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South Havra
South Havra ( sco, Sooth Haevra; non, Hafrey), formerly Hevera, is an uninhabited island in the Scalloway Islands, Shetland, Scotland. Geography and geology South Havra lies south of Burra and west of the southern peninsula of the Mainland. The island's rock is "epidiotic syenite with undifferentiated schist and gneiss." The soil is fairly fertile, but the lack of running water meant that, unusually for Shetland, the islanders resorted to building a windmill to grind corn. Geological features on the island include caves and natural arches. Little Havra is to its west. History Olaf Sinclair, foud (a kind of magistrate) of all Shetland lived here in the 16th century. The island's ruined windmill is an unusual sight in the Shetland Islands, especially as some have pointed out, that the Dutch Dutch commonly refers to: * Something of, from, or related to the Netherlands * Dutch people () * Dutch language () Dutch may also refer to: Places * Dutch, West Virginia, a comm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mainland, Shetland
The Mainland is the main island of Shetland, Scotland. The island contains Shetland's only burgh, Lerwick, and is the centre of Shetland's ferry and air connections. Geography It has an area of , making it the third-largest Scottish island and the fifth largest of the British Isles after Great Britain, Ireland, Lewis and Harris and Skye. Mainland is the second most populous of the Scottish islands (only surpassed by Lewis and Harris), and had 18,765 residents in 2011 compared to 17,550 in 2001. The mainland can be broadly divided into four sections: *The long southern peninsula, south of Lerwick, has a mixture of moorland and farmland and contains many important archaeological sites. **Bigton, Cunningsburgh, Sandwick, Scalloway, and Sumburgh *The Central Mainland has more farmland and some woodland plantations. *The West Mainland **Aith, Walls, and Sandness *The North Mainland – in particular the large Northmavine peninsula, connected to Mainland by a narrow isthmus at ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uninhabited Islands Of Shetland
The list of uninhabited regions includes a number of places around the globe. The list changes year over year as human beings migrate into formerly uninhabited regions, or migrate out of formerly inhabited regions. List As a group, the list of uninhabited places are called the "nonecumene". This is a special geography term which means the uninhabited area of the world. * Virtually all of the Ocean *Virtually all of Antarctica *Most of The Arctic *Most of Greenland *Most of The Sahara * Antipodes Islands * Ashmore and Cartier Islands * Bajo Nuevo Bank * Baker Island * Ball's Pyramid * Balleny Islands * Big Major Cay * Bouvet Island * Much of the interior of Brazil * Caroline Island * Clipperton Island * The semi-arid regions and deserts of Australia * Devon Island * Much of Eastern Oregon * Elephant Island * Elobey Chico * Ernst Thälmann Island * Much of Fiordland, New Zealand * Goa Island * Gough Island * Hans Island * Harmil * Hashima Island * Hatutu * Heard Island and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dutch People
The Dutch (Dutch: ) are an ethnic group and nation native to the Netherlands. They share a common history and culture and speak the Dutch language. Dutch people and their descendants are found in migrant communities worldwide, notably in Aruba, Suriname, Guyana, Curaçao, Argentina, Brazil, Canada,Based on Statistics Canada, Canada 2001 Censusbr>Linkto Canadian statistics. Australia, South Africa, New Zealand and the United States.According tFactfinder.census.gov The Low Countries were situated around the border of France and the Holy Roman Empire, forming a part of their respective peripheries and the various territories of which they consisted had become virtually autonomous by the 13th century. Under the Habsburgs, the Netherlands were organised into a single administrative unit, and in the 16th and 17th centuries the Northern Netherlands gained independence from Spain as the Dutch Republic. The high degree of urbanization characteristic of Dutch society was attained at a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Olave Sinclair
Olave Sinclair of Havera (South Havra) and Brow (died 1573) was an official on Shetland, known as the "foud". He collected taxes due to the Scottish crown. His first name is sometimes written as Oliver, Ola, or Olaf. Battle of Summerdale Olave Sinclair was present at the battle of Summerdale in 1529 and in 1539 was given a respite (exemption from prosecution) for the death of John Sinclair, 3rd Earl of Caithness. Olave Sinclair was probably a close relative of Edward Sinclair of Strome, who was foud of Shetland in the 1530s. Feud with the MacLeod of Lewis Olave Sinclair is said to have been blind in one eye, the result of leaping from Sumburgh Head to escape a band of marauders from the Isle of Lewis. A version of the story explains that Sinclair had a quarrel with William MacLeod of Lewis, whose wife had brought him lands in Shetland. Two previous attempts by the MacLeods to seize Sinclair in revenge for William MacLeod's death were foiled by his Fair Isle allies. Sinclair was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Havra
Little Havra is a small island off the west of South Mainland in Shetland. It is at its highest point, upon which there is a cairn. It is located west of South Havra South Havra ( sco, Sooth Haevra; non, Hafrey), formerly Hevera, is an uninhabited island in the Scalloway Islands, Shetland, Scotland. Geography and geology South Havra lies south of Burra and west of the southern peninsula of the Mainland. .... References Shetlopedia Uninhabited islands of Shetland {{Shetland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural Arch
A natural arch, natural bridge, or (less commonly) rock arch is a natural landform where an arch has formed with an opening underneath. Natural arches commonly form where inland cliffs, coastal cliffs, fins or stacks are subject to erosion from the sea, rivers or weathering ( subaerial processes). Most natural arches are formed from narrow fins and sea stacks composed of sandstone or limestone with steep, often vertical, cliff faces. The formations become narrower due to erosion over geologic time scales. The softer rock stratum erodes away creating rock shelters, or alcoves, on opposite sides of the formation beneath the relatively harder stratum, or caprock, above it. The alcoves erode further into the formation eventually meeting underneath the harder caprock layer, thus creating an arch. The erosional processes exploit weaknesses in the softer rock layers making cracks larger and removing material more quickly than the caprock; however, the caprock itself continues to er ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schist
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture (geology), texture reflects a high content of platy minerals, such as micas, talc, chlorite group, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium Metamorphism#Metamorphic grades, grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is us ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shetland
Shetland, also called the Shetland Islands and formerly Zetland, is a subarctic archipelago in Scotland lying between Orkney, the Faroe Islands and Norway. It is the northernmost region of the United Kingdom. The islands lie about to the northeast of Orkney, from mainland Scotland and west of Norway. They form part of the border between the Atlantic Ocean to the west and the North Sea to the east. Their total area is ,Shetland Islands Council (2012) p. 4 and the population totalled 22,920 in 2019. The islands comprise the Shetland (Scottish Parliament constituency), Shetland constituency of the Scottish Parliament. The local authority, the Shetland Islands Council, is one of the 32 council areas of Scotland. The islands' administrative centre and only burgh is Lerwick, which has been the capital of Shetland since 1708, before which time the capital was Scalloway. The archipelago has an oceanic climate, complex geology, rugged coastline, and many low, rolling hills. The lar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Syenite
Syenite is a coarse-grained intrusive igneous rock with a general composition similar to that of granite, but deficient in quartz, which, if present at all, occurs in relatively small concentrations (< 5%). Some syenites contain larger proportions of components and smaller amounts of felsic material than most granites; those are classed as being of . The equivalent of syenite is |
Burra, Shetland
Burra (Old Norse: ''Barrey'' ) is the collective name for two of the Shetland Islands, West (pop. 753) and East Burra (pop. 66), which are connected by bridge to one another, and to the Shetland Mainland via Trondra. In addition, Burra was an ancient Civil parish that included smaller additional islands such as South Havra, Little Havra, Papa and the tidal island West Head of Papa. The civil parish of Burra was merged into the civil parish of Lerwick, along with Quarff and Gulberwick, in 1891. It continues to exist as Quoad sacra parish of the Church of Scotland. ''Collins Encyclopedia of Scotland'' suggests that the name is a corruption of "Borgarey" (island of the broch),Keay, J. & Keay, J. (1994) ''Collins Encyclopaedia of Scotland''. London. HarperCollins. and while this is unlikely, and no broch is extant, the place name Brough, on West Burra West Burra is one of the Scalloway Islands, a subgroup of the Shetland Islands in Scotland. It is connected by bridge to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
