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Dechmont Law
''Disambiguation: the name Dechmont, and an associated "Dechmont Hill" are also places near Cambuslang in Scotland'' Dechmont Law is a hill in Livingston, West Lothian, Scotland. It lies around 700 yards southwest of the village of Dechmont, which provides its name. It is known locally as "Decky Hill" or as "Dechmont Hill" (''Law'' is Lowland Scots for "hill"). "Deer Hill" is another peak of the same hill, to the northeast of the main peak. It is the highest hill in the Livingston area, and Arthur's Seat and the Pentland Hills can be seen from here, as well as a view down the Almond valley. Geology Dechmont Law is a volcanic plug. History The slopes show signs of agricultural terracing, from the Bronze and Iron Age, but it is unclear whether it was ever a hillfort. Its strategic position makes this likely, but there is insufficient archaeological evidence. The "Livingston Incident" In 1979, forestry worker Bob Taylor had an alleged encounter with a UFO An un ...
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Cambuslang
Cambuslang ( sco, Cammuslang, from gd, Camas Lang) is a town on the south-eastern outskirts of Greater Glasgow, Scotland. With approximately 30,000 residents, it is the 27th largest town in Scotland by population, although, never having had a town hall, it may also be considered the largest village in Scotland. It is within the local authority area of South Lanarkshire and directly borders the town of Rutherglen to the west. Historically, it was a large civil parish incorporating the nearby hamlets of Newton, Flemington, Westburn and Halfway. Cambuslang is located just south of the River Clyde and about southeast of the centre of Glasgow. It has a long history of coal mining, from at least 1490, iron and steel making, and ancillary engineering works, most recently The Hoover Company (in the town from 1946 to 2005). The Clydebridge Steelworks and other smaller manufacturing businesses continue but most employment in the area comes from the distribution or service industrie ...
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River Almond, Lothian
The River Almond ( gd, Abhainn Amain) is a river in Lothian, Scotland. It is approximately 28 miles (45 km) long, rising at Hirst Hill in Lanarkshire near Shotts, running through West Lothian and draining into the Firth of Forth at Cramond, Edinburgh. The name Almond/Amon is simply old Celtic for "river". Environment Running through areas that were dominated for much of the 20th century by heavy industry and shale- and coal mining, the River Almond has long been notorious for its high levels of pollution. With the demise of mining and heavy industry in Central Scotland, the river became cleaner, and it is being actively repopulated by wildlife: there is a healthy population of brown trout and there are improving runs of both Atlantic salmon (''Salmo salar'') and sea trout (''Salmo trutta''). There is also a good array of birds to be seen around the river banks, including dippers, kingfishers and grey herons, and increasing numbers of otters are being reported. The river is ...
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Volcanic Plugs Of Scotland
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ...
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Hills Of The Scottish Midland Valley
A hill is a landform that extends above the surrounding terrain. It often has a distinct Summit (topography), summit. Terminology The distinction between a hill and a mountain is unclear and largely subjective, but a hill is universally considered to be not as tall, or as Grade (slope), steep as a mountain. Geographers historically regarded mountains as hills greater than above sea level, which formed the basis of the plot of the 1995 film ''The Englishman who Went up a Hill but Came down a Mountain''. In contrast, hillwalkers have tended to regard mountains as peaks above sea level. The ''Oxford English Dictionary'' also suggests a limit of and Whittow states "Some authorities regard eminences above as mountains, those below being referred to as hills." Today, a mountain is usually defined in the UK and Ireland as any summit at least high, while the official UK government's definition of a mountain is a summit of or higher. Some definitions include a topographical pro ...
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Hillfort
A hillfort is a type of earthwork used as a fortified refuge or defended settlement, located to exploit a rise in elevation for defensive advantage. They are typically European and of the Bronze Age or Iron Age. Some were used in the post-Roman period. The fortification usually follows the contours of a hill and consists of one or more lines of earthworks, with stockades or defensive walls, and external ditches. Hillforts developed in the Late Bronze and Early Iron Age, roughly the start of the first millennium BC, and were used in many Celtic areas of central and western Europe until the Roman conquest. Nomenclature The spellings "hill fort", "hill-fort" and "hillfort" are all used in the archaeological literature. The ''Monument Type Thesaurus'' published by the Forum on Information Standards in Heritage lists ''hillfort'' as the preferred term. They all refer to an elevated site with one or more ramparts made of earth, stone and/or wood, with an external ditch. Many ...
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Iron Age
The Iron Age is the final epoch of the three-age division of the prehistory and protohistory of humanity. It was preceded by the Stone Age (Paleolithic, Mesolithic, Neolithic) and the Bronze Age (Chalcolithic). The concept has been mostly applied to Iron Age Europe and the Ancient Near East, but also, by analogy, to other parts of the Old World. The duration of the Iron Age varies depending on the region under consideration. It is defined by archaeological convention. The "Iron Age" begins locally when the production of iron or steel has advanced to the point where iron tools and weapons replace their bronze equivalents in common use. In the Ancient Near East, this transition took place in the wake of the Bronze Age collapse, in the 12th century BC. The technology soon spread throughout the Mediterranean Basin region and to South Asia (Iron Age in India) between the 12th and 11th century BC. Its further spread to Central Asia, Eastern Europe, and Central Europe is somewhat dela ...
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Bronze Age
The Bronze Age is a historic period, lasting approximately from 3300 BC to 1200 BC, characterized by the use of bronze, the presence of writing in some areas, and other early features of urban civilization. The Bronze Age is the second principal period of the three-age system proposed in 1836 by Christian Jürgensen Thomsen for classifying and studying ancient societies and history. An ancient civilization is deemed to be part of the Bronze Age because it either produced bronze by smelting its own copper and alloying it with tin, arsenic, or other metals, or traded other items for bronze from production areas elsewhere. Bronze is harder and more durable than the other metals available at the time, allowing Bronze Age civilizations to gain a technological advantage. While terrestrial iron is naturally abundant, the higher temperature required for smelting, , in addition to the greater difficulty of working with the metal, placed it out of reach of common use until the end o ...
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Volcanic Plug
A volcanic plug, also called a volcanic neck or lava neck, is a volcanic object created when magma hardens within a vent on an active volcano. When present, a plug can cause an extreme build-up of high gas pressure if rising volatile-charged magma is trapped beneath it, and this can sometimes lead to an explosive eruption. In a plinian eruption the plug is destroyed and ash is ejected. Glacial erosion can lead to exposure of the plug on one side, while a long slope of material remains on the opposite side. Such landforms are called crag and tail. If a plug is preserved, erosion may remove the surrounding rock while the erosion-resistant plug remains, producing a distinctive upstanding landform. Examples of volcanic plugs Africa Near the village of Rhumsiki in the Far North Province of Cameroon, Kapsiki Peak is an example of a volcanic plug and is one of the most photographed parts of the Mandara Mountains. Spectacular volcanic plugs are present in the center of La Gomer ...
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Pentland Hills
The Pentland Hills are a range of hills southwest of Edinburgh, Scotland. The range is around in length, and runs southwest from Edinburgh towards Biggar and the upper Clydesdale. Etymology The name is first recorded for the farm of Pentland ( 1050, 1200) and probably derives from Brythonic ''pen llan'', head or top end of the church or enclosure. In the late 15th to mid-16th centuries, land transfers refer to Pentlandmure and Pentland – documents that also list adjacent parcels of land with such still-recognisable names as Loganehous, Hilend, Boghall and Mortounhall. 'Muir', in Pentlandmure, describes common grazings where the farm's livestock would be pastured in summer; and gradually the name was linked more specifically with the slopes of the nearby hills (perhaps Allermuir, Woodhouselee or Castlelaw). The name is completely unrelated to the name of the Pentland Firth in the north of Scotland. Timothy Pont mapped the area in the 1590s, and his work appeared in the ma ...
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West Lothian
West Lothian ( sco, Wast Lowden; gd, Lodainn an Iar) is one of the 32 council areas of Scotland, and was one of its shires of Scotland, historic counties. The county was called Linlithgowshire until 1925. The historic county was bounded geographically by the River Avon, Falkirk, Avon to the west and the River Almond, Lothian, Almond to the east. The modern council area occupies a larger area than the historic county. It was reshaped following local government reforms in 1975: some areas in the west were transferred to Falkirk (council area), Falkirk; some areas in the east were transferred to Edinburgh; and some areas that had formerly been part of in Midlothian were added to West Lothian. West Lothian lies on the southern shore of the Firth of Forth and is predominantly rural, though there were extensive coal, iron, and shale oil mining operations in the 19th and 20th centuries. These created distinctive red-spoil heaps (locally known as "bing (mining), bings") throughout the ...
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Arthur's Seat
Arthur's Seat ( gd, Suidhe Artair, ) is an ancient volcano which is the main peak of the group of hills in Edinburgh, Scotland, which form most of Holyrood Park, described by Robert Louis Stevenson as "a hill for magnitude, a mountain in virtue of its bold design". It is situated just to the east of the city centre, about to the east of Edinburgh Castle. The hill rises above the city to a height of , provides excellent panoramic views of the city and beyond, is relatively easy to climb, and is popular for hillwalking. Though it can be climbed from almost any direction, the easiest and simplest ascent is from the east, where a grassy slope rises above Dunsapie Loch. At a spur of the hill, Salisbury Crags has historically been a rock climbing venue with routes of various degrees of difficulty. Until recently rock climbing was restricted to the South Quarry, but access is currently banned altogether by Historic Environment Scotland. Name It is sometimes said that its name is de ...
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Hill
A hill is a landform that extends above the surrounding terrain. It often has a distinct Summit (topography), summit. Terminology The distinction between a hill and a mountain is unclear and largely subjective, but a hill is universally considered to be not as tall, or as Grade (slope), steep as a mountain. Geographers historically regarded mountains as hills greater than above sea level, which formed the basis of the plot of the 1995 film ''The Englishman who Went up a Hill but Came down a Mountain''. In contrast, hillwalkers have tended to regard mountains as peaks above sea level. The ''Oxford English Dictionary'' also suggests a limit of and Whittow states "Some authorities regard eminences above as mountains, those below being referred to as hills." Today, a mountain is usually defined in the UK and Ireland as any summit at least high, while the official UK government's definition of a mountain is a summit of or higher. Some definitions include a topographical pro ...
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