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Strathmore, Angus
Strathmore () is a broad valley or strath in east-central Scotland, lying between the Grampian Mountains (Scotland), Grampian mountains and the Sidlaws. It is approximately long and wide. Strathmore is underlain by Old Red Sandstone but this is largely obscured by glacial till, sands and gravels deposited during the ice age. Its northeast to southwest alignment is influenced by the underlying geological structure of the area which reflects the dominant Caledonian Orogeny, Caledonian trend of both the central lowlands and the Highlands of Scotland; its northern margin reflects the presence of the Highland Boundary Fault. Strathmore is fertile and has some of Scotland's best arable farmland, producing soft fruits and cereals. History The Romans established a series of castrum, marching camps in Strathmore as they moved northwards through the valley. Other antiquities include Pictish stones such as the Eassie Stone. The Earl of Strathmore takes his title from the valley, and hi ...
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Strathmore From The Air - Geograph
Strathmore may refer to: Organizations * Strathmore (Maryland), an arts foundation in North Bethesda, U.S. * Strathmore School, in Nairobi, Kenya * Strathmore University, in Nairobi, Kenya ** Strathmore Business School ** Strathmore Law School Places Australia * Strathmore, Queensland * Strathmore Station, near Croydon in Queensland, Australia * Strathmore Homestead, near Collinsville in Queensland, Australia * Strathmore, Victoria, a suburb of Melbourne, Australia * Strathmore railway station, Essendon, Melbourne, Australia Scotland * Strathmore (ward), Perth and Kinross * Strathmore, Sutherland, a valley in northern Scotland * Valley of Strathmore, in east central Scotland United States * Strathmore, California * Strathmore, New Jersey * Strathmore, New York * Strathmore, Syracuse, New York Other places * Strathmore, Alberta, Canada ** Strathmore (D.J. Murray) Airport ** Strathmore (Appleton Field) Aerodrome * Strathmore (Killiney), a mansion in Dún ...
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Castrum
''Castra'' () is a Latin language, Latin term used during the Roman Republic and Roman Empire for a military 'camp', and ''castrum'' () for a 'Fortification, fort'. Either could refer to a building or plot of land, used as a fortified military base.. Included is a discussion about the typologies of Roman fortifications. In English language, English usage, ''castrum'' commonly translates to "Roman fort", "Roman camp" and "Roman fortress". Scholastic convention tends to translate ''castrum'' as "fort", "camp", "marching camp" or "fortress". Romans used the term ''castrum'' for different sizes of camps – including large Roman legion, legionary fortresses, smaller forts for Cohort (military unit), cohorts or for auxiliary forces, military camp, temporary encampments, and "marching" forts. The diminutive form ''castellum'' was used for fortlets, typically occupied by a detachment of a cohort or a ''centuria''. Etymology ''Castrum'' appears in Oscan language, Oscan and Umbrian ...
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Landforms Of Angus, Scotland
A landform is a land feature on the solid surface of the Earth or other planetary body. They may be natural or may be anthropogenic (caused or influenced by human activity). Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great oceanic basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, structure stratification, rock exposure, and soil type. Gross physical features or landforms include intuitive elements such as berms, cliffs, hills, mounds, peninsulas, ridges, rivers, valleys, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodi ...
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Glens Of Scotland
A glen is a valley, typically one that is long and bounded by gently sloped concave sides, unlike a ravine, which is deep and bounded by steep slopes. The word is Goidelic in origin: ''gleann'' in Irish and Scottish Gaelic, ''glion'' in Manx. The designation "glen" also occurs often in place names. Glens are appreciated by tourists for their tranquility and scenery. Etymology The word is Goidelic in origin: ''gleann'' in Irish and Scottish Gaelic, ''glion'' in Manx. In Manx, ''glan'' is also to be found meaning glen. It is cognate with Welsh ''glyn''. Whittow defines it as a "Scottish term for a deep valley in the Highlands" that is "narrower than a strath". Examples in Northern England, such as Glenridding, Westmorland, or Glendue, near Haltwhistle, Northumberland, are thought to derive from the aforementioned Cumbric cognate, or another Brythonic equivalent. This likely underlies some examples in Southern Scotland. As the name of a river, it is thought to derive f ...
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Glamis Castle
Glamis Castle is situated beside the village of Glamis (, ) in Angus, Scotland. It is the home of the Earl of Strathmore and Kinghorne, and is open to the public. Glamis Castle has been the home of the Clan Lyon, Lyon family since the 14th century, though the present building dates largely from the 17th century. Glamis Castle was the childhood home of the late Queen Elizabeth, The Queen Mother. Her second daughter, Princess Margaret was born there on 21 August 1930. The castle is protected as a Category A listed, category A listed building, and the grounds are included on the Inventory of Gardens and Designed Landscapes in Scotland, the national listing of significant gardens. Setting Glamis is set in the broad and fertile lowland valley of Strathmore, Angus and Perth & Kinross, Strathmore, in Forfar, county town of Angus, which lies between the Sidlaw Hills to the south and the Grampian Mountains to the north, approximately inland from the North Sea. The estate surrounding th ...
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Earl Of Strathmore
Earl of Strathmore and Kinghorne is a title in the Peerage of Scotland and the Peerage of the United Kingdom. The earl is also Chief of Clan Lyon. History The established history of Clan Lyon states that the family is of French origin, with the original name ''de Leonne'', but James Balfour Paul, in his '' Scots Peerage'', states that the family is likely of Celtic origin. The family's earliest recorded possessions, the thanages of Glamis, Glamis, Tannadyce and Belhelvies, were in a Celtic stronghold, while government positions held by family chiefs would have required fluency in Gaelic. The first recorded family member, John Lyon, Lord of Glamis, was a courtier and diplomat, who was appointed Keeper of the Privy Seal in 1371 on the accession of Robert II. He acquired significant lands, and on 18 March 1372, Robert II granted him "the free barony of Glamuyss in the sheriffdom of Forfar." Glamis has remained the seat of the family ever since. His descendant Patrick Lyon, ...
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Eassie Stone
The Eassie Stone is a Class II Pictish stone of about the mid 8th century AD in the village of Eassie, Angus, Scotland. The stone was found in Eassie burn in the late 18th century and now resides in a purpose-built perspex building in the ruined Eassie church. Location The cross slab is housed in a purpose-built shelter with see-through walls within the roofless shell of the old Eassie parish church, on the north side A94 road some west of Glamis and east of Meigle. Description The stone is a cross-slab high and wide, tapering to at the top, and is thick. The slab is carved on both faces in relief Relief is a sculpture, sculptural method in which the sculpted pieces remain attached to a solid background of the same material. The term ''wikt:relief, relief'' is from the Latin verb , to raise (). To create a sculpture in relief is to give ... and, as it bears Pictish symbols, it falls into John Romilly Allen and Joseph Anderson's classification system as a Class ...
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Pictish Stone
A Pictish stone is a type of monumental stele, generally carved or incised with symbols or designs. A few have ogham inscriptions. Located in Scotland, mostly north of the River Clyde, Clyde-River Forth, Forth line and on the Eastern side of the country, these stones are the most visible remaining evidence of the Picts and are thought to date from the 6th to 9th century, a period during which the Picts became Christianized. The earlier stones have no parallels from the rest of the British Isles, but the later forms are variations within a wider Insular art, Insular tradition of monumental stones such as high crosses. About 350 objects classified as Pictish stones have survived, the earlier examples of which holding by far the greatest number of surviving examples of the mysterious symbols, which have long intrigued scholars.
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Highland Boundary Fault
The Highland Boundary Fault is a major fault zone that traverses Scotland from Arran and Helensburgh on the west coast to Stonehaven in the east. It separates two different geological terranes which give rise to two distinct physiographic terrains: the Highlands and the Lowlands, and in most places it is recognisable as a change in topography. Where rivers cross the fault, they often pass through gorges, and the associated waterfalls can be a barrier to salmon migration. The fault is believed to have formed in conjunction with the Strathmore syncline to the south-east during the Acadian orogeny in a transpressive regime that caused the uplift of the Grampian block and a small sinistral movement on the Highland Boundary Fault. Discovery One of the earliest and most prominent references to the Highland Boundary Fault was by George Barrow in 1912 ʻOn the Geology of Lower Dee-side and the Southern Highland Borderʼ, which highlights the nature of the rocks accompanying ...
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Strath
A strath is a large valley, typically a river valley that is wide and shallow (as opposed to a glen, which is typically narrower and deep). Word and etymology An anglicisation of the Gaelic word , it is one of many that have been absorbed into the English and Scots languages. It is commonly used in rural Scotland to describe a wide valley, even by non-Gaelic speakers. In Scottish place-names, ''Strath-'' is of Gaelic and Brittonic origin. ''Strath-'' names have a similar origin to Gaelic , meaning "broad-valley", as well as to Cumbric and Pictish cognates (''cf.'' Welsh ). Gaelic is derived from Old Irish , recorded as having meant "grassland". The modern Scottish Gaelic sense of "broad-valley", paralleling the meaning of Brittonic cognates, developed from substrate influence from Pictish. Toponymy It occurs in numerous place names within Scotland including Strathmore, Strathspey and Strathclyde. Abroad, many places with Scottish heritage also use the prefix, in ...
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Caledonian Orogeny
The Caledonian orogeny was a mountain-building cycle recorded in the northern parts of the British Isles, the Scandinavian Caledonides, Svalbard, eastern Greenland and parts of north-central Europe. The Caledonian orogeny encompasses events that occurred from the Ordovician to Early Devonian, roughly 490–390 million years ago ( Ma). It was caused by the closure of the Iapetus Ocean when the Laurentia and Baltica continents and the Avalonia microcontinent collided. The orogeny is named for Caledonia, the Latin name for Scotland. The term was first used in 1885 by Austrian geologist Eduard Suess for an episode of mountain building in northern Europe that predated the Devonian period. Geologists like Émile Haug and Hans Stille saw the Caledonian event as one of several episodic phases of mountain building that had occurred during Earth's history.McKerrow ''et al.'' (2002) Current understanding has it that the Caledonian orogeny encompasses a number of tectonic phases th ...
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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 ice age called Quaternary glaciation. Individual pulses of cold climate within an ice age are termed '' glacial periods'' (''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, the term ''ice age'' is defined by the presence of extensive ice sheets in the northern and southern hemispheres. By this definition, the current Holocene epoch is an interglacial period of an ice age. The accumulation of anthropogenic greenhouse gases is projected to delay the next glacial period. History of research ...
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