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West Lomond
West Lomond is the highest point in the county of Fife, Scotland and the highest peak in the Lomond Hills. Its cone-shaped summit, which is the remains of a volcanic plug, rises above an escarpment of Carboniferous sandstone and limestone layers, capped with a quartz-microgabbro sill. The conspicuous peaks of West Lomond, and its neighbour East Lomond, are visible for many miles around, which explains one suggested origin of their name, the 'Lomond' or 'beacon' hills. On the summit are the remains of an Iron Age hill fort. West Lomond is usually climbed from Craigmead car park on the Falkland-Leslie road which is at a height of almost 300 metres. Another route of ascent leaves from the Bunnet Stane and climbs diagonally up the steep north slopes of the escarpment to a gap in the cliffs, gaining the plateau a short distance from the summit cone. This route is steeper and begins at a much lower altitude than the Craigmead car park. Geodesy Until 1891 West Lomond was the meridi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Howe Of Fife take their name from the area.
The Howe of Fife is the broad, low-lying valley of the River Eden, lying between the Ochil Hills and the Lomond Hills in Fife, Scotland. ''Howe'', in Scots means a hollow or a plain bounded by hills. The alternative terms ''Laich of Fife'' and the ''Valley of Eden'' have fallen from use, as has ''Stratheden'', save for the hospital near Cupar. Cupar-based Howe of Fife RFC Howe of Fife RFC is a rugby union club based in Cupar, Fife, Scotland. It was founded in 1921, and they play in blue and white hoops. References Geography of Fife Valleys of Scotland {{Fife-geo-stub ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartz-dolerite
Quartz dolerite or quartz diabase is an intrusive rock similar to dolerite (also called diabase), but with an excess of quartz. Dolerite is similar in composition to basalt, which is volcanic, and gabbro, which is plutonic. The differing crystal sizes are due to the different rate of cooling, basalt cools quickly and has a very fine structure, while gabbro cools very slowly, at great depth, and large crystals develop. Dolerite is intermediate. Quartz dolerite is very common in central Scotland, in intrusive formations, sills and dykes, and is widely quarried for roadstone. It was used with some success for making millstones at one time, the Millstone Grit part of the carboniferous strata not being present in Scotland, but it is no longer used for this purpose, and would probably be illegal now due to the formation of small quartz and other silicate particles, which could cause the serious respiratory disease silicosis Silicosis is a form of occupational lung disease caused b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marilyns Of Scotland
This is a list of Marilyn hills and mountains in the United Kingdom, Isle of Man and Ireland by height. Marilyns are defined as peaks with a prominence of or more, regardless of height or any other merit (e.g. topographic isolation, as used in 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) '' Monroe''. The list of Marilyns was extended to Ireland by Clem Clements. Marilyn was the first of several subsequent British Isles classifications that rely solely on prominence, including the P600s, the HuMPs, and the TuMPs. Topographic prominence is a more difficult to estimate than t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Principal Meridian
A principal meridian is a meridian used for survey control in a large region. Canada The Dominion Land Survey of Western Canada took its origin at the First (or Principal) Meridian, located at 97°27′28.41″ west of Greenwich, just west of Winnipeg, Manitoba. This line is exactly ten miles west of the Red River at the Canada–United States border. Six other meridians were designated at four-degree intervals westward, with the seventh located in British Columbia; the second and fourth meridians form the general eastern border and the western border of Saskatchewan. United States In the United States Public Land Survey System, a principal meridian is the principal north-south line used for survey control in a large region, and which divides townships between east and west. The meridian meets its corresponding baseline at the point of origin, or initial point, for the land survey. For example, the Mount Diablo Meridian, used for surveys in California and Nevada, runs north-s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bunnet Stane
The Bunnet Stane (or ''bonnet stone'') is a rock formation near the hamlet of Gateside in Fife, at the foot of West Lomond. It sits upon one of the calciferous sandstone outcrops of the Old Red Sandstone suie that exist around the base of the Lomond Hills The Lomond Hills (meaning either beacon hills or bare hills), also known outside the locality as the Paps of Fife, are a range of hills in central Scotland. They lie in western central Fife and Perth and Kinross, Scotland. At West Lomond is the .... The Bunnet Stane itself consists of an elevated table of rock, about ten feet by twenty feet across, which sits upon a thin column of rock like a giant mushroom. There are several romantic explanations for the stone's shape, but it was formed entirely by the natural weathering of the exposed outcrop. Maiden's Bower There is a small man-made cave carved into the outcrop beneath the Bunnet Stane called Maiden's Bower. Originally termed ''Maiden-bore'', the term was also applied t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Falkland, Fife
Falkland ( gd, Fàclann), previously in the Lands of Kilgour ( 1200), is a village, parish and former royal burgh in Fife, Scotland, at the foot of the Lomond Hills. According to the 2008 population estimate, it has a population of 1,180. Etymology The earliest forms of this name include ''Falleland'' (c. 1128) and ''Falecklen'' (c. 1160), with the second element being the Scottish Gaelic ''lann'' (enclosure) or possibly its Pictish cognate, but the exact etymology is unclear since the first element could be the Gaelic ''falach'' (hidden), ''failc'' (wash), or ''falc'' (heavy rain). The later folk etymologies "falcon land" and "folkland" are not plausible., p. 158. In the Middle Ages, the name Falkland only applied to the Castle; the burgh and parish were known as Kilgour, which may mean "church/cell of Gabrán". History The lands of Kilgour existed at Falkland prior to the 12th century. However, this was not until the erection of Falkland Castle some time after 1160 which wa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hill Fort
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. M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Lomond
The Lomond Hills (meaning either beacon hills or bare hills), also known outside the locality as the Paps of Fife, are a range of hills in central Scotland. They lie in western central Fife and Perth and Kinross, Scotland. At West Lomond is the highest point in the county of Fife. Etymology The name ''Lomond Hills'' was first recorded ''Lomondys'' in 1315, and may derive from a Pictish cognate of Welsh ''llumon'', meaning "beacon", an element found for example in the hill-name Pumlumon in Wales. Also suggested is derivation from Gaelic ''lom monadh'', "bare hill", perhaps adapted from an earlier Pictish name containing cognate elements. Physical geography The Lomond Hills contain two prominent peaks, West Lomond and East Lomond (or Falkland Hill) (), which sit just under apart above a long north and west-facing escarpment over in length. The escarpment, made from beds of sandstone, limestone and a quartz-dolerite sill, rises steeply from the low ground to the north and w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sill (geology)
In geology, a sill is a tabular sheet intrusion that has intruded between older layers of sedimentary rock, beds of volcanic lava or tuff, or along the direction of foliation in metamorphic rock. A ''sill'' is a ''concordant intrusive sheet'', meaning that a sill does not cut across preexisting rock beds. Stacking of sills builds a sill complex . and a large magma chamber at high magma flux. In contrast, a dike is a discordant intrusive sheet, which does cut across older rocks. Sills are fed by dikes, except in unusual locations where they form in nearly vertical beds attached directly to a magma source. The rocks must be brittle and fracture to create the planes along which the magma intrudes the parent rock bodies, whether this occurs along preexisting planes between sedimentary or volcanic beds or weakened planes related to foliation in metamorphic rock. These planes or weakened areas allow the intrusion of a thin sheet-like body of magma paralleling the existing bedding pla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
