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Benbecula Airport Building
Benbecula (; gd, Beinn nam Fadhla or ) is an island of the Outer Hebrides in the Atlantic Ocean off the west coast of Scotland. In the 2011 census, it had a resident population of 1,283 with a sizable percentage of Roman Catholics. It is in a zone administered by or the Western Isles Council. The island is about from west to east and a similar distance from north to south. It lies between the islands of North Uist and South Uist and is connected to both by road causeways. Benbecula's main settlement and administrative centre is Balivanich (Scottish Gaelic: ''Baile a' Mhanaich'', meaning "Town of the Monk"). In 1746, Bonnie Prince Charlie was caught in a storm and forced to land on Benbecula. The population of Benbecula were sympathetic to the Jacobite cause, and smuggled him off the island to safety, as the song has it: "over the sea to Skye". In 2006, local residents took control of parts of the island in a community buy-out. The previous landowners, a sporting syndicate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uist
"Uist" is a group of six islands and are part of the Outer Hebridean Archipelago, part of the Outer Hebrides of Scotland. North Uist and South Uist ( or ; gd, Uibhist ) are two of the islands and are linked by causeways running via the isles of Benbecula and Grimsay. From south to north, the inhabited islands in the island group are (Eriskay), (South Uist), Grimsay (South), (Benbecula), ( Flodaigh), ( Grimsay (North)), , (North Uist), (Baleshare) and ( Berneray). The islands, collectively, have a population of 4,723. Major settlements The main settlements in Uist are: South Uist * (Daliburgh) * (Lochboisdale) * ( Snishvale) * (Stoneybridge) * (Eochar) * ( Polochar) * (Eriskay) Benbecula * (Balivanich) * ( Creagorry) * ( Liniclate) North Uist * ( Carinish) * ( Bayhead) * (Sollas) * (Lochmaddy) * (Balemore) 16th century Geography Writing in 1549, Sir Donald Monro, High Dean of the Isles stated of "Ywst" that it was a fertile country full of hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Folk Etymology
Folk etymology (also known as popular etymology, analogical reformation, reanalysis, morphological reanalysis or etymological reinterpretation) is a change in a word or phrase resulting from the replacement of an unfamiliar form by a more familiar one. The form or the meaning of an archaic, foreign, or otherwise unfamiliar word is reinterpreted as resembling more familiar words or morphemes. The term ''folk etymology'' is a loan translation from German language, German ''Volksetymologie'', coined by Ernst Förstemann in 1852. Folk etymology is a Productivity (linguistics), productive process in historical linguistics, language change, and social relation, social interaction. Reanalysis of a word's history or original form can affect its spelling, pronunciation, or meaning. This is frequently seen in relation to loanwords or words that have become archaic or obsolete. Examples of words created or changed through folk etymology include the English dialectal form wikt:sparrowgrass ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Foliation (geology)
Foliation in geology refers to repetitive layering in metamorphic rocks.Marshak, Stephen, ''Essentials of Geology,'' W. W. Norton 3rd Ed, 2009 Each layer can be as thin as a sheet of paper, or over a meter in thickness. The word comes from the Latin ''folium'', meaning "leaf", and refers to the sheet-like planar structure. It is caused by shearing forces (pressures pushing different sections of the rock in different directions), or differential pressure (higher pressure from one direction than in others). The layers form parallel to the direction of the shear, or perpendicular to the direction of higher pressure. Nonfoliated metamorphic rocks are typically formed in the absence of significant differential pressure or shear. Foliation is common in rocks affected by the regional metamorphic compression typical of areas of mountain belt formation (orogenic belts). More technically, foliation is any penetrative planar fabric present in metamorphic rocks. Rocks exhibiting foliat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amphibolite
Amphibolite () is a metamorphic rock that contains amphibole, especially hornblende and actinolite, as well as plagioclase feldspar, but with little or no quartz. It is typically dark-colored and dense, with a weakly foliated or schistose (flaky) structure. The small flakes of black and white in the rock often give it a salt-and-pepper appearance. Amphibolite frequently forms by metamorphism of mafic igneous rocks, such as basalt. However, because metamorphism creates minerals entirely based upon the chemistry of the protolith, certain 'dirty marls' and volcanic sediments may also metamorphose to an amphibolite assemblage. Deposits containing dolomite and siderite also readily yield amphibolite (tremolite-schist, grunerite-schist, and others) especially where there has been a certain amount of contact metamorphism by adjacent granitic masses. Metamorphosed basalt (metabasalt) creates ''ortho-amphibolite'' and other chemically appropriate lithologies create ''para-amphibolite''. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scourian Orogeny
The Scourian orogeny was an orogeny mountain building event 2.6 billion years ago during the Archean before the beginning of the Laxfordian orogeny (or potentially overlapping with the beginning of the Laxfordian. The orogeny is marked by northwest-southeast trending folds south of Laxford in northwest Scotland. The event affected the Lewisian gneiss The Lewisian complex or Lewisian gneiss is a suite of Precambrian metamorphic rocks that outcrop in the northwestern part of Scotland, forming part of the Hebridean Terrane and the North Atlantic Craton. These rocks are of Archaean and Paleopr .... Rubidium-strontium dating indicated Scourian metamorphism took place between 2.6 and 2.7 billion years ago{{cite book , year=1977, title= Precambrian of the Northern Hemisphere, url=https://archive.org/details/precambriannorth00salo, url-access=limited, publisher=Elsevier, 50} References Archean orogenies Geology of Scotland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Archean
The Archean Eon ( , also spelled Archaean or Archæan) is the second of four geologic eons of Earth's history, representing the time from . The Archean was preceded by the Hadean Eon and followed by the Proterozoic. The Earth Earth is the third planet from the Sun and the only astronomical object known to harbor life. While large volumes of water can be found throughout the Solar System, only Earth sustains liquid surface water. About 71% of Earth's surfa ... during the Archean was mostly a water world: there was continental crust, but much of it was under an ocean deeper than today's ocean. Except for some trace minerals, today's oldest continental crust dates back to the Archean. Much of the geological detail of the Archean has been destroyed by subsequent activity. The Earliest known life forms, earliest known life started in the Archean. Life was simple throughout the Archean, mostly represented by shallow-water microbial mats called stromatolites, and the a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lewisian Gneiss
The Lewisian complex or Lewisian gneiss is a suite of Precambrian metamorphic rocks that outcrop in the northwestern part of Scotland, forming part of the Hebridean Terrane and the North Atlantic Craton. These rocks are of Archaean and Paleoproterozoic age, ranging from 3.0–1.7 billion years ( Ga). They form the basement on which the Torridonian and Moine Supergroup sediments were deposited. The Lewisian consists mainly of granitic gneisses with a minor amount of supracrustal rocks. Rocks of the Lewisian complex were caught up in the Caledonian orogeny, appearing in the hanging walls of many of the thrust faults formed during the late stages of this tectonic event. Distribution The main outcrops of the Lewisian complex are on the islands of the Outer Hebrides, including Lewis, from which the complex takes its name. It is also exposed on several islands of the Inner Hebrides, small islands north of the Scottish mainland and forms a coastal strip on the mainland from near L ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Western Isles
The Outer Hebrides () or Western Isles ( gd, Na h-Eileanan Siar or or ("islands of the strangers"); sco, Waster Isles), sometimes known as the Long Isle/Long Island ( gd, An t-Eilean Fada, links=no), is an island chain off the west coast of mainland Scotland. The islands are geographically coextensive with , one of the 32 unitary council areas of Scotland. They form part of the archipelago of the Hebrides, separated from the Scottish mainland and from the Inner Hebrides by the waters of the Minch, the Little Minch, and the Sea of the Hebrides. Scottish Gaelic is the predominant spoken language, although in a few areas English speakers form a majority. Most of the islands have a bedrock formed from ancient metamorphic rocks, and the climate is mild and oceanic. The 15 inhabited islands have a total population of and there are more than 50 substantial uninhabited islands. The distance from Barra Head to the Butt of Lewis is roughly . There are various important prehistor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uachdar
Uachdar ( gd, An t-Uachdar ) is a settlement on the Outer Hebridean Island of Benbecula. Uachdar is within the parish of South Uist South Uist ( gd, Uibhist a Deas, ; sco, Sooth Uist) is the second-largest island of the Outer Hebrides in Scotland. At the 2011 census, it had a usually resident population of 1,754: a decrease of 64 since 2001. The island, in common with the .... The settlement is home to the only bakery on Benbecula, MacLeans Hebridean Bakery, which also has a small shop in the same complex as the bakery itself. References External links MacLeans Hebridean Bakery Villages in the Outer Hebrides Benbecula {{WesternIsles-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Accordion
Accordions (from 19th-century German ''Akkordeon'', from ''Akkord''—"musical chord, concord of sounds") are a family of box-shaped musical instruments of the bellows-driven free-reed aerophone type (producing sound as air flows past a reed in a frame), colloquially referred to as a squeezebox. A person who plays the accordion is called an accordionist. The concertina , harmoneon and bandoneón are related. The harmonium and American reed organ are in the same family, but are typically larger than an accordion and sit on a surface or the floor. The accordion is played by compressing or expanding the bellows while pressing buttons or keys, causing ''pallets'' to open, which allow air to flow across strips of brass or steel, called '' reeds''. These vibrate to produce sound inside the body. Valves on opposing reeds of each note are used to make the instrument's reeds sound louder without air leaking from each reed block.For the accordion's place among the families of musical ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lenition
In linguistics, lenition is a sound change that alters consonants, making them more sonority hierarchy, sonorous. The word ''lenition'' itself means "softening" or "weakening" (from Latin 'weak'). Lenition can happen both synchronic analysis, synchronically (within a language at a particular point in time) and historical linguistics, diachronically (as a evolutionary linguistics, language changes over time). Lenition can involve such changes as Voice (phonetics), voicing a voiceless consonant, causing a consonant to relax Occlusive, occlusion, to lose its place of articulation (a phenomenon called ''debuccalization'', which turns a consonant into a glottal consonant like or ), or even causing a consonant to disappear entirely. An example of synchronic lenition is found in most varieties of American English, in the form of flapping: the of a word like ''wait'' is pronounced as the more sonorous in the related form ''waiting'' . Some varieties of Spanish language, Spanish show ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Genitive
In grammar, the genitive case (abbreviated ) is the grammatical case that marks a word, usually a noun, as modifying another word, also usually a noun—thus indicating an attributive relationship of one noun to the other noun. A genitive can also serve purposes indicating other relationships. For example, some verbs may feature arguments in the genitive case; and the genitive case may also have adverbial uses (see adverbial genitive). Genitive construction includes the genitive case, but is a broader category. Placing a modifying noun in the genitive case is one way of indicating that it is related to a head noun, in a genitive construction. However, there are other ways to indicate a genitive construction. For example, many Afroasiatic languages place the head noun (rather than the modifying noun) in the construct state. Possessive grammatical constructions, including the possessive case, may be regarded as a subset of genitive construction. For example, the genitive construc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
