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Deil's Dyke
Deil's Dyke, Pict's Dyke or Celt's Dyke in south-west lowland Scotland is a linear earthwork that roughly follows the contours that divide upland pasture from lowland arable land, effectively acting like the head-dykes of medieval and later times although its true purpose has not been settled. The Deil's Dyke, sometimes written as 'dike', is formed from an earthen berm of rounded form that varies from 2.0-4.0m wide and a maximum of 0.7m high sometimes having a stone core. Where a fosse accompanies the bank it is usually an inconsequential 0.5m or so in width on average and around 0.4m deep, more often located on the uphill or outfield side. As a defensive structure the dyke has no obvious military value and its erratic route militates against it being a practical political boundary. Location The earthwork is not continuous however it is generally regarded as running from east of Afton Water () near New Cumnock to Burnmouth () in the parish of Durisdeer, having passed through ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Cumnock
New Cumnock is a town in East Ayrshire, Scotland. It expanded during the coal-mining era from the late 18th century, and mining remained its key industry until its pits were shut in the 1960s. The town is southeast of Cumnock, and east of Ayr. History Early history One of the first mentions of the village was when Patrick Dunbar of Comenagh signed the Ragman Roll of 1296. Blind Harry's poem ''The Wallace (poem), The Actes and Deidis of the Illustre and Vallyeant Campioun Schir William Wallace'' placed William Wallace in and around the village in his heroic tales of the patriot, calling it Cumno. In 1296, William Wallace and his men were forced to turn back from New Cumnock because the road at Corsencon had been destroyed. ''"At Corssencon the gait was spilt that tide"'' The main route from Nithsdale to Ayrshire passed by Corsencon hill in the east of the parish where since 1205 a toll and customs point had stood. Wallace's detour took him to Avondale (Strathhaven) where he ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deer Hay Wind
A deer hay wind, deer fold or elrick is an artificial, natural or modified natural feature used in the culling, capture or management of deer in relation to deer parks or natural woodland and open countryside. These structures have existed for many centuries and after falling out of use and their function having been forgotten the more substantial earth or stone examples have attracted names such as ''Roman Trenches'', ''Old Fortifications'', etc. The hinds were the main target of the hunt. History Deer hay winds, folds and elricks were sites where by means of traps wild deer were killed or caught. Evidence that during Saxon times deer hunting was taking place in this fashion survives in a tract written by a 10th-century monk called Ælfric who wrote "''I weave myself nets and set them in a suitable place and urge on my dogs so that they chase the wild animals until they come into the nets unawares and are thus ensnared and I kill them in the nets.''" In several Saxon documents 'De ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devil's Dyke, Cambridgeshire
Devil's Dyke or Devil's Ditch is a linear earthen barrier, thought to be of Anglo-Saxon origin, in eastern Cambridgeshire and Suffolk. It runs for in an almost straight line from Reach to Woodditton, with a ditch and bank system facing southwestwards, blocking the open chalkland between the marshy fens to the north and the formerly wooded hills to the south. It is a Scheduled Monument, a biological Site of Special Scientific Interest and a Special Area of Conservation. Description The name ''Devil's Ditch'' or ''Dyke'' is a post-medieval one. In medieval times it was simply called the ''dic'' ("the ditch"), or ''le Micheldyche'' or ''magnum fossatum'' ("great ditch"). Devil's Dyke is over long and is the largest of a series of ancient dykes in Cambridgeshire. In some places the bank measures high and across. The highest point along the Devil's Dyke is at Gallows Hill, where it measures from the bottom of the ditch to the top of the earth wall. Since the 19th cent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elrick
Elrick ( gd, An Eilreig) is a small village on the A944 road west of the city of Aberdeen, Scotland. The name derives from a Gaelic word meaning a place where deer Deer or true deer are hoofed ruminant mammals forming the family Cervidae. The two main groups of deer are the Cervinae, including the muntjac, the elk (wapiti), the red deer, and the fallow deer; and the Capreolinae, including the re ... were driven for hunting. Elrick is also a common surname in the local area. Stagecoach operate services 5 & 6A to & from the city via Queens Road. Also 218 Alford -Foresterhill - Aberdeen. It is to the south and west of Westhill. References External links * Villages in Aberdeenshire Westhill, Aberdeenshire {{Aberdeenshire-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scottish Gaelic
Scottish Gaelic ( gd, Gàidhlig ), also known as Scots Gaelic and Gaelic, is a Goidelic language (in the Celtic branch of the Indo-European language family) native to the Gaels of Scotland. As a Goidelic language, Scottish Gaelic, as well as both Irish and Manx, developed out of Old Irish. It became a distinct spoken language sometime in the 13th century in the Middle Irish period, although a common literary language was shared by the Gaels of both Ireland and Scotland until well into the 17th century. Most of modern Scotland was once Gaelic-speaking, as evidenced especially by Gaelic-language place names. In the 2011 census of Scotland, 57,375 people (1.1% of the Scottish population aged over 3 years old) reported being able to speak Gaelic, 1,275 fewer than in 2001. The highest percentages of Gaelic speakers were in the Outer Hebrides. Nevertheless, there is a language revival, and the number of speakers of the language under age 20 did not decrease between the 2001 and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Nith
The River Nith ( gd, Abhainn Nid; Common Brittonic: ''Nowios'') is a river in south-west Scotland. The Nith rises in the Carsphairn hills of East Ayrshire, more precisely between Prickeny Hill and Enoch Hill, east of Dalmellington. For the majority of its course it flows in a south-easterly direction through Dumfries and Galloway and then into the Solway Firth at Airds Point. The territory through which the river flows is called Nithsdale (historically known as "Stranit" from gd, Strath Nid, "valley of the Nith"). Length For estuaries the principle followed is that the river should be visible at all times. The measurement therefore follows the centre of the river at low tide and the mouth of the river is assumed to be at the coastal high tide mark. In Scotland this does not generally make a significant difference, except for rivers draining into shallow sloping sands of the Irish Sea and Solway Firth, notably the Nith. At low tide, the sea recedes to such an extent that th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Early Middle Ages
The Early Middle Ages (or early medieval period), sometimes controversially referred to as the Dark Ages, is typically regarded by historians as lasting from the late 5th or early 6th century to the 10th century. They marked the start of the Middle Ages of European history, following the decline of the Western Roman Empire, and preceding the High Middle Ages ( 11th to 13th centuries). The alternative term ''late antiquity'', for the early part of the period, emphasizes elements of continuity with the Roman Empire, while ''Early Middle Ages'' is used to emphasize developments characteristic of the earlier medieval period. The period saw a continuation of trends evident since late classical antiquity, including population decline, especially in urban centres, a decline of trade, a small rise in average temperatures in the North Atlantic region and increased migration. In the 19th century the Early Middle Ages were often labelled the ''Dark Ages'', a characterization based on t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roxburghshire
Roxburghshire or the County of Roxburgh ( gd, Siorrachd Rosbroig) is a historic county and registration county in the Southern Uplands of Scotland. It borders Dumfriesshire to the west, Selkirkshire and Midlothian to the north-west, and Berwickshire to the north. To the south-west it borders Cumberland and to the south-east Northumberland, both in England. It was named after the Royal Burgh of Roxburgh, a town which declined markedly in the 15th century and is no longer in existence. Latterly, the county town of Roxburghshire was Jedburgh. The county has much the same area as Teviotdale, the basin drained by the River Teviot and tributaries, together with the adjacent stretch of the Tweed into which it flows. The term is often treated as synonymous with Roxburghshire, but may omit Liddesdale as Liddel Water drains to the west coast.Ordnance Gazetteer of Scotland, by, Francis Groome, publ. 2nd edition 1896. Article on Roxburghshire History The county appears to have orig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Catrail
The Catrail is a linear earthwork in Roxburghshire, southern Scotland. It runs from Robert's Linn (), a burn (stream) flowing into the Slitrig Water, westward and north-westward to the head of the Dean Burn (), a tributary of the Borthwick Water. It is about {{convert, 11.5, mi, km, abbr=on long (as the crow flies), and consists of a ditch and bank. The Deil's Dyke was once considered to extend to the Catrail. Description The Catrail is discontinuous and although the various sections are not fully aligned they are considered parts of a single structure on the grounds that the profile is similar from section to section. Between sections, the line generally seems to follow the courses of streams and rivers. In profile, the earthwork consists of a ditch about 6–12 ft wide and 2–4.5 ft deep, and a parallel embankment about 8–13 ft wide and 2 ft high. There is generally a lesser bank running along the other side of the ditch which is quite wide but only a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glen Of The Bar - Geograph
A glen is a valley, typically one that is long and bounded by gently sloped concave sides, unlike a ravine, which is deep and bounded by steep slopes. Whittow defines it as a "Scottish term for a deep valley in the Highlands" that is "narrower than a strath".. The word is Goidelic in origin: ''gleann'' in Irish and Scottish Gaelic, ''glion'' in Manx. The designation "glen" also occurs often in place names. Etymology The word is Goidelic in origin: ''gleann'' in Irish and Scottish Gaelic, ''glion'' in Manx. In Manx, ''glan'' is also to be found meaning glen. It is cognate with Welsh ''glyn''. Examples in Northern England, such as Glenridding, Westmorland, or Glendue, near Haltwhistle, Northumberland, are thought to derive from the aforementioned Cumbric cognate, or another Brythonic equivalent. This likely underlies some examples in Southern Scotland. As the name of a river, it is thought to derive from the Irish word ''glan'' meaning clean, or the Welsh word ''gleindid'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eskdalemuir
Eskdalemuir is a civil parish and small village in Dumfries and Galloway, Scotland, with a population of 265.General Register Office for Scotland : ''Census 2001 : Usual Resident Population : Eskdalemuir Civil Parish'' Retrieved 2009-11-21 It is around north-west of Langholm and north-east of |
Gatelawbridge
Gatelawbridge is a hamlet in the region of Dumfries and Galloway, Scotland. It is situated two and a half miles east of Thornhill and near the gorge Crichope Linn. The origin of the name is unknown though in the past the locals called it Gateley Bridge, so perhaps it takes its name from a type of bridge over the Cample River in the centre of the settlement. The river divides the parishes, with all those east of the river being in Closeburn Parish, and those west of the river being in Morton Parish. The African explorer Joseph Thomson lived in Gatelawbridge from the age of 10 until leaving for Edinburgh. He attended the secondary school Morton Academy in Thornhill (now Wallace Hall), making the journey each day on his pony called Donald. His father was the quarry master and presumably that is where his interest in rocks began. He studied geology at the University of Edinburgh. After graduating he was engaged on several explorations in East and North Africa. He discovered the Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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