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Clackmannan, Clackmannanshire
Clackmannan ( ; gd, Clach Mhanainn, perhaps meaning "Stone of Manau"), is a small town and civil parish set in the Central Lowlands of Scotland. Situated within the Forth Valley, Clackmannan is south-east of Alloa and south of Tillicoultry. The town is within the county of Clackmannanshire, of which it was formerly the county town, until Alloa overtook it in size and importance. History and toponymy Name and toponymy The name ''Clackmannan'' may be of Brittonic origin. The first element is probably ''*clog'', meaning "rock, crag, cliff" (c.f. Welsh ''clog''), and the second is the personal name ''Manau'', from the root ''man-'' meaning "projecting''. The name of the town has been said to allude to the Stone of Manau or Stone of Mannan, a pagan monument that can be seen in the town square beside the Tolbooth or Tollbooth Tower, which dates from 1592. History The early growth of the town was due in large part to the port which lay on the banks of the tidal stretch of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ochil And South Perthshire (UK Parliament Constituency)
Ochil and South Perthshire is a county constituency of the House of Commons of the Parliament of the United Kingdom. It elects one Member of Parliament (MP) by the first-past-the-post system of election. The constituency was created for the 2005 general election as a result of the Fifth Review of the Boundary Commission for Scotland. It has been represented since 2019 by John Nicolson of the Scottish National Party (SNP). Boundaries The constituency is composed of the Clackmannanshire council area (all five wards), and the Perth and Kinross council wards of Strathtay, Strathearn, Strathallan, Almond and Earn, and Kinross-shire. The constituency was created to cover Clackmannanshire and a southern portion of Perth and Kinross; the Perth and North Perthshire constituency was created at the same time to cover the rest of the Perth and Kinross council area. Prior to the 2005 election, the council areas had been covered by the Angus, Ochil, Perth and North Tayside constitu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Historic Scotland
Historic Scotland ( gd, Alba Aosmhor) was an executive agency of the Scottish Office and later the Scottish Government from 1991 to 2015, responsible for safeguarding Scotland's built heritage, and promoting its understanding and enjoyment. Under the terms of a Bill of the Scottish Parliament published on 3 March 2014, Historic Scotland was dissolved and its functions were transferred to Historic Environment Scotland (HES) on 1 October 2015. HES also took over the functions of the Royal Commission on the Ancient and Historical Monuments of Scotland. Role Historic Scotland was a successor organisation to the Ancient Monuments Division of the Ministry of Works and the Scottish Development Department. It was created as an agency in 1991 and was attached to the Scottish Executive Education Department, which embraces all aspects of the cultural heritage, in May 1999. As part of the Scottish Government, Historic Scotland was directly accountable to the Scottish Ministers. In 2 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kincardine, Fife
Kincardine ( ; gd, Cinn Chàrdainn) or Kincardine-on-Forth is a small town on the north shore of the Firth of Forth, in Fife, Scotland. The town was given the status of a burgh of barony in 1663. It was at one time a reasonably prosperous minor port. The townscape retains many good examples of Scottish vernacular buildings from the 17th, 18th and early 19th centuries, although it was greatly altered during the construction of Kincardine Bridge in 1932–1936. It is in the civil parish of Tulliallan. Etymology The name ''Kincardine'', recorded in 1540 as ''Kincarne'', may be of either Pictish or Scottish Gaelic, Gaelic origin (It is also recorded as ''Kincarnyne''). The second element is Pictish ''*carden'', conceivably Loanword, loaned into Gaelic, meaning "woodland" or perhaps "enclosure, encampment" (Middle Welsh ''cardden''). The first element is the Gaelic ''ceann'', "head end", but in view of the second element's "Pictish" distribution, it is most appropriately seen as ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clackmannanshire Bridge
The Clackmannanshire Bridge is a road bridge over the Firth of Forth in Scotland which opened to traffic on 19 November 2008. Prior to 1 October 2008 the bridge was referred to as the upper Forth crossing while the name was chosen. Background The increasing levels of traffic using the existing Kincardine Bridge led to a public inquiry being held into options to ease traffic flow over the Forth and around the small town of Kincardine. The Kincardine Bridge was the main access across the river for heavy goods vehicles during stormy weather when the Forth Road Bridge would not allow high-sided vehicles to cross during strong winds. In 2000 proposals were put forward for a number of alternatives, one of which was a new crossing running north-northwest of the existing bridge, bypassing the town of Kincardine altogether. In 2005 the new crossing was given the go-ahead, and construction began in June 2006, with the sod-cutting ceremony performed by the Scottish Transport Minister, Ta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headland Archaeology
Headland Archaeology Ltd is a wholely owned subsidiary of the RSK Group. Headland provides archaeological services and heritage advice to the construction industry. Company history Headland Archaeology Ltd was established in 1996. Headquartered in Edinburgh, this company expanded as a provider of commercial archaeology services in the UK. Expansion into the Irish market led to the establishment of Headland Archaeology (Ireland) Ltd in 2000, in County Cork, Co. Cork. Restructuring of the companies in May and June 2008 involved the renaming of Headland Archaeology Ltd as Headland Group Limited. A new company, Headland Archaeology (UK) Limited, was founded at this time to give, in conjunction with Headland Archaeology (Ireland) Ltd, a coherent structure to the group based on trading areas. The acquisition of Hereford-based Archaeological Investigations Ltd in 2010 expanded its UK operation. Archaeological Investigations Ltd was subsequently assimilated as a regional office of Head ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Robert Lorimer
Sir Robert Stodart Lorimer, KBE (4 November 1864 – 13 September 1929) was a prolific Scottish architect and furniture designer noted for his sensitive restorations of historic houses and castles, for new work in Scots Baronial and Gothic Revival styles, and for promotion of the Arts and Crafts movement. Early life Lorimer was born in Edinburgh, the son of Hannah Stodart (1835–1916) and James Lorimer, who was Regius Professor of Public Law at University of Edinburgh from 1862 to 1890. In his youth the family lived at 21 Hill Street, a Georgian house in Edinburgh's South Side, close to where his father worked at Old College. From 1877 to 1882 he was educated at Edinburgh Academy, going on to study at University of Edinburgh from 1882 to 1885, however he left without completing his studies. He was part of a talented family, being the younger brother of painter John Henry Lorimer, and father to the sculptor Hew Lorimer. In 1878 the Lorimer family acquired the lease of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous Period
The Carboniferous ( ) is a Period (geology), geologic period and System (stratigraphy), system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago (Myr, Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin ''wikt:carbo#Latin, carbō'' ("coal") and ''wikt:fero#Latin, ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare (geologist), William Conybeare and William Phillips (geologist), William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian (geology), Mississippian and the later Pennsylvanian (geology), Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Stegocephalia, Tetrapods ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Namurian
The Namurian is a stage in the regional stratigraphy of northwest Europe with an age between roughly 326 and 313 Ma (million years ago). It is a subdivision of the Carboniferous system or period and the regional Silesian series. The Namurian is named for the Belgian city and province of Namur where strata of this age occur (part of the Belgian Coal Measures). The Millstone Grit Group in the lithostratigraphy of northern England and parts of Wales is also of Namurian age. The Namurian age lasted from 326 to 313 million years ago. It is preceded by the Visean stage/age (which corresponds to the upper Carboniferous Limestone of Great Britain) and succeeded by the Westphalian stage/age (which corresponds to the lower and middle Coal Measures of Great Britain). In the official geologic timescale of the International Commission on Stratigraphy (ICS), the Namurian straddles the boundary between the Mississippian epoch (359-318 Ma) and the Pennsylvanian epoch (318-299 Ma). The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dinantian
Dinantian is the name of a series (stratigraphy), series or Epoch (reference date), epoch from the Lower Carboniferous system (stratigraphy), system in Europe. It can stand for a series of rocks in Europe or the time span in which they were deposited. The Dinantian is equal to the lower part of the Mississippian age, Mississippian series in the international geologic timescale of the International Commission on Stratigraphy, ICS. The Dinantian is named for the Belgian city of Dinant where strata of this age occur. The name is still used among European geologists. Earlier terms for the Dinantian were Bernician Series, Bernician from the Anglo-Scottish borderland, and Avonian (divided into upper (Kidwellian) and lower (Clevedonian) substages) from Kidwelly on the Welsh and Clevedon on the English sides of the Bristol Channel. References {{Geological history, p, p, state=collapsed Mississippian geochronology Carboniferous Europe Stratigraphy of Europe Carboniferous Ireland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clackmannan Group
The Clackmannan Group is the name given to a suite of rocks of late Dinantian and Namurian age laid down during the Carboniferous period in the Midland Valley of Scotland. Description The Group comprises a lower unit of coarse sandstones, siltstones, mudstone, and limestones with thin coals and ironstones known as the Lower Limestone Formation, an overlying sequence of similar rocks known as the Limestone Coal Formation, then an Upper Limestone Formation and at its top the sandstones of the Passage Formation. This last formation also includes fireclays, siltstones, mudstones, ironstones, coal and seatrocks. The Clackmannan Group conformably overlays the rocks of the Strathclyde Group and underlays the Coal Measures, this latter boundary also being conformable In mathematics, a matrix is conformable if its dimensions are suitable for defining some operation (''e.g.'' addition, multiplication, etc.). Examples * If two matrices have the same dimensions (number of rows ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coalfields
A coalfield is an area of certain uniform characteristics where coal is mined. The criteria for determining the approximate boundary of a coalfield are geographical and cultural, in addition to geological. A coalfield often groups the seams of coal, railroad companies, cultural groups, and watersheds and other geographical considerations. At one time the coalfield designation was an important category in business and industrial discussions. The terminology declined into unimportance as the 20th century progressed, and was probably only referred to by a few small railroads and history buffs by the 1980s. Renewed interest in industrial heritage and coal mining history has brought the old names of the coalfields before a larger audience. Australia New South Wales *Gunnedah Basin coalfields *Hunter Valley coalfields *South Maitland coalfields *Sydney Basin coalfields Queensland *Bowen Basin coalfields *Galilee Basin coalfields *Surat Basin coalfields *Walloon coalfields Victoria ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carbonaceous
Carbon () is a chemical element with the chemical symbol, symbol C and atomic number 6. It is nonmetallic and tetravalence, tetravalent—its atom making four electrons available to form covalent bond, covalent chemical bonds. It belongs to group 14 of the periodic table. Carbon makes up only about 0.025 percent of Earth's crust. Three Isotopes of carbon, isotopes occur naturally, Carbon-12, C and Carbon-13, C being stable, while Carbon-14, C is a radionuclide, decaying with a half-life of about 5,730 years. Carbon is one of the Timeline of chemical element discoveries#Ancient discoveries, few elements known since antiquity. Carbon is the 15th Abundance of elements in Earth's crust, most abundant element in the Earth's crust, and the Abundance of the chemical elements, fourth most abundant element in the universe by mass after hydrogen, helium, and oxygen. Carbon's abundance, its unique diversity of organic compounds, and its unusual ability to form polymers at the tempera ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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