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Ruberslaw Parish Church, Bedrule - Geograph
Rubers Law is a prominent, conical hill in the Scottish Borders area of south-east Scotland. It stands on the south bank of the River Teviot, between the towns of Hawick and Jedburgh, and south of the village of Denholm. The hill is on the border between the historic parishes of Cavers and Hobkirk, and until 1975 it stood within the historic county of Roxburghshire. Much of the hill is agricultural land with coniferous plantations, and with rough grazing land around the top. A number of routes to the rocky summit of the hill are possible for walkers, from which there is a wide view in all directions. The summit rocks represent the remains of a volcanic vent, formed by a volcanic eruption during the Carboniferous Period, roughly 330 million years ago. On and around the summit are the remains of several historical structures: an Iron Age hill fort, a Roman signal station, and a "nuclear fort" of the Early Middle Ages. Alexander Peden may have preached to illegal conventicles o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hawick
Hawick ( ; sco, Haaick; gd, Hamhaig) is a town in the Scottish Borders council area and historic county of Roxburghshire in the east Southern Uplands of Scotland. It is south-west of Jedburgh and south-south-east of Selkirk. It is one of the farthest towns from the sea in Scotland, in the heart of Teviotdale, and is the biggest town in the former county of Roxburghshire. The town is at the confluence of the Slitrig Water with the River Teviot. The town was formally established in the 16th century, but was previously the site of historic settlement going back hundreds of years. By the late 17th century, the town began to grow significantly, especially during the Industrial Revolution and Victorian era as a centre for the production of textiles, with a focus on knitting and weaving, involving materials such as tweed and cashmere. By the late 20th century, textile production had declined but the town remains an important regional centre for shopping, tourism and services. H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian line ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dry Stone
Dry stone, sometimes called drystack or, in Scotland, drystane, is a building method by which structures are constructed from stones without any mortar to bind them together. Dry stone structures are stable because of their construction method, which is characterized by the presence of a load-bearing façade of carefully selected interlocking stones. Dry stone construction is best known in the context of stone walls, traditionally used for the boundaries of fields and churchyards, or as retaining walls for terracing, but dry stone sculptures, buildings, bridges, and other structures also exist. The term tends not to be used for the many historic styles which used precisely-shaped stone, but did not use mortar, for example the Greek temple and Inca architecture. The art of dry stone walling was inscribed in 2018 on the UNESCO representative list of the intangible cultural heritage of humanity, for dry stone walls in countries such as France, Greece, Italy, Slovenia, Cr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Selkirkshire
Selkirkshire or the County of Selkirk ( gd, Siorrachd Shalcraig) is a historic county and registration county of Scotland. It borders Peeblesshire to the west, Midlothian to the north, Roxburghshire to the east, and Dumfriesshire to the south. It derives its name from its county town, the royal burgh of Selkirk. The county was historically also known as Ettrick Forest. Unlike many historic counties, Selkirkshire does not have its own lieutenancy area, but forms part of the Roxburgh, Ettrick and Lauderdale lieutenancy area. History In the 1st Century AD Selkirk formed part of the lands of the native people who hunted it rather than settled there. Neither the Romans, Angles, or the Saxons cleared much of the forestry there and for centuries Selkirk was known for its forest coverage. Indeed, an alternative name for the county was Ettrick Forest. Under the Scottish kings the forest was regarded as Royal. Despite this it was not until the reign of James V that sheriffs were appoi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Liddesdale
Liddesdale, the valley of the Liddel Water, in the Roxburghshire, County of Roxburgh, southern Scotland, extends in a south-westerly direction from the vicinity of Peel Fell to the River Esk, Dumfries and Galloway, River Esk, a distance of . The Waverley Line, Waverley route of the North British Railway runs down the dale, and the Catrail, or Picts' Dyke, crosses its head. Liddesdale was also a historic district of Scotland, bordering Teviotdale to the east, Annandale, Dumfries and Galloway, Annandale to the west and Tweeddale to the north, with the England, English county of Cumberland across the border to the south. The area was in the Sheriffdom of Roxburgh and later became part of the Roxburghshire, County of Roxburgh, one of the counties of Scotland. The main reorganisation took place during the Local Government (Scotland) Act 1889, this Act established a uniform system of county councils and town councils in Scotland and restructured many of Scotland's counties. (See: Histor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lammermuir Hills
The Lammermuirs are a range of hills in southern Scotland, forming a natural boundary between East Lothian and the Borders. The name "Lammermuir" comes from the Old English ''lambra mōr'', meaning "moorland of the lambs". Geology The Lammermuir Hills are formed from a succession of Silurian and Ordovician age marine sediments known as greywackes together with siltstones, shales and mudstones. They are assigned to the Gala Group. Unconformably overlying these highly faulted and folded strata are outcrops of the early Devonian age Great Conglomerate Formation which forms a part of the Reston Group of Old Red Sandstone rocks. These coarse red-purple conglomerates underlie a band of country in the east between Longformacus and Oldhamstocks and also occur in an isolated outcrop east of Soutra Hill and beneath the Dun Law Wind Farm on the western margin of the hills. The same strata extend down Lauderdale on the western margin of the hills. Numerous dykes of different litholo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eildon Hill
Eildon Hill lies just south of Melrose, Scotland in the Scottish Borders, overlooking the town. The name is usually pluralised into "the Eildons" or "Eildon Hills", because of its triple peak. The high eminence overlooks Teviotdale to the South.R. Milne & H. Brown, ''The Corbetts and Other Scottish Hills,'' p. 29. Published by the Scottish Mountaineering Trust, 2002. The north hilltop (of three peaks) is surrounded by over of ramparts, enclosing an area of about 16 ha (40 acres) in which at least 300 level platforms have been cut into the rock to provide bases for turf or timber-walled houses, forming one of the largest hill forts known in Scotland. A Roman army signalling station was later constructed on the same site as this hill fort. The mid hilltop is the highest, whilst the south hilltop is the lowest. The hills are owned by the Duke of Buccleuch, Scotland's largest private landowner. As with all land in Scotland the public have a right of responsible access t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rule Water
Rule or ruling may refer to: Education * Royal University of Law and Economics (RULE), a university in Cambodia Human activity * The exercise of political or personal control by someone with authority or power * Business rule, a rule pertaining to the structure or behavior internal to a business * School rule, a rule that is part of school discipline * Sport rule, a rule that defines how a sport is played * Game rule, a rule that defines how a game is played * Moral, a rule or element of a moral code for guiding choices in human behavior * Norm (philosophy), a kind of sentence or a reason to act, feel or believe * Rule of thumb, a principle with broad application that is not intended to be strictly accurate or reliable for every situation * Unspoken rule, an assumed rule of human behavior that is not voiced or written down * Slide rule, a mechanical analog computer Science * Rule of inference or transformation rule, a term in logic for a function which takes premises ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old English
Old English (, ), or Anglo-Saxon, is the earliest recorded form of the English language, spoken in England and southern and eastern Scotland in the early Middle Ages. It was brought to Great Britain by Anglo-Saxon settlement of Britain, Anglo-Saxon settlers in the mid-5th century, and the first Old English literature, Old English literary works date from the mid-7th century. After the Norman conquest of 1066, English was replaced, for a time, by Anglo-Norman language, Anglo-Norman (a langues d'oïl, relative of French) as the language of the upper classes. This is regarded as marking the end of the Old English era, since during this period the English language was heavily influenced by Anglo-Norman, developing into a phase known now as Middle English in England and Early Scots in Scotland. Old English developed from a set of Anglo-Frisian languages, Anglo-Frisian or Ingvaeonic dialects originally spoken by Germanic peoples, Germanic tribes traditionally known as the Angles, Sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Borders
The Scottish Borders ( sco, the Mairches, 'the Marches'; gd, Crìochan na h-Alba) is one of 32 council areas of Scotland. It borders the City of Edinburgh, Dumfries and Galloway, East Lothian, Midlothian, South Lanarkshire, West Lothian and, to the south-west, south and east, the English counties of Cumbria and Northumberland. The administrative centre of the area is Newtown St Boswells. The term Scottish Borders, or normally just "the Borders", is also used to designate the areas of southern Scotland and northern England that bound the Anglo-Scottish border. Geography The Scottish Borders are in the eastern part of the Southern Uplands. The region is hilly and largely rural, with the River Tweed flowing west to east through it. The highest hill in the region is Broad Law in the Manor Hills. 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 flow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lothian
Lothian (; sco, Lowden, Loudan, -en, -o(u)n; gd, Lodainn ) is a region of the Scottish Lowlands, lying between the southern shore of the Firth of Forth and the Lammermuir Hills and the Moorfoot Hills. The principal settlement is the Scottish capital, Edinburgh, while other significant towns include Livingston, Linlithgow, Bathgate, Queensferry, Dalkeith, Bonnyrigg, Penicuik, Musselburgh, Prestonpans, North Berwick, Dunbar, Whitburn and Haddington. Historically, the term Lothian referred to a province encompassing most of what is now southeastern Scotland. In the 7th century it came under the control of the Anglian kingdom of Bernicia, the northern part of the later kingdom of Northumbria, but the Angles' grip on Lothian was quickly weakened following the Battle of Nechtansmere in which they were defeated by the Picts. Lothian was annexed to the Kingdom of Scotland around the 10th century. Subsequent Scottish history saw the region subdivided into three counties— ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Leyden
John Caspar Leyden, M.D., (8 September 1775 – 28 August 1811) was a Scottish indologist. Biography Leyden was born at Denholm on the River Teviot, not far from Hawick. His father, a shepherd, had contrived to send him to Edinburgh University to study for the ministry. Leyden was a diligent but somewhat haphazard student, apparently reading everything except theology, for which he seems to have had no taste. Though he completed his divinity course, and in 1798 was licensed to preach from the presbytery of St Andrews, it soon became clear that the pulpit was not his vocation. In 1794, Leyden formed an acquaintance with Dr Robert Anderson, editor of ''The British Poets'', and of ''The Literary Magazine''. It was Anderson who later introduced him to Dr Alexander Murray, and Murray, probably, who led him to the study of Eastern languages. They became warm friends and generous rivals, though Leyden excelled, perhaps, in the rapid acquisition of new tongues and acquaintance with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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