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Beinn A' Chroin
Beinn a' Chroin is a mountain in the Breadalbane, Scotland, Breadalbane region of the Scottish Highlands, six kilometres south of Crianlarich. With a height of it qualifies as a Munro. Overview Beinn a’ Chroin stands well into the interior of the Crianlarich group of seven munros and so it is usually climbed with other hills in the area, more often than not it is ascended with An Caisteal"The Munros" Pages 13 (Gives route with An Caisteal). which lies 1.5 kilometres to the north west across the Bealach Buidhe (805 metres). The hill is well seen from the upper part of Glen Falloch from where the long summit ridge and the steep head wall of Cirque, Coire Earb can be appreciated. The translation of the mountains name from the Scottish Gaelic language, Gaelic language is vague and there are three possible meanings. Some sources give the translation as "hill of danger""100 Best Routes on Scottish Mountains" Pages 30 Gives translation as "Hill of Danger". although Beinn a’ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grampian Mountains (Scotland)
The Grampian Mountains (''Am Monadh'' in Gaelic) is one of the three major mountain ranges in Scotland, that together occupy about half of Scotland. The other two ranges are the Northwest Highlands and the Southern Uplands. The Grampian range extends southwest to northeast between the Highland Boundary Fault and the Great Glen. The range includes many of the highest mountains in the British Isles, including Ben Nevis (whose peak contains the highest point in the British Isles at above sea level) and Ben Macdui (whose peak contains second-highest at ). A number of rivers and streams rise in the Grampians, including the Tay, Spey, Cowie Water, Burn of Muchalls, Burn of Pheppie, Burn of Elsick, Cairnie Burn, Don, Dee and Esk. The area is generally sparsely populated. There is some ambiguity about the extent of the range, and until the nineteenth century, they were generally considered to be more than one range, which all formed part of the wider Scottish Highlands. This view ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cloven Hoof
A cloven hoof, cleft hoof, divided hoof or split hoof is a hoof split into two toes. This is found on members of the mammalian order Artiodactyla. Examples of mammals that possess this type of hoof are cattle, deer, pigs, antelopes, gazelles, goats and sheep. In folklore and popular culture, a cloven hoof has long been associated with the Devil. The two digits of cloven-hooved animals are homologous to the third and fourth fingers of the hand. They are called claws and are named for their relative location on the foot: the outer, or lateral, claw and the inner, or medial claw. The space between the two claws is called the interdigital cleft; the area of skin is called the interdigital skin. The hard outer covering of the hoof is called the hoof wall or horn. It is a hard surface, similar to the human fingernail. The almost finger-like dexterity available to cloven-hooved mammals such as mountain goats and wild sheep combined with a hard outer shell and soft and flexible inner ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Munros
A Munro () is defined as a mountain in Scotland with a height over , and which is on the Scottish Mountaineering Club (SMC) official list of Munros; there is no explicit topographical prominence requirement. The best known Munro is Ben Nevis (Beinn Nibheis), the highest mountain in the British Isles at . Munros are named after Sir Hugh Munro, 4th Baronet (1856–1919), who produced the first list of such hills, known as ''Munro's Tables'', in 1891. Also included were what Munro considered lesser peaks, now known as Munro Tops, which are also over 3,000 feet but are lower than the nearby primary mountain. The publication of the original list is usually considered to be the epoch event of modern peak bagging. The list has been the subject of subsequent variation and as of 10 December 2020, the Scottish Mountaineering Club has listed 282 Munros and 226 Munro Tops. "Munro bagging" is the activity of climbing all the listed Munros. As of 31 December 2021, 7,098 people had reported ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Irvine Butterfield
Irvine Butterfield (1936–2009) was an environmentalist, hillwalker and author of several books about mountains and the outdoor environment who took a significant role in the running of organisations with such interests in Scotland. He was a good organiser and volunteered large amounts of his time to causes he believed in. Personal life Butterfield was born in Farnhill, North Yorkshire on 8 August 1936 and from his youth he was a keen walker. He worked at the local gasworks and then in the Post Office. In 1957 he moved to London to start his lifetime career with HM Customs and Excise, in 1960 transferring to its whisky departments in Perth, Dundee and then Inverness. reported in It was here that he developed his love for the Scottish hills. Butterfield was a burly man, not built with the physique for climbing, who never claimed to be more than a hillwalker. He admitted that to climb the Inaccessible Pinnacle "a climbing friend from Manchester hauled me up it". Butterfield d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
A82 Road
The A82 is a major road in Scotland that runs from Glasgow to Inverness via Fort William, Highland, Fort William. It is one of the principal north-south routes in Scotland and is mostly a trunk road managed by Transport Scotland, who view it as an important link from the Central Belt to the Scottish Highlands and beyond. The road passes close to numerous landmarks, including; Loch Lomond, Rannoch Moor, Glen Coe, the Ballachulish Bridge, Ben Nevis, the Commando Memorial, Loch Ness, and Urquhart Castle. The route is derived in several places from the Old military roads of Scotland, military roads constructed through the Highlands by George Wade, General George Wade and William Caulfeild (British Army officer), Major William Caulfeild in the 18th century, along with later roads constructed by Thomas Telford in the 19th. The modern route is based on that designed by Telford, but with a number of improvements primarily dating from the 1920s and 30s. These include a diversion across ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Firth Of Forth
The Firth of Forth () is the estuary, or firth, of several Scottish rivers including the River Forth. It meets the North Sea with Fife on the north coast and Lothian on the south. Name ''Firth'' is a cognate of ''fjord'', a Norse word meaning a narrow inlet. ''Forth'' stems from the name of the river; this is ''*Vo-rit-ia'' (slow running) in Proto-Celtic, yielding '' Foirthe'' in Old Gaelic and '' Gweryd'' in Welsh. It was known as ''Bodotria'' in Roman times. In the Norse sagas it was known as the ''Myrkvifiörd''. An early Welsh name is ''Merin Iodeo'', or the "Sea of Iudeu". Geography and economy Geologically, the Firth of Forth is a fjord, formed by the Forth Glacier in the last glacial period. The drainage basin for the Firth of Forth covers a wide geographic area including places as far from the shore as Ben Lomond, Cumbernauld, Harthill, Penicuik and the edges of Gleneagles Golf Course. Many towns line the shores, as well as the petrochemical complexes at Gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Firth Of Clyde
The Firth of Clyde is the mouth of the River Clyde. It is located on the west coast of Scotland and constitutes the deepest coastal waters in the British Isles (it is 164 metres deep at its deepest). The firth is sheltered from the Atlantic Ocean by the Kintyre peninsula, which encloses the outer firth in Argyll and Ayrshire. The Kilbrannan Sound is a large arm of the Firth of Clyde, separating the Kintyre Peninsula from the Isle of Arran. Within the Firth of Clyde is another major island – the Isle of Bute. Given its strategic location at the entrance to the middle and upper Clyde, Bute played a vital naval military role during World War II. Geography At its entrance, the firth is about wide. At one area in its upper reaches, it is joined by Loch Long and the Gare Loch. This area includes the large anchorage off of Greenock that is known as the Tail of the Bank. (The “Bank” is a reference to the sandbank and shoal that separates the firth from the estuary of the Ri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and greenhouse periods, during which there are no glaciers on the planet. Earth is currently in the Quaternary glaciation. Individual pulses of cold climate within an ice age are termed ''glacial periods'' (or, alternatively, ''glacials, glaciations, glacial stages, stadials, stades'', or colloquially, ''ice ages''), and intermittent warm periods within an ice age are called '' interglacials'' or ''interstadials''. In glaciology, ''ice age'' implies the presence of extensive ice sheets in both northern and southern hemispheres. By this definition, Earth is currently in an interglacial period—the Holocene. The amount of anthropogenic greenhouse gases emitted into Earth's oceans and atmosphere is predicted to prevent the next glacial period for th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moraine
A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Proven ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cruach Ardrain
Cruach Ardrain is a Munro mountain in the Breadalbane region of the Scottish Highlands, with a height of 1,046 metres (3,432 feet). It is five kilometres southeast of Crianlarich village and is one of the Crianlarich Hills. Name The Gaelic name ''Cruach Àrdrain'' may come from ''Cruach Àrd-dhobhrain'', meaning "stack of the high water or high stream". It overlooks Coire Ardrain, from which a stream flows into the River Fillan at Inverardran. Other suggested meanings include "stack of the high part","The Munros" Pages 14 Gives translation as “Stack of the High Part“. "high heap","The High Mountains of Britain and Ireland" Pages 318 Gives translation as “The High Heap“. "high mound""100 Best Routes on Scottish Mountains" Page 32 Gives translation as “The High Mound“. and "high slopes"."Hamish‘s Mountain Walk" Page 94 Gives translation as “High Slopes. Landscape Cruach Ardrain is clearly delineated to the west by the upper valley of the River Falloch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scottish Gaelic Language
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 20 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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