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Cummertrees
Cummertrees is a coastal village and civil parish In England, a civil parish is a type of administrative parish used for local government. It is a territorial designation which is the lowest tier of local government below districts and counties, or their combined form, the unitary authority ... of Annandale, Dumfries and Galloway, Annandale in the historical county of Dumfriesshire in Dumfries and Galloway. It lies about inland, on the Pow Water to the northwest of Powfoot, from Dumfries and from Annan, Dumfries and Galloway, Annan. Etymology Cummertrees, recorded as ''Cumbertres'' in 1204 and 1207, is probably of Cumbric origin. The second element represents ''*tres'' 'strife, tumult, violence', cognate with Welsh language, Welsh ''tres'' and Scottish Gaelic, Gaelic ''treas''. The first element is ''*cümber, cömber'' 'confluence. Andrew Breeze proposes the meaning 'confluence of turbulent water'. Alan James suggests that ''*tres'' may have been a stream-name. Howeve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cummertrees Railway Station
Cummertrees railway station was a train station, railway station in Dumfries and Galloway south of Dumfries, serving the village of Cummertrees. The village lies some west of Annan, Dumfries and Galloway, Annan and south of Lockerbie. History The station opened in 1848. The station is now closed, although the line running through the station remains open. The station building has been converted into a private dwelling. Cummertrees was opened by the Glasgow, Dumfries and Carlisle Railway, which then became part of the Glasgow and South Western Railway; in 1923 it became part of the London Midland and Scottish Railway at the Railways Act 1921, Grouping, passing on to the Scottish Region of British Railways following the 1948 nationalisation of the railways. It was closed by British Railways in 1955. The station lay south of the old terminus at St Enoch railway station, Glasgow St Enoch. An unstaffed siding at the station was closed 1 April 1959. A Cummertrees Lime siding exi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marquess Of Queensberry
Marquess of Queensberry is a title in the Peerage of Scotland. The title has been held since its creation in 1682 by a member of the Douglas family. The Marquesses also held the title of Duke of Queensberry from 1684 to 1810, when it was inherited by the Duke of Buccleuch. History The feudal barony of Drumlanrig was held by Sir William Douglas, illegitimate son of The 2nd Earl of Douglas and Mar, some time before 1427, when he died. His descendant William Douglas, 9th of Drumlanrig, was created the 1st Earl of Queensberry in 1633. The subsidiary titles of Lord Queensberry are: Earl of Queensberry (created 1633), Viscount Drumlanrig (1628) and Lord Douglas of Hawick and Tibbers (1628), all in the peerage of Scotland. He is also a Scottish baronet, styled "of Kelhead", created 26 February 1668, so the 6th Marquess was the 5th Baronet. The courtesy title used by Lord Queensberry's eldest son and heir is ''Viscount Drumlanrig''. There is no special courtesy title for Lord Dr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kinmount House
Kinmount House is a 19th-century country house in the parish of Cummertrees in the historic county of Dumfriesshire in Dumfries and Galloway region, Scotland. It is located west of Annan. The house was designed by Sir Robert Smirke for the 6th Marquess of Queensberry and completed in 1820. It is protected as a category A listed building, and the grounds are included on the Inventory of Gardens and Designed Landscapes in Scotland. History The lands of Kinmount were granted to the Carlyle family in the 13th century and acquired by William Douglas, 1st Earl of Queensberry, in 1633. The 4th Duke of Queensberry carried out extensive planting on the estate in the late 18th century. On his death in 1810, Kinmount passed to the 6th Marquess of Queensberry, who commissioned a new house from the English architect Sir Robert Smirke. The Greek Revival house was built between 1813 and 1820, with Smirke's assistant William Burn acting as executant architect. The masonry was carved by Joh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Powfoot
Powfoot is a coastal village in Dumfries and Galloway, Scotland that lies on the northern shore of the Solway Firth. It is located approximately 4 miles south west of the town of Annan and approximately 1.5 miles south east of the neighbouring village of Cummertrees. The Pow water, a local river runs through the village. History The village was begun circa 1800 and originally included a small harbour. The village was expanded several times, as part of wider efforts to create a new seaside resort on the north side of the Solway. John Bell and Joseph Burnie, local builders who had made money in Merseyside, returned to the area in 1894 and developed the characteristic red- Ashlar brick houses that exist today in the centre of the village beside the Pow water. These include the 4 semi-detached villas at 1-8 Ellerslie (built in 1900 to a design by Frank C Carruthers of Lockerbie and Dumfries), the terraced houses at 1-14 Lakeview, and the terrace houses at 1-9 Bella Vista. The bric ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glasgow, Dumfries And Carlisle Railway
The Glasgow, Dumfries and Carlisle Railway was a railway company in Scotland, which constructed the line from near Cumnock to Gretna Junction, forming the route from Glasgow to Carlisle via Dumfries, in association with other lines. Its promoters hoped it would form the only railway between central Scotland and England, but it lost out to rival companies. It opened in stages between 1846 and 1850, and on completion of its line it merged with the Glasgow, Paisley, Kilmarnock and Ayr Railway. The combined company took the name Glasgow & South Western Railway (G&SWR). The G&SWR formed an alliance with the English Midland Railway and for many years express passenger trains ran between Glasgow and London over the routes. The line is open today, continuing to form part of the Glasgow - Kilmarnock - Dumfries - Carlisle line; but that has diminished in importance and is now a secondary route. Passenger services are operated by ScotRail. History A line into Ayrshire, and later to En ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dumfriesshire
Dumfriesshire or the County of Dumfries or Shire of Dumfries (''Siorrachd Dhùn Phris'' in Gaelic) is a historic county and registration county in southern Scotland. The Dumfries lieutenancy area covers a similar area to the historic county. In terms of historic counties it borders Kirkcudbrightshire to the west, Ayrshire to the north-west, Lanarkshire, Peeblesshire and Selkirkshire to the north, and Roxburghshire to the east. To the south is the coast of the Solway Firth, and the English county of Cumberland. Dumfriesshire has three traditional subdivisions, based on the three main valleys in the county: Annandale, Eskdale and Nithsdale. These had been independent provinces in medieval times but were gradually superseded as administrative areas by the area controlled by the sheriff of Dumfries, or Dumfriesshire. A Dumfriesshire County Council existed from 1890 until 1975. Since 1975, the area of the historic county has formed part of the Dumfries and Galloway council ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hoddom Castle
Hoddom Castle is a large tower house in Dumfries and Galloway, south Scotland. It is located by the River Annan, south-west of Ecclefechan and the same distance north-west of Brydekirk in the parish of Cummertrees. The castle is protected as a category A listed building. History The lands of Hoddom or Hoddam belonged to the Herries family, allies of the Bruce family who were Lords of Annandale from 1124. It passed to the Carruthers family, and then to the Maxwells. At the core of the castle is an L-plan tower house, built in the 16th century. It was probably built for Sir John Maxwell, who acquired Hoddom in the mid 16th-century when he married the heiress Agnes, Lady Herries. In the aftermath of the reign of Mary, Queen of Scots, the Regent Moray besieged Hoddom, which capitulated after ten hours, on 21 June 1568. It was briefly the base of Douglas of Drumlanrig, a Warden of the Scottish West March, but was recaptured in 1569 by supporters of Queen Mary. The following year ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Robert I Of Scotland
Robert I (11 July 1274 – 7 June 1329), popularly known as Robert the Bruce (Scottish Gaelic: ''Raibeart an Bruis''), was King of Scots from 1306 to his death in 1329. One of the most renowned warriors of his generation, Robert eventually led Scotland during the First War of Scottish Independence against England. He fought successfully during his reign to regain Scotland's place as an independent kingdom and is now revered in Scotland as a national hero. Robert was a fourth great-grandson of King David I, and his grandfather, Robert de Brus, 5th Lord of Annandale, was one of the claimants to the Scottish throne during the "Great Cause". As Earl of Carrick, Robert the Bruce supported his family's claim to the Scottish throne and took part in William Wallace's revolt against Edward I of England. Appointed in 1298 as a Guardian of Scotland alongside his chief rival for the throne, John Comyn of Badenoch, and William Lamberton, Bishop of St Andrews, Robert resigned in 1300 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Redgauntlet
''Redgauntlet'' (1824) is a historical novel by Sir Walter Scott, one of the Waverley novels, set primarily in Dumfriesshire, southwest Scotland, in 1765, and described by Magnus Magnusson (a point first made by Andrew Lang) as "in a sense, the most autobiographical of Scott's novels."Magnus Magnusson. ''Scotland: Story of a Nation''. Harper Collins, 2000. Page 637. It describes a plot to start a fictional ''third'' Jacobite Rebellion, and includes "Wandering Willie's Tale", a famous short story which frequently appears in anthologies. Composition Composition of ''Redgauntlet'' was swift and steady. It began very shortly after the completion of ''Saint Ronan's Well'' in early December 1823, and by early January 1824 proofs had reached the fourth letter. The first volume was in print before the end of March, the second was probably written in late March and April, and the third was certainly composed in May. Editions The first edition was published in Edinburgh by Archibald Const ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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