Stronachlachar
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Stronachlachar
Loch Katrine (; or ) is a freshwater loch in the Trossachs area of the Scottish Highlands, east of Loch Lomond, within the historic county and registration county of Perthshire and the contemporary district of Stirling. The loch is about long and wide at its widest point, and runs the length of Strath Gartney (Gaelic: ''Srath Ghartain''). It is within the drainage basins of the River Teith and River Forth. It is a popular scenic attraction for tourists and day-visitors from Glasgow and nearby towns; fly and boat fishing for trout are permitted on the loch from spring to autumn. It also serves as a reservoir for the water supply of the Glasgow conurbation, some south, being connected by two aqueducts constructed in 1859. It is the fictional setting of Sir Walter Scott's poem ''The Lady of the Lake'' and of the subsequent opera by Gioachino Rossini, ''La donna del lago''. Name etymology William Watson, a renowned scholar of Scottish place names, judged ''Katrine'' to be "t ...
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Trossachs
The Trossachs (; gd, Na Tròiseachan) generally refers to an area of wooded glens, braes, and lochs lying to the east of Ben Lomond in the Stirling council area of Scotland. The name is taken from that of a small woodland glen that lies at the centre of the area, but is now generally applied to the wider region. The wooded hills and lochs of the area may be considered to represent a microcosm of a typical highland landscape, and the woodlands are an important habitat for many species. Much of the Trossachs area is protected by various different protected areas of Scotland, conservation designations, including the Great Trossachs Forest National nature reserve (Scotland), National Nature Reserve. The Trossachs form part of the Loch Lomond and The Trossachs National Park, which was established in 2002. The area has long been visited by tourists due to the relative proximity of major population centres such as Glasgow and Stirling, and remains popular with walkers, cyclists and t ...
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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 ...
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Walter Scott
Sir Walter Scott, 1st Baronet (15 August 1771 – 21 September 1832), was a Scottish novelist, poet, playwright and historian. Many of his works remain classics of European and Scottish literature, notably the novels ''Ivanhoe'', ''Rob Roy (novel), Rob Roy'', ''Waverley (novel), Waverley'', ''Old Mortality'', ''The Heart of Mid-Lothian'' and ''The Bride of Lammermoor'', and the narrative poems ''The Lady of the Lake (poem), The Lady of the Lake'' and ''Marmion (poem), Marmion''. He had a major impact on European and American literature. As an advocate, judge and legal administrator by profession, he combined writing and editing with daily work as Clerk of Session and Sheriff court, Sheriff-Depute of Selkirkshire. He was prominent in Edinburgh's Tory (political faction), Tory establishment, active in the Royal Highland and Agricultural Society of Scotland, Highland Society, long a president of the Royal Society of Edinburgh (1820–1832), and a vice president of the Society o ...
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Micaceous
Micas ( ) are a group of silicate minerals whose outstanding physical characteristic is that individual mica crystals can easily be split into extremely thin elastic plates. This characteristic is described as perfect basal cleavage. Mica is common in igneous and metamorphic rock and is occasionally found as small flakes in sedimentary rock. It is particularly prominent in many granites, pegmatites, and schists, and "books" (large individual crystals) of mica several feet across have been found in some pegmatites. Micas are used in products such as drywalls, paints, fillers, especially in parts for automobiles, roofing and shingles, as well as in electronics. The mineral is used in cosmetics and food to add "shimmer" or "frost." Properties and structure The mica group is composed of 37 phyllosilicate minerals. All crystallize in the monoclinic system, with a tendency towards pseudohexagonal crystals, and are similar in structure but vary in chemical composition. Micas are ...
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Schist
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture (geology), texture reflects a high content of platy minerals, such as micas, talc, chlorite group, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium Metamorphism#Metamorphic grades, grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is us ...
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Bathymetric Chart
A bathymetric chart is a type of isarithmic map that depicts the submerged topography and physiographic features of ocean and sea bottoms. Their primary purpose is to provide detailed depth contours of ocean topography as well as provide the size, shape and distribution of underwater features. Topographic maps display elevation above ground and are complementary to bathymetric charts. Charts use a series of lines and points at equal intervals to showcase depth or elevation. A closed shape with increasingly smaller shapes inside of it can indicate an ocean trench or a seamount, or underwater mountain, depending on whether the depths increase or decrease going inward.Bathymetric surveys and charts are associated with the science of oceanography, particularly marine geology, and underwater engineering or other specialized purposes. Bathymetric data used to produce charts can also be converted to bathymetric profiles which are vertical sections through a feature. History Ancient Eg ...
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Loch Katrine By Alexander Nasmyth, 1810
''Loch'' () is the Scottish Gaelic, Scots and Irish word for a lake or sea inlet. It is cognate with the Manx lough, Cornish logh, and one of the Welsh words for lake, llwch. In English English and Hiberno-English, the anglicised spelling lough is commonly found in place names; in Lowland Scots and Scottish English, the spelling "loch" is always used. Many loughs are connected to stories of lake-bursts, signifying their mythical origin. Sea-inlet lochs are often called sea lochs or sea loughs. Some such bodies of water could also be called firths, fjords, estuaries, straits or bays. Background This name for a body of water is Insular CelticThe current form has currency in the following languages: Scottish Gaelic, Irish, Manx, and has been borrowed into Lowland Scots, Scottish English, Irish English and Standard English. in origin and is applied to most lakes in Scotland and to many sea inlets in the west and north of Scotland. The word comes from Proto-Indo ...
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Loch Lubnaig
Loch Lubnaig (Loch Lùbnaig in Gaelic) is a small freshwater loch near Callander in the Stirling council area, Scottish Highlands. It lies in the former county of Perthshire. It is part of the Loch Lomond and The Trossachs National Park. The loch nestles in the space between Ben Ledi and Ben Vorlich. Fed by the River Balvaig from the north and drained by the Garbh Uisge to the south, Loch Lubnaig offers fishing from the shore while canoes can be rented at the north end. Alternatively, two car parking areas on the east shore offer perfect, albeit sometimes busy, canoe launching points. The route of the former Callander and Oban Railway runs along the west shore of the loch. This route has now been converted to a part of the National Cycle Network's "Route 7" allowing cyclists and walkers to travel the between Callander and Strathyre. The name is derived from the Gaelic Lùbnaig, meaning ''crooked''. Like many lochs of the Highlands, the name is almost identical to its Gaelic ...
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Proto-Celtic Language
Proto-Celtic, or Common Celtic, is the ancestral proto-language of all known Celtic languages, and a descendant of Proto-Indo-European. It is not attested in writing but has been partly Linguistic reconstruction, reconstructed through the comparative method. Proto-Celtic is generally thought to have been spoken between 1300 and 800 BC, after which it began to split into different languages. Proto-Celtic is often associated with the Urnfield culture and particularly with the Hallstatt culture. Celtic languages share common features with Italic languages that are not found in other branches of Indo-European, suggesting the possibility of an earlier Italo-Celtic linguistic unity. Proto-Celtic is currently being reconstructed through the comparative method by relying on later Celtic languages. Though Continental Celtic presents much substantiation for Proto-Celtic phonology, and some for its morphology (linguistics), morphology, recorded material is too scanty to allow a secure rec ...
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Pictish
Pictish is the extinct language, extinct Brittonic language spoken by the Picts, the people of eastern and northern Scotland from Late Antiquity to the Early Middle Ages. Virtually no direct attestations of Pictish remain, short of a limited number of toponymy, geographical and anthroponymy, personal names found on monuments and the contemporary records in the area controlled by the Picts#Kings and kingdoms, kingdoms of the Picts, dating to the early medieval period. Such evidence, however, points strongly to the language being an Insular Celtic language related to the Common Brittonic, Brittonic language spoken prior to Anglo-Saxon settlement of Britain, Anglo-Saxon settlement in what is now southern Scotland, England, and Wales. The prevailing view in the second half of the 20th century was that Pictish was a non-Indo-European languages, Indo-European language isolate, predating a Gaelic colonisation of Scotland or that a non-Indo-European Pictish and Brittonic Pictish language ...
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Scottish Toponymy
Scottish toponymy derives from the languages of Scotland. The toponymy varies in each region, reflecting the linguistic history of each part of the country. Goidelic roots accounts for most place-names in eastern Scotland, with a few Anglic names in Fife and Angus and with a small number Pictish elements assimilated into the total toponymy. Nearly every place-name in the Northern Isles has Norse roots (see Norn language and Scandinavian toponymy), as do many in the Western Isles and along the coasts of the mainland. In the highlands, the names are primarily from Scottish Gaelic, with emphasis on natural features; elements such as Glen- (Gaelic: ', valley) and Inver- (Gaelic: ', confluence, mouth) are common. Some Gaelic elements may themselves also be ultimately of Pictish or Brythonic origin, such as ' (Aber-, meaning confluence; cf modern Welsh ') and ' (Strath-, a wide, shallow river valley; cf modern Welsh '). In lowland Scotland, names are of more diverse origin. Man ...
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