Cairn O' Mount
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Cairn O' Mount
Cairn O' Mounth/Cairn O' Mount ( gd, Càrn Mhon) is a high mountain pass in Aberdeenshire, Scotland. The place name is a survival of the ancient name for what are now the Grampian Mountains, earlier called "the Mounth" (in Gaelic: "monadh", meaning ''mountains''). The name change happened from circa 1520 AD. The Ordnance Survey shows the name as ''Cairn o' Mount''. It has served as an ancient military route at least from Roman times through the 13th century AD.Andrew Wyntoun, ''Original Chronicle'', ed. F.J. Amours, vol. 4, pp 298-299 and 300-301 (c. 1420) The alignment of the Cairnamounth, Elsick Mounth and Causey Mounth ancient trackways had a strong influence on the medieval siting of many fortifications and other settlements in the area comprised by present-day Aberdeenshire on both sides of the River Dee. Geography Cairn O' Mounth is at 1493 feet (454 m) above mean sea level, and there are various commanding views of the surrounding landscape which extend as far as the ...
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Cairn O Mount - Geograph
A cairn is a man-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the gd, càrn (plural ). Cairns have been and are used for a broad variety of purposes. In prehistoric times, they were raised as markers, as memorials and as burial monuments (some of which contained chambers). In modern times, cairns are often raised as landmarks, especially to mark the summits of mountains. Cairns are also used as trail markers. They vary in size from small stone markers to entire artificial hills, and in complexity from loose conical rock piles to elaborate megalithic structures. Cairns may be painted or otherwise decorated, whether for increased visibility or for religious reasons. A variant is the inuksuk (plural inuksuit), used by the Inuit and other peoples of the Arctic region of North America. History Europe The building of cairns for various purposes goes back into prehistory in Eurasia, ranging in s ...
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Mean Sea Level
There are several kinds of mean in mathematics Mathematics is an area of knowledge that includes the topics of numbers, formulas and related structures, shapes and the spaces in which they are contained, and quantities and their changes. These topics are represented in modern mathematics ..., especially in statistics. Each mean serves to summarize a given group of data, often to better understand the overall value (magnitude (mathematics), magnitude and sign (mathematics), sign) of a given data set. For a data set, the ''arithmetic mean'', also known as "arithmetic average", is a measure of central tendency of a finite set of numbers: specifically, the sum of the values divided by the number of values. The arithmetic mean of a set of numbers ''x''1, ''x''2, ..., x''n'' is typically denoted using an overhead bar, \bar. If the data set were based on a series of observations obtained by sampling (statistics), sampling from a statistical population, the arithmetic mean is th ...
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Invasion
An invasion is a military offensive in which large numbers of combatants of one geopolitical entity aggressively enter territory owned by another such entity, generally with the objective of either: conquering; liberating or re-establishing control or authority over a territory; forcing the partition of a country; altering the established government or gaining concessions from said government; or a combination thereof. An invasion can be the cause of a war, be a part of a larger strategy to end a war, or it can constitute an entire war in itself. Due to the large scale of the operations associated with invasions, they are usually strategic in planning and execution. History Archaeological evidence indicates that invasions have been frequent occurrences since prehistory. In antiquity, before radio communications and fast transportation, the only way for a military to ensure adequate reinforcements was to move armies as one massive force. This, by its very nature, led to the s ...
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England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ...
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Mac Bethad
Macbeth ( – 15 August 1057) was King of Scots from 1040 until his death. He ruled over the Kingdom of Alba, which covered only a portion of present-day Scotland. Little is known about Macbeth's early life, although he was the son of Findláech of Moray and may have been a grandson of Malcolm II. He became Mormaer of Moray – a semi-autonomous Provinces of Scotland, province – in 1032, and was probably responsible for the death of the previous mormaer, Gille Coemgáin of Moray, Gille Coemgáin. He subsequently married Gille Coemgáin's widow, Gruoch of Scotland, Gruoch, but they had no children together. In 1040, Duncan I of Scotland, Duncan I launched an attack into Moray and was killed in action by Macbeth's troops. Macbeth succeeded him as King of Alba, apparently with little opposition. His 17-year reign was mostly peaceful, although in 1054 he was faced with an English invasion, led by Siward, Earl of Northumbria, on behalf of Edward the Confessor. Macbeth was killed a ...
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Flood
A flood is an overflow of water ( or rarely other fluids) that submerges land that is usually dry. In the sense of "flowing water", the word may also be applied to the inflow of the tide. Floods are an area of study of the discipline hydrology and are of significant concern in agriculture, civil engineering and public health. Human changes to the environment often increase the intensity and frequency of flooding, for example land use changes such as deforestation and removal of wetlands, changes in waterway course or flood controls such as with levees, and larger environmental issues such as climate change and sea level rise. In particular climate change's increased rainfall and extreme weather events increases the severity of other causes for flooding, resulting in more intense floods and increased flood risk. Flooding may occur as an overflow of water from water bodies, such as a river, lake, or ocean, in which the water overtops or breaks levees, resulting ...
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Scottish Tourist Board
VisitScotland, formerly the Scottish Tourist Board, is a national tourism organisation for Scotland. It is an executive non-departmental public body of the Scottish Government, with offices in Edinburgh, Glasgow, Aberdeen, Inverness, and other parts of Scotland. Among the organisation's tasks is the attraction of visitors to Scotland through advertising and promotional campaigns. VisitScotland also manages a number of quality grading schemes for tourist accommodation and attractions. The organisation also operates the VisitScotland.com website which provides bookings and information service for visitors to Scotland. From 2001 this website was operated as a public-private partnership venture, though this venture (and the website) was brought back into public ownership in 2008. Aims and operation VisitScotland's primary aim is to market Scotland as a tourism destination, which it does through advertising and promotion as well as encouraging press articles on Scotland and what ...
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Clachnaben
Clachnaben (archaically "Cloch-na'bain"; Scottish Gaelic: "Clach na Beinne") is a 589-metre hill in Glen Dye, Aberdeenshire, Scotland. It is a distinctive hill visible from many points on Lower Deeside and is topped with a large granite tor. ''Clachnaben'' is the war cry of Clan Strachan. The hill gives its name to one of the houses at Aboyne Academy. Geography A popular walk starts at the car park on the Cairn O' Mounth (Banchory–Fettercairn) road, 10 kilometres south of Banchory. Popularity has caused some erosion on the old steep path which climbs this hill directly; however, efforts have been made to stabilise the erosion. A new improved path takes an easier and less direct route from Millar's Bog to the summit. There are views to Mount Battock, Lochnagar and Bennachie. The granite tor provides some rock climbing Rock climbing is a sport in which participants climb up, across, or down natural rock formations. The goal is to reach the summit of a formation or the ...
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Tor (rock Formation)
A tor, which is also known by geomorphologists as either a castle koppie or kopje, is a large, free-standing rock outcrop that rises abruptly from the surrounding smooth and gentle slopes of a rounded hill summit or ridge crest. In the South West of England, the term is commonly also used for the hills themselves – particularly the high points of Dartmoor in Devon and Bodmin Moor in Cornwall.Ehlen, J. (2004) ''Tor'' in Goudie, A., ed., pp. 1054-1056. ''Encyclopedia of Geomorphology.'' Routledge. London, England. Etymology Although English topographical names often have a Celtic etymology, the Oxford English Dictionary lists no cognates to the Old English word in either the Breton or Cornish languages (the Scottish Gaelic ''tòrr'' is thought to derive from the Old English word). It is therefore accepted that the English word ''Tor'' derives from the Old Welsh word ''tẁrr'' or ''twr'', meaning a cluster or heap. Formation Tors are landforms created by the erosion and weath ...
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Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ...
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Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap (landform), gap, saddle (landform), saddle, col or notch (landform), notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pas ...
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