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Brother Isle
Brother Isle ( non, breiðare øy meaning broad beach island) is a small, uninhabited island in Shetland, Scotland. It lies between the islands of Yell and Shetland Mainland. It is in size. Geography and geology The island's rock is "undifferentiated moine gneiss and quartzite." History It is sometimes assumed that the "Brother" in the name refers to Culdees/''papar The Papar (; from Latin ''papa'', via Old Irish, meaning "father" or "pope") were, according to early Icelandic sagas, Irish monks who took eremitic residence in parts of what is now Iceland before that island's habitation by the Norsemen of S ...'' who were frequent inhabitants of the smaller islands, however, in this case there is no apparent evidence for this claim, and it would appear to be merely folk etymology. At only 40 hectares in size (about 1/6 of a sq. mile) and surrounded by tidal rips which make landing difficult, it would seem unlikely that the island has ever been inhabited. However, ...
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El Nido, Palawan
El Nido, officially the Municipality of El Nido ( cyo, Banwa i'ang El Nido, tgl, Bayan ng El Nido), is a 1st class municipality of the Philippines, municipality in the Philippine Province, province of Palawan, Philippines. According to the 2020 census, it has a population of 50,494 people. It is about south-west of Manila, and about north-east of Puerto Princesa, capital of Palawan. A Protected area, managed resource protected area,Destination: El Nido
Accessed 24, 2008.
it is known for its white-sand beaches, coral reefs, and limestone cliffs, as well as for being the gateway to the Bacuit archipelago.


History

El Nido has been inhabited by humans since early 2680 BC, or even up to 22,000 years ago. This was confirmed by the fossils and burial sites, dating back to the Neolithic, Lat ...
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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 ...
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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 ...
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Scotland
Scotland (, ) is a country that is part of the United Kingdom. Covering the northern third of the island of Great Britain, mainland Scotland has a border with England to the southeast and is otherwise surrounded by the Atlantic Ocean to the north and west, the North Sea to the northeast and east, and the Irish Sea to the south. It also contains more than 790 islands, principally in the archipelagos of the Hebrides and the Northern Isles. Most of the population, including the capital Edinburgh, is concentrated in the Central Belt—the plain between the Scottish Highlands and the Southern Uplands—in the Scottish Lowlands. Scotland is divided into 32 administrative subdivisions or local authorities, known as council areas. Glasgow City is the largest council area in terms of population, with Highland being the largest in terms of area. Limited self-governing power, covering matters such as education, social services and roads and transportation, is devolved from the Scott ...
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Yell, Shetland
Yell ( sco, Yell) is one of the North Isles of Shetland, Scotland. In the 2011 census it had a usually resident population of 966. It is the second largest island in Shetland after the Mainland with an area of ,Penrith, James & Deborah (2007) ''Orkney & Shetland'' (part of ''The Scottish Islands'' series). Richmond. Crimson Publishing. and is the third most populous in the archipelago (fifteenth out of the islands in Scotland), after the Mainland and Whalsay. The island's bedrock is largely composed of Moine schist with a north–south grain, which was uplifted during the Caledonian mountain building period. Peat covers two-thirds of the island to an average depth of . Yell has been inhabited since the Neolithic times, and a dozen broch sites have been identified from the pre-Norse period. Norse rule lasted from the 9th to 14th centuries until Scottish control was asserted. The modern economy of the island is based on crofting, fishing, transport and tourism. The island claim ...
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Moine Supergroup
The Moine Supergroup is a sequence of Neoproterozoic metamorphic rocks that form the dominant outcrop of the Scottish Highlands between the Moine Thrust Belt to the northwest and the Great Glen Fault to the southeast. The sequence is metasedimentary in nature and was metamorphosed and deformed in a series of tectonic events during the Late Proterozoic and Early Paleozoic. It takes its name from ''A' Mhòine'', a peat bog in northern Sutherland. Distribution The main outcrop of the Moine series lies northwest of the Great Glen Fault, structurally above the Moine Thrust to the west forming what is known as the Northern Highlands Terrane. A smaller area of similar rocks that are correlated with these, outcrop within the 'Grampian Terrane' to the southeast of the Great Glen. Moinian rocks are also recognised on Mull, Orkney and Shetland. Stratigraphy The Moine Supergroup has been subdivided into different groups or divisions. The relationship between individual groups in terms of ag ...
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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 ...
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Quartzite
Quartzite is a hard, non- foliated metamorphic rock which 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. 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 resistant hilltops. The nearly pure silica conte ...
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Culdee
The Culdees ( ga, Céilí Dé,  "Spouses of God") were members of ascetic Christian monastic and eremitical communities of Ireland, Scotland, Wales and England in the Middle Ages. Appearing first in Ireland and subsequently in Scotland, attached to cathedral or collegiate churches, they lived in monastic fashion though not taking monastic vows.D'Alton, Edward Alfred (1908). "Culdees". In ''Catholic Encyclopedia''. 4. New York: Robert Appleton Company. Etymology According to the Swiss theologian Philip Schaff, the term Culdee or Ceile De, or Kaledei, first appeared in the 8th century. While "giving rise to much controversy and untenable theories", it probably means servants or worshippers of God. The term was applied to anchorites, who, in entire seclusion from society, sought the perfection of sanctity. They afterward associated themselves into communities of hermits and were finally brought under canonical rule along with the secular clergy. It was at the time the name Culdee ...
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Papar
The Papar (; from Latin ''papa'', via Old Irish, meaning "father" or "pope") were, according to early Icelandic sagas, Irish monks who took eremitic residence in parts of what is now Iceland before that island's habitation by the Norsemen of Scandinavia, as evidenced by the sagas and recent archaeological findings. Origins The first Norsemen began settling in Iceland in 874 CE. The oldest Scandinavian source mentioning the existence of the Papar, however, the ''Íslendingabók'' ("Book of the Icelanders") by Icelandic chronicler Ari Þorgilsson, was written between 1122 and 1133, some time after the event. Ari writes of "Christian men", titled the 'Papar' by the Norsemen, who departed the isle because of their dislike of the 'heathen' Norse, pointing to the possibility of the Papar having arrived before the Norse. An earlier source that could possibly refer to the Papar is the work of Dicuil, an early 9th-century Irish monk and geographer, which included mention of the wa ...
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Folk Etymology
Folk etymology (also known as popular etymology, analogical reformation, reanalysis, morphological reanalysis or etymological reinterpretation) is a change in a word or phrase resulting from the replacement of an unfamiliar form by a more familiar one. The form or the meaning of an archaic, foreign, or otherwise unfamiliar word is reinterpreted as resembling more familiar words or morphemes. The term ''folk etymology'' is a loan translation from German language, German ''Volksetymologie'', coined by Ernst Förstemann in 1852. Folk etymology is a Productivity (linguistics), productive process in historical linguistics, language change, and social relation, social interaction. Reanalysis of a word's history or original form can affect its spelling, pronunciation, or meaning. This is frequently seen in relation to loanwords or words that have become archaic or obsolete. Examples of words created or changed through folk etymology include the English dialectal form wikt:sparrowgrass ...
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Rip Current
A rip current, often simply called a rip (or misleadingly a ''rip tide''), is a specific kind of water current that can occur near beaches with breaking waves. A rip is a strong, localized, and narrow current of water which moves directly away from the shore, cutting through the lines of breaking waves like a river running out to sea. The current in a rip is strongest and fastest next to the surface of the water. Rip currents can be hazardous to people in the water. Swimmers who are caught in a rip current and who do not understand what is happening, or who may not have the necessary water skills, may panic, or they may exhaust themselves by trying to swim directly against the flow of water. Because of these factors, rip currents are the leading cause of rescues by lifeguards at beaches, and in the United States, they are the cause of an average of 46 deaths by drowning per year. A rip current is not the same thing as undertow, although some people use the term incorrectly whe ...
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