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Gigha
Gigha (; gd, Giogha, italic=yes; sco, Gigha) or the Isle of Gigha (and formerly Gigha Island) is an island off the west coast of Kintyre in Scotland. The island forms part of Argyll and Bute and has a population of 163 people. The climate is mild with higher than average sunshine hours and the soils are fertile. The main settlement is Ardminish. Gigha has been inhabited continuously since prehistoric times. It may have had an important role during the Kingdom of Dalriada and is the ancestral home of Clan MacNeill. It fell under the control of the Norse and the Lords of the Isles before becoming incorporated into modern Scotland and saw a variety of conflicts during the medieval period. The population of Gigha peaked at over 700 in the eighteenth century, but during the 20th century the island had numerous owners, which caused various problems in developing the island. By the beginning of the 21st century the population had fallen to 98. However a "community buy-out" in 2002 h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clan MacNeil
Clan MacNeil, also known in Scotland as Clan Niall, is a highland Scottish clan of Irish origin. According to their early genealogies and some sources they're descended from Eógan mac Néill and Niall of the Nine Hostages. The clan is particularly associated with the Outer Hebridean island of Barra. The early history of Clan MacNeil is obscure, however despite this the clan claims to descend from the legendary Irish King Niall of the Nine Hostages, who is counted as the 1st Clan Chief, the current Clan Chief being the 47th. The clan itself takes its name from a ''Niall'' who lived in the 13th or early 14th century, and who belonged to the same dynastic family of Cowal and Knapdale as the ancestors of the Lamonts, MacEwens of Otter, Maclachlans, and the MacSweens. While the clan is centred in Barra in the Outer Hebrides, there is a branch of the clan in Argyll (McNeill/MacNeill) that some historians have speculated was more senior in line, or possibly even unrelated. However, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ardminish
Ardminish (Scottish Gaelic: Aird Mhèanais) is the sole village on the Isle of Gigha in the Inner Hebrides, in Argyll and Bute, Scotland, and considered its "capital". It is connected to the mainland through a regular ferry service that runs to Tayinloan Tayinloan (, ) is a village situated on the west coast of the Kintyre peninsula in Argyll and Bute, Scotland. The village has a sub post office, general store and a small hotel (all currently closed), a village hall and a play park. There is a .... In 1961 it had a population of 84. Ardminish has the pier, post office and shop. The name Ardminish means "The headland of the narrow point", from a mixture of Gaelic and Norse. Image:Ardminish Bay, Gigha.jpg, Ardminish Bay, from the Gigha ferry Image:Gigha Hotel, Ardminish.jpg, The Gigha Hotel, Ardminish References Villages in Argyll and Bute Villages in the Inner Hebrides Ports and harbours of Scotland Isle of Gigha {{Argyll-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Argyll And Bute
Argyll and Bute ( sco, Argyll an Buit; gd, Earra-Ghàidheal agus Bòd, ) is one of 32 unitary authority council areas in Scotland and a lieutenancy area. The current lord-lieutenant for Argyll and Bute is Jane Margaret MacLeod (14 July 2020). The administrative centre for the council area is in Lochgilphead at Kilmory Castle, a 19th-century Gothic Revival building and estate. The current council leader is Robin Currie, a councillor for Kintyre and the Islands. Description Argyll and Bute covers the second-largest administrative area of any Scottish council. The council area adjoins those of Highland, Perth and Kinross, Stirling and West Dunbartonshire. Its border runs through Loch Lomond. The present council area was created in 1996, when it was carved out of the Strathclyde region, which was a two-tier local government region of 19 districts, created in 1975. Argyll and Bute merged the existing Argyll and Bute district and one ward of the Dumbarton district. The Dumbart ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kintyre
Kintyre ( gd, Cinn Tìre, ) is a peninsula in western Scotland, in the southwest of Argyll and Bute. The peninsula stretches about , from the Mull of Kintyre in the south to East and West Loch Tarbert in the north. The region immediately north of Kintyre is known as Knapdale. Kintyre is long and narrow, at no point more than from west coast to east coast, and is less than wide where it connects to Knapdale. The east side of the Kintyre Peninsula is bounded by Kilbrannan Sound, with a number of coastal peaks such as Torr Mor. The central spine of the peninsula is mostly hilly moorland, the highest point being Beinn an Tuirc at .Ordnance Survey. Landranger 1:50,000 Map Sheet 68 (South Kintyre & Cambeltown) The coastal areas and hinterland, however, are rich and fertile. Kintyre has long been a prized area for settlers, including the early Scots who migrated from Ulster to western Scotland and the Vikings or Norsemen who conquered and settled the area just before the start of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Argyllshire
Argyll (; archaically Argyle, in modern Gaelic, ), sometimes called Argyllshire, is a historic county and registration county of western Scotland. Argyll is of ancient origin, and corresponds to most of the part of the ancient kingdom of on Great Britain. Argyll was also a medieval bishopric with its cathedral at Lismore, as well as an early modern earldom and dukedom, the Dukedom of Argyll. It borders Inverness-shire to the north, Perthshire and Dunbartonshire to the east, and—separated by the Firth of Clyde—neighbours Renfrewshire and Ayrshire to the south-east, and Buteshire to the south. Between 1890 and 1975, Argyll was an administrative county with a county council. Its area corresponds with most of the modern council area of Argyll and Bute, excluding the Isle of Bute and the Helensburgh area, but including the Morvern and Ardnamurchan areas of the Highland council area. There was an Argyllshire constituency of the Parliament of Great Britain then Parliam ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hebrides
The Hebrides (; gd, Innse Gall, ; non, Suðreyjar, "southern isles") are an archipelago off the west coast of the Scottish mainland. The islands fall into two main groups, based on their proximity to the mainland: the Inner and Outer Hebrides. These islands have a long history of occupation (dating back to the Mesolithic period), and the culture of the inhabitants has been successively influenced by the cultures of Celtic-speaking, Norse-speaking, and English-speaking peoples. This diversity is reflected in the various names given to the islands, which are derived from the different languages that have been spoken there at various points in their history. The Hebrides are where much of Scottish Gaelic literature and Gaelic music has historically originated. Today, the economy of the islands is dependent on crofting, fishing, tourism, the oil industry, and renewable energy. The Hebrides have less biodiversity than mainland Scotland, but a significant number of seals an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hákonar Saga Hákonarsonar
''Hákonar saga Hákonarsonar'' ("The Saga of Haakon Haakonarson") or ''Hákonar saga gamla'' ("The Saga of Old Haakon") is an Old Norse Kings' Saga, telling the story of the life and reign of King Haakon Haakonarson of Norway. Content and style The circumstances of the saga's composition are exceptionally well understood, as they are recorded in some detail in '' Sturlunga saga'' (particularly ''Sturlu þáttr''): the saga was written in the 1260s (apparently 1264–65) by the Icelandic historian and chieftain Sturla Þórðarson (nephew of the noted historian Snorri Sturluson). Sturla Þórðarson was at the court of Haakon's son Magnus Lagabøte when Magnus learned of his father's death in Kirkwall in Orkney. Magnus is said to have immediately commissioned Sturla to write his father's saga. This was awkward for Sturla: 'King Hákon had instigated the death of Sturla's uncle, Snorri Sturluson, in 1241. Sturla rightly regarded Hákon as his most dangerous enemy, for he had steadf ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sill (geology)
In geology, a sill is a tabular sheet intrusion that has intruded between older layers of sedimentary rock, beds of volcanic lava or tuff, or along the direction of foliation in metamorphic rock. A ''sill'' is a ''concordant intrusive sheet'', meaning that a sill does not cut across preexisting rock beds. Stacking of sills builds a sill complex . and a large magma chamber at high magma flux. In contrast, a dike is a discordant intrusive sheet, which does cut across older rocks. Sills are fed by dikes, except in unusual locations where they form in nearly vertical beds attached directly to a magma source. The rocks must be brittle and fracture to create the planes along which the magma intrudes the parent rock bodies, whether this occurs along preexisting planes between sedimentary or volcanic beds or weakened planes related to foliation in metamorphic rock. These planes or weakened areas allow the intrusion of a thin sheet-like body of magma paralleling the existing bedding pla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Igneous Rock
Igneous rock (derived from the Latin word ''ignis'' meaning fire), or magmatic rock, is one of the three main The three types of rocks, rock types, the others being Sedimentary rock, sedimentary and metamorphic rock, metamorphic. Igneous rock is formed through the cooling and solidification of magma or lava. The magma can be derived from Partial melting, partial melts of existing rocks in either a Terrestrial planet, planet's mantle (geology), mantle or crust (geology), crust. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. Solidification into rock occurs either below the surface as intrusive rocks or on the surface as extrusive (geology), extrusive rocks. Igneous rock may form with crystallization to form granular, crystalline rocks, or without crystallization to form Volcanic glass, natural glasses. Igneous rocks occur in a wide range of geological settings: shields, platforms ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metamorphism
Metamorphism is the transformation of existing rock (the protolith) to rock with a different mineral composition or texture. Metamorphism takes place at temperatures in excess of , and often also at elevated pressure or in the presence of chemically active fluids, but the rock remains mostly solid during the transformation. Metamorphism is distinct from weathering or diagenesis, which are changes that take place at or just beneath Earth's surface. Various forms of metamorphism exist, including regional, contact, hydrothermal, shock, and dynamic metamorphism. These differ in the characteristic temperatures, pressures, and rate at which they take place and in the extent to which reactive fluids are involved. Metamorphism occurring at increasing pressure and temperature conditions is known as ''prograde metamorphism'', while decreasing temperature and pressure characterize ''retrograde metamorphism''. Metamorphic petrology is the study of metamorphism. Metamorphic petrologists re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Argyll Group
The Argyll Group is a thick sequence of metamorphosed Neoproterozoic sedimentary rocks that outcrop across the Central Highlands of Scotland, east of the Great Glen, as well as appearing in the north of Ireland. It is a subdivision of the Dalradian Supergroup and is itself divided into four units; from oldest to youngest these are the Islay, Easdale, Crinan and Tayvallich subgroups. Islay Subgroup The lower boundary of the Islay Subgroup and hence the Argyll Group as a whole is defined at the base of the Port Askaig tillite, a diamictite which displays limestone clasts overlain by quartzite and granite clasts. The tillite is thickest in its type area and on the Garvellachs. The Schiehallion Boulder Bed of the eastern Grampians correlates with this tillite. The tillite is overlain by the Bonahaven Dolomite and then the Jura Quartzite which can reach up to 5 km thick but which is more typically between 500 and 1000m thick. Psammites and pelites occur within the sequence in t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metasedimentary Rock
In geology, metasedimentary rock is a type of metamorphic rock. Such a rock was first formed through the deposition and solidification of sediment Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand an .... Then, the rock was buried underneath subsequent rock and was subjected to high pressures and temperatures, causing the rock to recrystallize. The overall composition of a metasedimentary rock can be used to identify the original sedimentary rock, even where they have been subject to high-grade metamorphism and intense deformation. Types of metasedimentary rocks See also * References Metamorphic petrology {{petrology-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
