Lochaline Hotel 2014
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Lochaline Hotel 2014
Lochaline ( gd, Loch Àlainn) is the main village in the Morvern area of Highland (council area), Highland, Scotland. The coastal village is situated at the mouth of Loch Aline, on the northern shore of Sound of Mull, the Sound of Mull. A ferry operates regularly over to Fishnish on the Isle of Mull. Population The current population of Lochaline is around 200 people. In 1930, some Gaelic-speaking residents of the archipelago of St Kilda were evacuated by Williamina Barclay and relocated to Lochaline. Many of them lived and settled in Lochaline, although with some difficulty. Transport A regular ferry operated by Caledonian MacBrayne runs over to Fishnish on the Isle of Mull. The ferry takes only about 20 minutes, runs multiple times a day, and day trips from Lochaline are possible. A snack bar by the pier is opened daily, offering hot and cold take-away snacks and beverages for the journey. There is also an infrequent bus service, 507, operated by Shiel Buses - this run ...
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Morvern
Morvern, historically also spelt Morven, is a peninsula and traditional district in the Highlands, on the west coast of Scotland. It lies south of the districts of Ardgour and Sunart, and is bounded on the north by Loch Sunart and Glen Tarbert, on the south east by Loch Linnhe and on the south west by the Sound of Mull. The name is derived from the Gaelic ''A' Mhorbhairne'' (the Sea-Gap). The highest point is the summit of the Corbett Creach Bheinn which reaches in elevation. Administratively Morvern is now part of the ward management area of Lochaber, in Highland council area. It forms part of the traditional shire and current registration county of Argyll. Morvern is approximately in area, with a current population of about 320. Prehistory and archaeology In 2010, forestry planting by the then Forestry Commission Scotland let to the discovery of a Mesolithic stone tool scatter. Subsequent archaeology excavations also found evidence that people in the Bronze Age also ...
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Underwater Diving
Underwater diving, as a human activity, is the practice of descending below the water's surface to interact with the environment. It is also often referred to as diving, an ambiguous term with several possible meanings, depending on context. Immersion in water and exposure to high ambient pressure have physiological effects that limit the depths and duration possible in ambient pressure diving. Humans are not physiologically and anatomically well-adapted to the environmental conditions of diving, and various equipment has been developed to extend the depth and duration of human dives, and allow different types of work to be done. In ambient pressure diving, the diver is directly exposed to the pressure of the surrounding water. The ambient pressure diver may dive on breath-hold (freediving) or use breathing apparatus for scuba diving or surface-supplied diving, and the saturation diving technique reduces the risk of decompression sickness (DCS) after long-duration deep dives ...
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Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth b ...
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Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ...
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Crown Glass (optics)
Crown glass is a type of optical glass used in lenses and other optical components. It has relatively low refractive index (≈1.52) and low dispersion (with Abbe numbers around 60). Crown glass is produced from alkali-lime silicates containing approximately 10% potassium oxide and is one of the earliest low dispersion glasses. As well as the specific material named ''crown glass'', there are other optical glasses with similar properties that are also called crown glasses. Generally, this is any glass with Abbe numbers in the range 50 to 85. For example, the borosilicate glass Schott BK7 (Schott designates it as 517642. The first three digits tell you its refractive index (1.517) and the last three tell you its Abbé number (64.2))The crown/flint distinction is so important to optical glass technology that many glass names, notably Schott glasses, incorporate it. A ''K'' in a Schott name indicates a crown glass (''Krone'' in German — Schott is a German company). The ''B'' in ...
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Sand
Sand is a granular material composed of finely divided mineral particles. Sand has various compositions but is defined by its grain size. Sand grains are smaller than gravel and coarser than silt. Sand can also refer to a textural class of soil or soil type; i.e., a soil containing more than 85 percent sand-sized particles by mass. The composition of sand varies, depending on the local rock sources and conditions, but the most common constituent of sand in inland continental settings and non-tropical coastal settings is silica (silicon dioxide, or SiO2), usually in the form of quartz. Calcium carbonate is the second most common type of sand, for example, aragonite, which has mostly been created, over the past 500million years, by various forms of life, like coral and shellfish. For example, it is the primary form of sand apparent in areas where reefs have dominated the ecosystem for millions of years like the Caribbean. Somewhat more rarely, sand may be composed of calciu ...
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Silicon Dioxide
Silicon dioxide, also known as silica, is an oxide of silicon with the chemical formula , most commonly found in nature as quartz and in various living organisms. In many parts of the world, silica is the major constituent of sand. Silica is one of the most complex and most abundant families of materials, existing as a compound of several minerals and as a synthetic product. Notable examples include fused quartz, fumed silica, silica gel, opal and aerogels. It is used in structural materials, microelectronics (as an electrical insulator), and as components in the food and pharmaceutical industries. Structure In the majority of silicates, the silicon atom shows tetrahedral coordination, with four oxygen atoms surrounding a central Si atomsee 3-D Unit Cell. Thus, SiO2 forms 3-dimensional network solids in which each silicon atom is covalently bonded in a tetrahedral manner to 4 oxygen atoms. In contrast, CO2 is a linear molecule. The starkly different structures of the dioxid ...
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Loch
''Loch'' () is the Scottish Gaelic, Scots language, Scots and Irish language, Irish word for a lake or sea inlet. It is Cognate, cognate with the Manx language, Manx lough, Cornish language, Cornish logh, and one of the Welsh language, Welsh words for lake, llwch. In English English and Hiberno-English, the Anglicisation, anglicised spelling lough is commonly found in place names; in Lowland Scots and Scottish English, the spelling "loch" is always used. Many loughs are connected to stories of lake-bursts, signifying their mythical origin. Sea-inlet lochs are often called sea lochs or sea loughs. Some such bodies of water could also be called firths, fjords, estuary, estuaries, straits or bays. Background This name for a body of water is Insular Celtic languages, Insular CelticThe current form has currency in the following languages: Scottish Gaelic, Irish language, Irish, Manx language, Manx, and has been borrowed into Scots language, Lowland Scots, Scottish English, Iri ...
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Earls Of Argyll
Duke of Argyll ( gd, Diùc Earraghàidheil) is a title created in the peerage of Scotland in 1701 and in the peerage of the United Kingdom in 1892. The earls, marquesses, and dukes of Argyll were for several centuries among the most powerful noble families in Scotland. As such, they played a major role in Scottish history throughout the 16th, 17th, and 18th centuries. The Duke of Argyll also holds the hereditary titles of chief of Clan Campbell and Master of the Household of Scotland. Since 2001, Torquhil Campbell has been Duke of Argyll and is the thirteenth man to hold the title. History Sir Colin Campbell of Lochow was knighted in 1280. In 1445 James II of Scotland raised Sir Colin's descendant Sir Duncan Campbell to the peerage to become Duncan Campbell of Lochow, Lord of Argyll, Knight, 1st Lord Campbell. Colin Campbell (c. 1433–1493) succeeded his grandfather as the 2nd Lord Campbell in 1453 and was created Earl of Argyll in 1457. The 8th Earl of Argyll was c ...
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Iona
Iona (; gd, Ì Chaluim Chille (IPA: iːˈxaɫ̪ɯimˈçiʎə, sometimes simply ''Ì''; sco, Iona) is a small island in the Inner Hebrides, off the Ross of Mull on the western coast of Scotland. It is mainly known for Iona Abbey, though there are other buildings on the island. Iona Abbey was a centre of Gaelic monasticism for three centuries and is today known for its relative tranquility and natural environment. It is a tourist destination and a place for spiritual retreats. Its modern Scottish Gaelic name means "Iona of (Saint) Columba" (formerly anglicised as "Icolmkill"). In 2019, the island's estimated population was 120. Residents engage in farming, using traditional methods. Other occupations include crofting and tourism-related work; some craftsmen make goods for sale locally, such as pottery, tapestries, jewellery and knitted goods. In March 1980, the Hugh Fraser Foundation donated much of the main island (and its off-lying islands) to the current owner, the National ...
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John Of Islay, Lord Of The Isles
:''This article refers to John I, Lord of the Isles; for John II, see John of Islay, Earl of Ross'' John of Islay (or John MacDonald) ( gd, Eòin Mac Dòmhnuill or gd, Iain mac Aonghais Mac Dhòmhnuill) (died 1386) was the Lord of the Isles (1336–1386) and chief of Clan Donald. In 1336, he styled himself ''Dominus Insularum'', "Lord of the Isles"; although this was not the first ever recorded instance of the title in use. Some modern historians nevertheless count John as the first of the later medieval Lords of the Isles, although this rather broad Latin style corresponds roughly with the older Gaelic title ''Rí Innse Gall'' ("King of the Isles"), in use since the Viking Age. For instance, the even more similar Latin title ''dominus de Inchegal'' ("Lord of the Hebrides"), applied to Raghnall Mac Somhairle in the mid-12th century. In fact John is actually styled ''Rí Innsi Gall'' or King of the Isles shortly after his death in a contemporary entry in the Irish Annals of Ulste ...
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Clan Donald
Clan Donald, also known as Clan MacDonald ( gd, Clann Dòmhnaill; Mac Dòmhnaill ), is a Highland Scottish clan and one of the largest Scottish clans. The Lord Lyon King of Arms, the Scottish official with responsibility for regulating heraldry in that country, issuing new grants of coats of arms, and serving as the judge of the Court of the Lord Lyon, recognises under Scottish law the ''High Chief of Clan Donald''. Historically the chiefs of the Clan Donald held the title of Lord of the Isles until 1493 and two of those chiefs also held the title of Earl of Ross until 1476. There are also numerous branches to the Clan Donald and several of these have chiefs recognised by the Lord Lyon King of Arms; these are: Clan Macdonald of Sleat, Clan Macdonald of Clanranald, Clan MacDonell of Glengarry, Clan MacDonald of Keppoch, and Clan MacAlister. There are also notable historic branches of Clan Donald without chiefs so-recognised, these are: the Clan MacDonald of Dunnyveg, Clan MacDona ...
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