands in Scotland * List of rivers of Scotland * List of lochs in Scotland * Waterfalls of Scotland * List of Munros *Extreme points of Scotland Lists of places within Scottish local authorities * List of places in Aberdeen * List of places in Aberdeenshire * List of places in Angus *List of places in Argyll and Bute * List of places in Clackmannanshire * List of places in Dumfries and Galloway * List of places in Dundee * List of places in East Ayrshire * List of places in East Dunbartonshire *List of places in East Lothian * List of places in East Renfrewshire * List of places in na h-Eileanan Siar (Western Isles) * List of place ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Places In The Scottish Borders
''Map of places in the Scottish Borders compiled from this list'':See the list of places in Scotland for places in other counties. This list of places in the Scottish Borders includes towns, villages, hamlets, castles, golf courses, historic houses, hillforts, lighthouses, nature reserves, reservoirs, rivers, and other places of interest in the Scottish Borders council area of Scotland. A * Abbey Mill *Abbey St. Bathans * Abbotsford Ferry railway station, Abbotsford House * Abbotrule * Addinston *Aikwood Tower * Ale Water * Alemoor Loch *Allanbank *Allanshaugh *Allanshaws * Allanton * Ancrum, Ancrum Old Parish Church * Anglo-Scottish Border * Appletreehall * Ashiestiel * Ashkirk *Auchencrow *Ayton, Ayton Castle, Ayton Parish Church, Ayton railway station B * Baddinsgill, Baddinsgill Reservoir *Bairnkine * Bassendean *Battle of Ancrum Moor * Battle of Humbleton Hill * Battle of Nesbit Moor (1355) * Battle of Nesbit Moor (1402) * Battle of P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Borders Abbeys Way
The Borders Abbeys Way is a long-distance footpath in the Scottish Borders area of Scotland. It is a circular walkway and is in length. The theme of the footpath is the ruined Borders abbeys (established by David I of Scotland) along its way: Kelso Abbey, Jedburgh Abbey, Melrose Abbey and Dryburgh Abbey. These abbeys were homes to monks, who lived there between the 12th and 16th centuries. The route also passes through the towns of Hawick and Selkirk, and close to Abbotsford House, the home of Sir Walter Scott. Along the Borders Abbeys Way there are several rivers: Jed Water, River Teviot, River Tweed, Ale Water, and Rule Water. The route was opened in 2006, and is managed and maintained by Scottish Borders Council. It is now designated as one of Scotland's Great Trails by NatureScot. The route links with four of the other Great Trails: the Cross Borders Drove Road, the Romans and Reivers Route, St Cuthbert's Way and the·Southern Upland Way. About 15,000 people use the path ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canongate Bridge
The Canongate Bridge is a pedestrian bridge in the Scottish Borders town of Jedburgh. It was built as the town's main bridge over the Jed Water in the 16th century. Since 1971 it has been a category A listed building. Description The Canongate Bridge is a 16th-century stone arch bridge that crosses Jed Water in the centre of Jedburgh. The viaduct is built of cream-coloured sandstone and it spans the river with three arches, one of which normally runs over land. The passageway is up to three meters wide. The bridge said to be in desperate need of repair in 1677 and 1770 and repairs took place in 1772. The Canongate Bridge was built as a road bridge and it has refuges where pedestrians can stand safely whilst heavy traffic passed. The bridge was the main access into the town but it has been closed to motorised traffic for some years. The bridge is now within the town's conservation area and many of the surrounding buildings are listed. At one end is Duck Row and the Piper's House ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies ( marine snow). Sedimentation may also occur as dissolved minerals precipita ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hutton's Unconformity
Hutton's Unconformity is a name given to various notable geological sites in Scotland identified by the 18th-century Scottish geologist James Hutton as places where the junction between two types of rock formations can be seen. This geological phenomenon marks the location where rock formations created at different times and by different forces adjoin. For Hutton, such an unconformity provided evidence for his Plutonist theories of uniformitarianism and the age of Earth. An unconformity is any break in the normal progression of sedimentary deposits, which are laid the newer on top of the older. In his search, Hutton and colleagues examined rock outcrops and cliffs, both riverside and sea, and found several locations where two adjoining rock types had been laid bare, the most noted being at Siccar Point on the coast of Berwickshire. Theory of rock formations Hutton hit on a variety of ideas to explain the rock formations he saw, and, after a quarter century of work, he read hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
James Hutton
James Hutton (; 3 June O.S.172614 June 1726 New Style. – 26 March 1797) was a Scottish geologist, agriculturalist, chemical manufacturer, naturalist and physician. Often referred to as the father of modern geology, he played a key role in establishing geology as a modern science. Hutton advanced the idea that the physical world's remote history can be inferred from evidence in present-day rocks. Through his study of features in the landscape and coastlines of his native Scottish lowlands, such as Salisbury Crags or Siccar Point, he developed the theory that geological features could not be static but underwent continuing transformation over indefinitely long periods of time. From this he argued, in agreement with many other early geologists, that the Earth could not be young. He was one of the earliest proponents of what in the 1830s became known as uniformitarianism, the science which explains features of the Earth's crust as the outcome of continuing natural proc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cumbric
Cumbric was a variety of the Common Brittonic language spoken during the Early Middle Ages in the '' Hen Ogledd'' or "Old North" in what is now the counties of Westmorland, Cumberland and northern Lancashire in Northern England and the southern Scottish Lowlands. It was closely related to Old Welsh and the other Brittonic languages. Place name evidence suggests Cumbric may also have been spoken as far south as Pendle and the Yorkshire Dales. The prevailing view is that it became extinct in the 12th century, after the incorporation of the semi-independent Kingdom of Strathclyde into the Kingdom of Scotland. Problems with terminology Dauvit Broun sets out the problems with the various terms used to describe the Cumbric language and its speakers.Broun, Dauvit (2004): 'The Welsh identity of the kingdom of Strathclyde, ca 900-ca 1200', ''Innes Review'' 55, pp 111–80. The people seem to have called themselves the same way that the Welsh called themselves (most likely fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cheviot Hills
The Cheviot Hills (), or sometimes The Cheviots, are a range of uplands straddling the Anglo-Scottish border between Northumberland and the Scottish Borders. The English section is within the Northumberland National Park. The range includes The Cheviot (the highest hill), plus Hedgehope Hill to the east, Windy Gyle to the west, and Cushat Law and Bloodybush Edge to the south. The hills are sometimes considered a part of the Southern Uplands of Scotland as they adjoin the uplands to the north. Since the Pennine Way runs through the region, the hills are also considered a part of the northern Pennines although they are separated from the Cheviot Hills by the Tyne Gap, part of which lies within the southern extent of the Northumberland National Park. The Cheviot Hills are primarily associated with geological activity from approximately 480 to 360 million years ago, when the continents of Avalonia and Laurentia collided, resulting in extensive volcanic activity (the Caledonia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
