Slate Islands, Scotland
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Slate Islands, Scotland
The Slate Islands are an island group in the Inner Hebrides, lying immediately off the west coast of Scotland, north of Jura, Scotland, Jura and southwest of Oban. The main islands are Seil, Easdale, Luing, Shuna, Slate Islands, Shuna, Torsa and Belnahua. Scarba and Kerrera, which lie nearby, are not usually included. The underlying geology of the islands is Dalradian slate, which was quarried widely until the mid-20th century. Quarry working began in 1630 and at the turn of the 20th century, the quarries were yielding some eight million slates every year. The Garvellachs lie to the southwest. Definition Unlike some of Scotland's larger archipelagos such as Orkney and the Outer Hebrides, which are distant from other islands and also have their own Council area, local authority, the Slate Islands have no formal definition. The islands from which the slate that gives rise to the name was quarried on a substantial commercial basis are Easdale, Belnahua, Luing and Seil. The webs ...
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Easdale Village - Panoramio
Easdale () is one of the Slate Islands, in the Firth of Lorn, Scotland. Once the centre of the Scottish slate industry, there has been some recent island regeneration by the owners. This is the smallest of the Inner Hebrides' inhabited islands and is "home to traditional white-washed cottages, a small pub and disused slate quarries". One of the latter, filled with water, is used for swimming. A ferry sails from Easdale to Ellenabeich (Gaelic: ''Eilean nam Beathach'') on the nearby island of Seil (Gaelic: ''Saoil''), which is separated from Easdale by only a narrow channel. Confusingly, Ellenabeich is sometimes known as ''Easdale'' as a result of its traditional connections with the island. Etymology In 1549, Donald Monro, " Dean of the Isles" wrote, in brief reference to Easdale, of an island "namit in the Erische Leid Ellan Eisdcalfe" However the derivation of "Eisdcalfe" and this word's etymological relationship to "Easdale" is not clear. Haswell Smith (2004) notes that ''ea ...
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Garvellachs
The Garvellachs (Scottish Gaelic: ''Na Garbh Eileacha'') or Isles of the Sea form a small archipelago in the Inner Hebrides of Scotland. The islands include Garbh Eileach, Dùn Chonnuill and Eileach an Naoimh. Part of the Argyll and Bute council area, they lie in Firth of Lorne west of Lunga and northwest of Scarba and have been uninhabited since the 19th century. The islands are known for their early Christian connections to Brendan the Navigator and Columba and for their bedrock containing rare formations in relation to the global Sturtian glaciation. Overview The waters surrounding the islands are extensively used for leisure sailing. Due to the array of separate tidal races produced by the underwater topography there are some treacherous stretches of water. These include the Grey Dog between Scarba and Lunga and the Gulf of Corryvreckan, between Scarba and Jura, in which is located the infamous Corryvreckan whirlpool, which is the third-largest whirlpool in the wor ...
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Hectare
The hectare (; SI symbol: ha) is a non-SI metric unit of area equal to a square with 100-metre sides (1 hm2), that is, square metres (), and is primarily used in the measurement of land. There are 100 hectares in one square kilometre. An acre is about and one hectare contains about . In 1795, when the metric system was introduced, the ''are'' was defined as 100 square metres, or one square decametre, and the hectare (" hecto-" + "are") was thus 100 ''ares'' or  km2 ( square metres). When the metric system was further rationalised in 1960, resulting in the International System of Units (), the ''are'' was not included as a recognised unit. The hectare, however, remains as a non-SI unit accepted for use with the SI and whose use is "expected to continue indefinitely". Though the dekare/decare daa () and are (100 m2) are not officially "accepted for use", they are still used in some contexts. Description The hectare (), although not a unit of SI, is ...
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Blaeu - Atlas Of Scotland 1654 - LORNA - The Firth Of Lorn
Blaeu is the name of * Willem Blaeu (1571–1638), Dutch cartographer and father of Joan Blaeu * Joan Blaeu (1596–1673), Dutch cartographer and son of Willem Blaeu * ''Blaeu Atlas of Scotland'', by Joan Blaeu, published in 1654 * ''Atlas Blaeu'' or ''Atlas Maior'', by Joan Blaeu, published in 1635 * ''Stedenboek Blaeu'' or '' Toonneel der Steeden'', by Joan Blaeu, published in 1649 See also * Blaauw Blaauw () is a Dutch language, Dutch surname. It is an archaic spelling of modern Dutch ''blauw'', meaning ''blue''. This may have referred to the pale skin, the eyes, or the clothes of the original bearer of the name or the surname may be metonymic ...
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Skerry
A skerry ( ) is a small rocky island, or islet, usually too small for human habitation. It may simply be a rocky reef. A skerry can also be called a low stack (geology), sea stack. A skerry may have vegetative life such as moss and small, hardy grasses. They are often used as resting places by animals such as Pinniped, seals and seabird, birds. Etymology The term ''skerry'' is derived from the Old Norse ', which means a small rocky island in the sea (which in turn derives from the Proto-Indo-European root *''sker''-, "cut", in the sense of a rock cut off from the land). The Old Norse term ' was brought into the English language via the Scots language word spelled or . It is a cognate of the Scandinavian languages' words for ''skerry'' – Icelandic language, Icelandic, , , , , found also in , , , , and (). In Scottish Gaelic, it appears as ', e.g. Sula Sgeir, in Irish language, Irish as '','' in Welsh language, Welsh as '','' and in Manx language, Manx as ''.'' Formatio ...
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Quartzite
Quartzite is a hard, non- foliated metamorphic rock that was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts, and hence quartzite is a metasandstone. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resist ...
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Eilean Dubh Mòr
Eilean Dubh Mòr () is an uninhabited island in the Inner Hebrides of Scotland. It lies at the mouth of the Firth of Lorn The Firth of Lorn or Lorne () is the inlet of the sea between the south-east coast of the Isle of Mull and the mainland of Scotland. It includes a number of islands, and is noted for the variety of wildlife habitats that are found. In 2005, a l ..., between the islands of Lunga and Garbh Eileach. The area of the island has been measured variously—at by Livingstone and by Haswell-Smith, the latter including the nearby islet of Eilean Dubh Beag (), which is joined to Eilean Dubh Mòr at low tide. Footnotes External links Uninhabited islands of Argyll and Bute {{Argyll-geo-stub ...
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Lunga, Firth Of Lorn
Lunga is one of the Slate Islands in the Firth of Lorn in Argyll and Bute, Scotland. The "Grey Dog" tidal race, which runs in the sea channel to the south, reaches in full flood. The name "Lunga" is derived from the Old Norse for "isle of the longships', but almost all other place names are Gaelic in origin. The population was never substantial and today the main activity is an adventure centre on the northern headland of ''Rubha Fiola''. The surrounding seas are fished for prawns and scallops and there is a salmon farm off the south eastern shores. The Special Area of Conservation of which the island is part hosts a growing number of outdoor leisure pursuits. Geography Lunga is west of Luing and just north of Scarba. The nearest town is Oban, some to the north. The channel to the south, ''Bealach a' Choin Ghlais'' (pass of the grey dog), is only wide and is scoured by the notorious "Grey Dog" tidal race which reaches when in full flood. According to an 1845 description: ...
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Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), 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 (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ...
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Gazetteer For Scotland
The ''Gazetteer for Scotland'' is a gazetteer covering the geography, history and people of Scotland. It was conceived in 1995 by Bruce Gittings of the University of Edinburgh and David Munro of the Royal Scottish Geographical Society, and contains 25,870 entries as of July 2019. It claims to be "the largest dedicated Scottish resource created for the web". The Gazetteer for Scotland provides a carefully researched and editorially validated resource widely used by students, researchers, tourists and family historians with interests in Scotland. Following on from a strong Scottish tradition of geographical publishing, the ''Gazetteer for Scotland'' is the first comprehensive gazetteer to be produced for the country since Francis Groome's '' Ordnance Gazetteer of Scotland'' (1882–1886) (the text of which is incorporated into relevant entries). The aim is not to produce a travel guide, of which there are many, but to write a substantive and thoroughly edited description of ...
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Council Area
{{Unreferenced, date=May 2019, bot=noref (GreenC bot) A council area is one of the areas defined in Schedule 1 of the Local Government etc. (Scotland) Act 1994 and is under the control of one of the local authorities in Scotland created by that Act. Legislation Local Government (Scotland) Act 1889 In Scotland, local government counties were created under the Local Government (Scotland) Act 1889. The 1889 legislation created county councils, turned each civil county (with one exception) into a contiguous area (without separate fragments) and adjusted boundaries where civil parishes straddled county boundaries, or had fragments in more than one county. The counties of Ross and Cromarty were merged to form Ross and Cromarty. Local Government (Scotland) Act 1973 Under the Local Government (Scotland) Act 1973, local government counties, cities and their subordinate councils (including burghs and parishes) were abolished and replaced by an upper tier of ''regions'' each of which ...
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Outer Hebrides
The Outer Hebrides ( ) or Western Isles ( , or ), sometimes known as the Long Isle or Long Island (), is an Archipelago, island chain off the west coast of mainland Scotland. It is the longest archipelago in the British Isles. The islands 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. The Outer Hebrides are considered to be the traditional heartland of the Gaelic language. The islands form one of the 32 council areas of Scotland, which since 1998 has used only the Gaelic form of its name, including in English language contexts. The council area is called Na h-Eileanan an Iar ('the Western Isles') and its council is ('Council of the Western Isles'). Most of the islands have a bedrock formed from ancient metamorphic rocks, and the climate is mild and oceanic. The 15 inhabited islands had a total population of in and there are more th ...
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