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Dumyat
Dumyat or Dunmyat (Scottish Gaelic: Dùn Mhèad) is a hill at the western extremity of the Ochil Hills in central Scotland. The name is thought to originate from ''Dun'' (hill fort) ''of the Maeatae''. Although relatively small (its height is 418 metres), the characteristic shape of the hill forms an important part of the distinctive scenery of the Stirling area, and it is often depicted (particularly in postcards and calendars) in combination with the nearby Abbey Craig. The hill is a popular climb with tourists and visitors to the Stirling and Trossachs area, due to the historical nature of Stirling and the proximity of the Wallace Monument. Dumyat has two principal summits: Castle Law on the west, and Dumyat proper on the east. On the summit of Castle Law the remains of an ancient hill fort, originally occupied by the Maeatae, are still clearly discernible. The fort is a scheduled monument. At one time the favourite route to the summit of either Dumyat or Castle ...
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Dumyat - Memorial And Beacon Brazier
Dumyat or Dunmyat (Scottish Gaelic: Dùn Mhèad) is a hill at the western extremity of the Ochil Hills in central Scotland. The name is thought to originate from ''Dun'' (hill fort) ''of the Maeatae''. Although relatively small (its height is 418 metres), the characteristic shape of the hill forms an important part of the distinctive scenery of the Stirling area, and it is often depicted (particularly in postcards and calendars) in combination with the nearby Abbey Craig. The hill is a popular climb with tourists and visitors to the Stirling and Trossachs area, due to the historical nature of Stirling and the proximity of the Wallace Monument. Dumyat has two principal summits: Castle Law on the west, and Dumyat proper on the east. On the summit of Castle Law the remains of an ancient hill fort, originally occupied by the Maeatae, are still clearly discernible. The fort is a scheduled monument. At one time the favourite route to the summit of either Dumyat or Castle ...
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Menstrie Glen
Menstrie Glen is the glen which separates Dumyat from Myreton Hill and the main body of the Ochil Hills in Scotland. Once farmed but no longer inhabited, it is now used for sheep pasture, a public water supply and recreation in the form of fishing and walking. A plan is under consideration (autumn 2014) for commercial forestry on the eastern and northern flanks of the glen. Vegetation and topography Much of the area of the glen is rough pasture where sheep graze. Bracken is also abundant while broad-leaved trees grow in the deeply cut burnsides and in the vicinity of abandoned settlements. The bed of the glen ranges in altitude from 228m, at the saddle at UK Grid reference NN819002, to about 20m where it emerges onto the flood plain in Menstrie at NS849970. Near its upper (west) end, the glen contains the Lossburn Reservoir which holds drinking water and is used for recreational fishing. The reservoir accepts water from the north-western slopes of Dumyat and from the south-w ...
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Maeatae
The Maeatae were a confederation of tribes that probably lived beyond the Antonine Wall in Roman Britain. The historical sources are vague as to the exact region they inhabited, but an association is thought to be indicated in the names of two hills with fortifications. Near the summit of Dumyat hill in the Ochils, overlooking Stirling, there are remains of a fort and the name of the hill (in Gaelic ''Dùn Mhèad'') is believed to derive from name meaning the hill of the Maeatae. The prominent hill fort may have marked their northern boundary, but Myot Hill, near Fankerton, plausibly marks their southern limits. A discussion of two views of the importance of Dumyat and Myot Hill is given in Wainwright. Cassius Dio describes them in detail in his ''Roman History'' (Book LXXVII), and is later quoted by Joseph Ritson and others. John Rhys seems convinced that they occupied the land between the Firth of Forth and the Firth of Tay or parts of what is now Clackmannanshire, Fife and ...
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Ochil Hills
The Ochil Hills (; gd, Monadh Ochail is a range of hills in Scotland north of the Forth valley bordered by the towns of Stirling, Alloa, Kinross, Auchterarder and Perth. The only major roads crossing the hills pass through Glen Devon/ Glen Eagles and Glenfarg, the latter now largely replaced except for local traffic by the M90 Edinburgh-Perth motorway cutting through the eastern foothills. The hills are part of a Devonian lava extrusion whose appearance today is largely due to the Ochil Fault which results in the southern face of the hills forming an escarpment. The plateau is undulating with no prominent peak, the highest point being Ben Cleuch at . The south-flowing burns have cut deep ravines including Dollar Glen, Silver Glen and Alva Glen, often only passable with the aid of wooden walkways. The extent of the Ochils is not well-defined but by some definitions continues to include the hills of north Fife. Historically, the hills, combined with the town's site at th ...
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Stirling
Stirling (; sco, Stirlin; gd, Sruighlea ) is a city in central Scotland, northeast of Glasgow and north-west of Edinburgh. The market town, surrounded by rich farmland, grew up connecting the royal citadel, the medieval old town with its merchants and tradesmen, the Old Bridge and the port. Located on the River Forth, Stirling is the administrative centre for the Stirling council area, and is traditionally the county town of Stirlingshire. Proverbially it is the strategically important "Gateway to the Highlands". It has been said that "Stirling, like a huge brooch clasps Highlands and Lowlands together". Similarly "he who holds Stirling, holds Scotland" is often quoted. Stirling's key position as the lowest bridging point of the River Forth before it broadens towards the Firth of Forth made it a focal point for travel north or south. When Stirling was temporarily under Anglo-Saxon sway, according to a 9th-century legend, it was attacked by Danish invaders. The sound of a ...
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Ochil Fault
The Ochil Fault is the geological feature which defines the southern edge of the Ochil Hills escarpment in Scotland. North of the fault, Devonian lava flows and pyroclastic deposits slope gently down, thinning towards the north. These are in part overlain by Old Red Sandstone rocks formed later in the Devonian period. Because the deposits thin towards the north, and there are few signs of volcanic necks within the Ochil Hills themselves, it is thought that the eruptive centres were south of the fault, however these are buried deep beneath the Carboniferous rocks including coal measures which are found beneath the low-lying carse lands to the south. To put this in perspective, the prominent hill Dumyat which defines the western extremity of the Ochil Hills has a height of . The nearest colliery, Manor Powis, approximately south of the fault, was approximately the same depth, in carse land that is scarcely above sea level, and was mining coal from Carboniferous strata at least ...
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Marilyn (hill)
This is a list of Marilyn hills and mountains in the United Kingdom, Isle of Man and Republic of Ireland, Ireland by height. Lists of mountains and hills in the British Isles#Marilyns, Marilyns are defined as peaks with a topographic prominence, prominence of or more, regardless of height or any other merit (e.g. topographic isolation, as used in Lists of mountains and hills in the British Isles#Munros, Munros). Thus, Marilyns can be mountains, with a height above , or relatively small hills. there were 2,011 recorded Marilyns. Definition The Marilyn classification was created by Alan Dawson in his 1992 book ''The Relative Hills of Britain''. The name Marilyn was coined by Dawson as a punning contrast to the ''Munro'' classification of Scottish mountains above , but which has no explicit prominence threshold, being homophonous with (Marilyn) ''Marilyn Monroe, Monroe''. The list of Marilyns was extended to Ireland by Clem Clements. Marilyn was the first of several subsequen ...
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Barytes
Baryte, barite or barytes ( or ) is a mineral consisting of barium sulfate ( Ba S O4). Baryte is generally white or colorless, and is the main source of the element barium. The ''baryte group'' consists of baryte, celestine (strontium sulfate), anglesite (lead sulfate), and anhydrite (calcium sulfate). Baryte and celestine form a solid solution (Ba,Sr)SO4. Names and history The radiating form, sometimes referred to as ''Bologna Stone'', attained some notoriety among alchemists for specimens found in the 17th century near Bologna by Vincenzo Casciarolo. These became phosphorescent upon being calcined. Carl Scheele determined that baryte contained a new element in 1774, but could not isolate barium, only barium oxide. Johan Gottlieb Gahn also isolated barium oxide two years later in similar studies. Barium was first isolated by electrolysis of molten barium salts in 1808 by Sir Humphry Davy in England. The American Petroleum Institute specification API 13/ISO 13500, which governs ...
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Copper
Copper is a chemical element with the symbol Cu (from la, cuprum) and atomic number 29. It is a soft, malleable, and ductile metal with very high thermal and electrical conductivity. A freshly exposed surface of pure copper has a pinkish-orange color. Copper is used as a conductor of heat and electricity, as a building material, and as a constituent of various metal alloys, such as sterling silver used in jewelry, cupronickel used to make marine hardware and coins, and constantan used in strain gauges and thermocouples for temperature measurement. Copper is one of the few metals that can occur in nature in a directly usable metallic form ( native metals). This led to very early human use in several regions, from circa 8000 BC. Thousands of years later, it was the first metal to be smelted from sulfide ores, circa 5000 BC; the first metal to be cast into a shape in a mold, c. 4000 BC; and the first metal to be purposely alloyed with another metal, tin, to create ...
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Sheep Fold
Sheep or domestic sheep (''Ovis aries'') are domesticated, ruminant mammals typically kept as livestock. Although the term ''sheep'' can apply to other species in the genus ''Ovis'', in everyday usage it almost always refers to domesticated sheep. Like all ruminants, sheep are members of the order Artiodactyla, the even-toed ungulates. Numbering a little over one billion, domestic sheep are also the most numerous species of sheep. An adult female is referred to as a ''ewe'' (), an intact male as a ''ram'', occasionally a ''tup'', a castrated male as a ''wether'', and a young sheep as a ''lamb''. Sheep are most likely descended from the wild mouflon of Europe and Asia, with Iran being a geographic envelope of the domestication center. One of the earliest animals to be domesticated for agricultural purposes, sheep are raised for fleeces, meat (lamb, hogget or mutton) and milk. A sheep's wool is the most widely used animal fiber, and is usually harvested by shearing. In Commonwea ...
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Sheep
Sheep or domestic sheep (''Ovis aries'') are domesticated, ruminant mammals typically kept as livestock. Although the term ''sheep'' can apply to other species in the genus ''Ovis'', in everyday usage it almost always refers to domesticated sheep. Like all ruminants, sheep are members of the order Artiodactyla, the even-toed ungulates. Numbering a little over one billion, domestic sheep are also the most numerous species of sheep. An adult female is referred to as a ''ewe'' (), an intact male as a ''ram'', occasionally a ''tup'', a castrated male as a ''wether'', and a young sheep as a ''lamb''. Sheep are most likely descended from the wild mouflon of Europe and Asia, with Iran being a geographic envelope of the domestication center. One of the earliest animals to be domesticated for agricultural purposes, sheep are raised for fleeces, meat (lamb, hogget or mutton) and milk. A sheep's wool is the most widely used animal fiber, and is usually harvested by shearing. In Commonw ...
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Scree
Scree is a collection of broken rock fragments at the base of a cliff or other steep rocky mass that has accumulated through periodic rockfall. Landforms associated with these materials are often called talus deposits. Talus deposits typically have a concave upwards form, where the maximum inclination corresponds to the angle of repose of the mean debris particle size. The exact definition of scree in the primary literature is somewhat relaxed, and it often overlaps with both ''talus'' and ''colluvium''. The term ''scree'' comes from the Old Norse term for landslide, ''skriða'', while the term ''talus'' is a French word meaning a slope or embankment. In high-altitude arctic and subarctic regions, scree slopes and talus deposits are typically adjacent to hills and river valleys. These steep slopes usually originate from late-Pleistocene periglacial processes. Notable scree sites in Eastern North America include the Ice Caves at White Rocks National Recreation Area in southern Ve ...
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