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Lochalsh Woodland Garden
Lochalsh is a district of mainland Scotland that is currently part of the Highland council area. The Lochalsh district covers all of the mainland either side of Loch Alsh - and of Loch Duich - between Loch Carron and Loch Hourn, ie. from Stromeferry in the north on Loch Carron down to Corran on Loch Hourn (past Arnisdale at the south end of the road from Glenelg) and as (south-)west as Kintail. It was sometimes more narrowly defined as just being the hilly peninsula that lies between Loch Carron and Loch Alsh. The main settlement is Kyle of Lochalsh, located at the entrance to Loch Alsh, opposite the village of Kyleakin on the adjacent island of Skye. A ferry used to connect the two settlements but was replaced by the Skye Bridge in 1995. The earliest known inhabitants were Picts, but in the late 6th century Loch Alsh became part of the Gaelic island kingdom of Dál Riata. Between the 8th and 13th centuries the area was disputed between the kingdoms of Norway and Alba a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lochalsh
Lochalsh is a district of mainland Scotland that is currently part of the Highland (council area), Highland council area. The Lochalsh district covers all of the mainland either side of Loch Alsh - and of Loch Duich - between Loch Carron and Loch Hourn, ie. from Stromeferry in the north on Loch Carron down to Corran on Loch Hourn (past Arnisdale at the south end of the road from Glenelg) and as (south-)west as Kintail. It was sometimes more narrowly defined as just being the hilly peninsula that lies between Loch Carron and Loch Alsh. The main settlement is Kyle of Lochalsh, located at the entrance to Loch Alsh, opposite the village of Kyleakin on the adjacent island of Skye. A ferry used to connect the two settlements but was replaced by the Skye Bridge in 1995. The earliest known inhabitants were Picts, but in the late 6th century Loch Alsh became part of the Gaelic island kingdom of Dál Riata. Between the 8th and 13th centuries the area was disputed between the kingdoms of Nor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charles Edward Stuart
Charles Edward Louis John Sylvester Maria Casimir Stuart (20 December 1720 – 30 January 1788) was the elder son of James Francis Edward Stuart, grandson of James II and VII, and the Stuart claimant to the thrones of England, Scotland and Ireland from 1766 as Charles III. During his lifetime, he was also known as "the Young Pretender" and "the Young Chevalier"; in popular memory, he is known as Bonnie Prince Charlie. Born in Rome to the exiled Stuart court, he spent much of his early and later life in Italy. In 1744, he travelled to France to take part in a planned invasion to restore the Stuart monarchy under his father. When the French fleet was partly wrecked by storms, Charles resolved to proceed to Scotland following discussion with leading Jacobites. This resulted in Charles landing by ship on the west coast of Scotland, leading to the Jacobite rising of 1745. The Jacobite forces under Charles initially achieved several victories in the field, including the Battle of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fossil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lewisian Complex
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] |
Orogeny
Orogeny is a mountain building process. An orogeny is an event that takes place at a convergent plate margin when plate motion compresses the margin. An ''orogenic belt'' or ''orogen'' develops as the compressed plate crumples and is uplifted to form one or more mountain ranges. This involves a series of geological processes collectively called orogenesis. These include both structural deformation of existing continental crust and the creation of new continental crust through volcanism. Magma rising in the orogen carries less dense material upwards while leaving more dense material behind, resulting in compositional differentiation of Earth's lithosphere ( crust and uppermost mantle). A synorogenic process or event is one that occurs during an orogeny. The word "orogeny" () comes from Ancient Greek (, , + , , ). Although it was used before him, the term was employed by the American geologist G. K. Gilbert in 1890 to describe the process of mountain-building as distinguished f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loch Eriboll
__NOTOC__ Loch Eriboll (Scottish Gaelic: "Loch Euraboil") is a long sea loch on the north coast of Scotland, which has been used for centuries as a deep water anchorage as it is safe from the often stormy seas of Cape Wrath and the Pentland Firth. Bronze Age remains can be found in the area, including a souterrain and a very well preserved wheelhouse on the hillside above the west shore. A small scale lime industry developed here in the 19th century and Ard Neakie, a promontory on the eastern shore of the loch, had four large lime kilns developed in around 1870.Ard Neackie, Limekilns, Quarry Canmore. Retrieved 11 April 2021. Before the development of the coast road around the loch in 1890, the Heilam ferry ran from the quay at |
Sleat
Sleat is a peninsula and civil parish on the island of Skye in the Highland council area of Scotland, known as "the garden of Skye". It is the home of the clan ''MacDonald of Sleat''. The name comes from the Scottish Gaelic , which in turn comes from Old Norse ''sléttr'' (smooth, even), which well describes Sleat when considered in the surrounding context of the mainland, Skye and mountains that dominate the horizon all about Sleat. Geography The peninsula extends from an isthmus between the heads of Loch Eishort and Loch na Dal for southwest to Point of Sleat at the southern tip of Skye. It is bounded on the northwest by Loch Eishort and on the southeast by the Sound of Sleat. Most of Sleat, unlike most of Skye, is fairly fertile, and though there are hills, most do not reach a great height. Communities Sleat is a traditional parish that has several communities and two major landowners (the Clan Donald Lands Trust and Eilean Iarmain Estate). Most of the population li ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moine Thrust Belt
The Moine Thrust Belt or Moine Thrust Zone is a linear tectonic feature in the Scottish Highlands which runs from Loch Eriboll on the north coast south-west to the Sleat peninsula on the Isle of Skye. The thrust belt consists of a series of thrust faults that branch off the Moine Thrust itself. Topographically, the belt marks a change from rugged, terraced mountains with steep sides sculptured from weathered igneous, sedimentary and metamorphic rocks in the west to an extensive landscape of rolling hills over a metamorphic rock base to the east. Mountains within the belt display complexly folded and faulted layers and the width of the main part of the zone varies up to , although it is significantly wider on Skye. Discovery The presence of metamorphic gneisses and schists lying apparently stratigraphically above sedimentary rocks of lower Paleozoic age in the Northwest Highlands had been known since the early 19th century, convincing Roderick Murchison that the change was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Strait
A strait is an oceanic landform connecting two seas or two other large areas of water. The surface water generally flows at the same elevation on both sides and through the strait in either direction. Most commonly, it is a narrow ocean channel that lies between two land masses. Some straits are not navigable, for example because they are either too narrow or too shallow, or because of an unnavigable reef or archipelago. Straits are also known to be loci for sediment accumulation. Usually, sand-size deposits occur on both the two opposite strait exits, forming subaqueous fans or deltas. Terminology The terms ''channel'', ''pass'', or ''passage'' can be synonymous and used interchangeably with ''strait'', although each is sometimes differentiated with varying senses. In Scotland, ''firth'' or ''Kyle'' are also sometimes used as synonyms for strait. Many straits are economically important. Straits can be important shipping routes and wars have been fought for control of them. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scots Gaelic
Scottish Gaelic ( gd, Gàidhlig ), also known as Scots Gaelic and Gaelic, is a Goidelic language (in the Celtic branch of the Indo-European language family) native to the Gaels of Scotland. As a Goidelic language, Scottish Gaelic, as well as both Irish and Manx, developed out of Old Irish. It became a distinct spoken language sometime in the 13th century in the Middle Irish period, although a common literary language was shared by the Gaels of both Ireland and Scotland until well into the 17th century. Most of modern Scotland was once Gaelic-speaking, as evidenced especially by Gaelic-language place names. In the 2011 census of Scotland, 57,375 people (1.1% of the Scottish population aged over 3 years old) reported being able to speak Gaelic, 1,275 fewer than in 2001. The highest percentages of Gaelic speakers were in the Outer Hebrides. Nevertheless, there is a language revival, and the number of speakers of the language under age 20 did not decrease between the 2001 and 20 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scots Language
Scots ( endonym: ''Scots''; gd, Albais, ) is an Anglic language variety in the West Germanic language family, spoken in Scotland and parts of Ulster in the north of Ireland (where the local dialect is known as Ulster Scots). Most commonly spoken in the Scottish Lowlands, Northern Isles and northern Ulster, it is sometimes called Lowland Scots or Broad Scots to distinguish it from Scottish Gaelic, the Goidelic Celtic language that was historically restricted to most of the Scottish Highlands, the Hebrides and Galloway after the 16th century. Modern Scots is a sister language of Modern English, as the two diverged independently from the same source: Early Middle English (1150–1300). Scots is recognised as an indigenous language of Scotland, a regional or minority language of Europe, as well as a vulnerable language by UNESCO. In the 2011 United Kingdom census, 2011 Scottish Census, over 1.5 million people in Scotland reported being able to speak Scots. As there are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
