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Blane Water
Strathblane ( gd, Strath Bhlàthain, ) is a village and parish in the registration county of Stirlingshire, situated in the southwestern part of the Stirling council area, in central Scotland. It lies at the foothills of the Campsie Fells and the Kilpatrick Hills on the Blane Water, north of Glasgow, east-southeast of Dumbarton, and southwest of Stirling. Strathblane is a dormitory village for Greater Glasgow, and has a total resident population of 1,811. Historically, Strathblane was the name of a parish in Stirlingshire which comprised three villages: Edenkill, Netherton and Mugdock. Mugdock was the ancient seat of the Earls of Lennox, and to the east of Strathblane lies the town of Lennoxtown. Blanefield is a settlement contiguous with Strathblane's northwestern fringe. To the west is the volcanic plug Dumgoyne, Glengoyne Distillery and the Trossachs National Park. The West Highland Way—a long-distance trail—passes close to the village. The Gaelic name ' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stirling (council Area)
The Stirling council area ( sco, Stirlin; gd, Sruighlea) is one of the 32 council areas of Scotland, and has a population of about ( estimate). It was created under the Local Government etc (Scotland) Act 1994 with the boundaries of the Stirling district of the former Central local government region, and it covers most of Stirlingshire (except Falkirk) and the south-western portion of Perthshire. Both counties were abolished for local government purposes under the Local Government (Scotland) Act 1973. The administrative centre of the area is the city of Stirling, with the headquarters at Old Viewforth. The area borders the council areas of Clackmannanshire (to the east), North Lanarkshire (to the south), Falkirk (to the south east), Perth and Kinross (to the north and north east), Argyll and Bute (to the north and north west), and both East and West Dunbartonshire to Stirling's southwest. The majority of the population of the area is located in its southeast corner, in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lennoxtown
Lennoxtown ( gd, Baile na Leamhnachd, ) is a town in East Dunbartonshire council area and the historic county of Stirlingshire, Scotland at the foot of the Campsie Fells, which are just to the north. The town had a population of 4,094 at the 2011 UK Census. History The focus of Lennoxtown area used to be the busy Lennox Mill, where tenants of the Woodhead estate brought their corn to be ground. There were several corn mills. Lennox Mill was located in the vicinity of the recently demolished Kali Nail Works. A significant event in the history of the locality was the establishment of the calico printing works at Lennoxmill during the late 1780s. It was on a site adjacent to the old corn mill. Calico is a type of cotton cloth, the printing of cotton cloth was soon established as the major industry in the area, also at Milton of Campsie. Calico was constructed during the late eighteenth and early nineteenth centuries to provide accommodation for the block makers and other cotton ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Britons (historic)
The Britons ( *''Pritanī'', la, Britanni), also known as Celtic Britons or Ancient Britons, were people of Celtic language and culture who inhabited Great Britain from at least the British Iron Age and into the Middle Ages, at which point they diverged into the Welsh, Cornish and Bretons (among others). They spoke the Common Brittonic language, the ancestor of the modern Brittonic languages. The earliest written evidence for the Britons is from Greco-Roman writers and dates to the Iron Age.Koch, pp. 291–292. Celtic Britain was made up of many tribes and kingdoms, associated with various hillforts. The Britons followed an Ancient Celtic religion overseen by druids. Some of the southern tribes had strong links with mainland Europe, especially Gaul and Belgica, and minted their own coins. The Roman Empire conquered most of Britain in the 1st century, creating the province of Britannia. The Romans invaded northern Britain, but the Britons and Caledonians in the n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
William Forbes Skene
William Forbes Skene Writer to the Signet, WS FRSE Society of Antiquaries of Scotland, FSA(Scot) Doctor of Civil Law, DCL Legum Doctor, LLD (7 June 1809 – 29 August 1892), was a Scotland, Scottish lawyer, historian and antiquary. He co-founded the Scottish legal firm Skene Edwards which was prominent throughout the 20th century but disappeared in 2008 when it merged with Morton Fraser. Life He was born in Inverey, the second son of Sir Walter Scott's friend, James Skene (1775–1864), of Rubislaw, near Aberdeen, and his wife, Jane Forbes, daughter of Sir William Forbes, 6th Baronet of Pitsligo. The family moved to Edinburgh in 1817, originally living with his uncle, Andrew Skene then from 1820 living at 126 Princes Street facing Edinburgh Castle.Edinburgh Post Office Directory 1820 He was educated at the Royal High School, Edinburgh, High School in Edinburgh. He was then apprenticed as a lawyer first to Francis Wilson WS at Parliament Square then to Henry Jardine WS also ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loch Lomond
Loch Lomond (; gd, Loch Laomainn - 'Lake of the Elms'Richens, R. J. (1984) ''Elm'', Cambridge University Press.) is a freshwater Scottish loch which crosses the Highland Boundary Fault, often considered the boundary between the lowlands of Central Scotland and the Highlands.Tom Weir. ''The Scottish Lochs''. pp. 33-43. Published by Constable and Company, 1980. Traditionally forming part of the boundary between the counties of Stirlingshire and Dunbartonshire, Loch Lomond is split between the council areas of Stirling, Argyll and Bute and West Dunbartonshire. Its southern shores are about northwest of the centre of Glasgow, Scotland's largest city. The Loch forms part of the Loch Lomond and The Trossachs National Park which was established in 2002. Loch Lomond is long and between wide, with a surface area of . It is the largest lake in Great Britain by surface area; in the United Kingdom, it is surpassed only by Lough Neagh and Lough Erne in Northern Ireland. In the Briti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Endrick Water
The Endrick Water or River Endrick ( gd, Eunarag) is a river which flows into the eastern end of Loch Lomond, Scotland. Its drainage basin covers a large part of the west of Stirling District. The Burnfoot Burn rising on the southern slopes of the Gargunnock Hills and the Backside Burn rising on the eastern slopes of the Fintry Hills combine to form the Endrick Water which flows south before turning sharply westwards at the foot of the western dam of Carron Valley Reservoir. The river flows through Strathendrick, the village of Fintry and past Balfron and Drymen Drymen (; from gd, Druiminn ) is a village in the Stirling district of central Scotland. Once a popular stopping place for cattle drovers, it is now popular with visiting tourists given its location near Loch Lomond. The village is centred aroun ... before entering Loch Lomond. External links Sites of Special Scientific Interest in Scotland Rivers of Stirling (council area) Rivers of West Dunbartonshire ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alabaster
Alabaster is a mineral or rock that is soft, often used for carving, and is processed for plaster powder. Archaeologists and the stone processing industry use the word differently from geologists. The former use it in a wider sense that includes varieties of two different minerals: the fine-grained massive type of gypsum and the fine-grained banded type of calcite.''More about alabaster and travertine'', brief guide explaining the different use of these words by geologists, archaeologists, and those in the stone trade. Oxford University Museum of Natural History, 2012/ref> Geologists define alabaster only as the gypsum type. Chemically, gypsum is a Water of crystallization, hydrous sulfur, sulfate of calcium, while calcite is a carbonate of calcium. The two types of alabaster have similar properties. They are usually lightly colored, translucent, and soft stones. They have been used throughout history primarily for carving decorative artifacts."Grove": R. W. Sanderson and Francis ... [...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] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratum
In geology and related fields, a stratum ( : strata) is a layer of rock or sediment characterized by certain lithologic properties or attributes that distinguish it from adjacent layers from which it is separated by visible surfaces known as either '' bedding surfaces'' or ''bedding planes''.Salvador, A. ed., 1994. ''International stratigraphic guide: a guide to stratigraphic classification, terminology, and procedure. 2nd ed.'' Boulder, Colorado, The Geological Society of America, Inc., 215 pp. . Prior to the publication of the International Stratigraphic Guide, older publications have defined a stratum as either being either equivalent to a single bed or composed of a number of beds; as a layer greater than 1 cm in thickness and constituting a part of a bed; or a general term that includes both ''bed'' and ''lamina''.Neuendorf, K.K.E., Mehl, Jr., J.P., and Jackson, J.A. , eds., 2005. ''Glossary of Geology'' 5th ed. Alexandria, Virginia, American Geological Institute. 779 pp. . ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Long-distance Trail
A long-distance trail (or long-distance footpath, track, way, greenway) is a longer recreational trail mainly through rural areas used for hiking, backpacking, cycling, horse riding or cross-country skiing. They exist on all continents except Antarctica. Many trails are marked on maps. Typically, a long-distance route will be at least long, but many run for several hundred miles, or longer. Many routes are waymarked and may cross public or private land and/or follow existing rights of way. Generally, the surface is not specially prepared, and the ground can be rough and uneven in areas, except in places such as converted rail tracks or popular walking routes where stone-pitching and slabs have been laid to prevent erosion. In some places, official trails will have the surface specially prepared to make the going easier. Historically Historically, and still nowadays in countries where most people move on foot or with pack animals, long-distance trails linked far away t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Highland Way
The West Highland Way ( gd, Slighe na Gàidhealtachd an Iar) is a linear long-distance route in Scotland. It is long, running from Milngavie north of Glasgow to Fort William in the Scottish Highlands, with an element of hill walking in the route. The trail, which opened in 1980, was Scotland's first officially designated Long Distance Route, and is now designated by NatureScot as one of Scotland's Great Trails. It is primarily intended as a long distance walking route, and whilst many sections are suitable for mountain biking and horseriding there are obstacles and surfaces that will require these users to dismount in places. It is managed by the West Highland Way Management Group (WHWMG) consisting of the local authorities for East Dunbartonshire, Stirling, Argyll and Bute and Highland, alongside the Loch Lomond and The Trossachs National Park Authority and NatureScot. About 120,000 people use the path every year, of whom about 36,000 walk the entire route. The path is esti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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