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Rostrevor Gaelic Footballers
Rostrevor () is a village and townland in County Down, Northern Ireland. It lies at the foot of Slieve Martin on the coast of Carlingford Lough, near Warrenpoint. The Kilbroney River flows through the village and Rostrevor Forest is nearby. It is within Newry, Mourne and Down District. Rostrevor had a population of 2,800 in the 2011 Census. This article contains quotations from this source, which is available under th Open Government Licence v3.0 © Crown copyright. Name The first part of the name "Rostrevor" comes from the Irish word ''ros'', meaning a wood or wooded headland. The second part of the name comes from Sir Edward Trevor from Denbighshire in Wales, who settled in the area in the early 17th century and was succeeded by his son Marcus Trevor, who later became Viscount Dungannon. Walter Harris, writing in 1744, mistakenly believed that the first part of the name came from Sir Edward Trevor's wife Rose, a daughter of Henry Ussher, Archbishop of Armagh. His etymo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
2011 United Kingdom Census
A census of the population of the United Kingdom is taken every ten years. The 2011 census was held in all countries of the UK on 27 March 2011. It was the first UK census which could be completed online via the Internet. The Office for National Statistics (ONS) is responsible for the census in England and Wales, the General Register Office for Scotland (GROS) is responsible for the census in Scotland, and the Northern Ireland Statistics and Research Agency (NISRA) is responsible for the census in Northern Ireland. The Office for National Statistics is the executive office of the UK Statistics Authority, a non-ministerial department formed in 2008 and which reports directly to Parliament. ONS is the UK Government's single largest statistical producer of independent statistics on the UK's economy and society, used to assist the planning and allocation of resources, policy-making and decision-making. ONS designs, manages and runs the census in England and Wales. In its capacity as t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edward Trevor
Sir Edward Trevor (c. 1580–1642) was the founder of the fortunes of the Trevor dynasty, a major family of Denbighshire. He was the son of Robert Trevor and Katherine ap Llewellyn. His first wife was Anne Balle, daughter of Nicholas Balle. While on military service in Ireland, in 1612 Edward Trevor married as his second wife Rose, a daughter of Henry Ussher, Archbishop of Armagh and his first wife Margaret Elliott, and acquired an estate in County Down which was renamed Rostrevor, incorporating his own name. He was knighted in 1617 and built the mansion of Brynkynallt on his estates at Chirk in 1619. Archbishop Ussher appointed him joint executor of his will in 1613, together with his brother-in-law Sir Elliott. In 1622 he was appointed High Sheriff of Denbighshire. In 1641 Trevor was captured and imprisoned by Irish rebels, and he died in captivity. Children His son Marcus Trevor was a soldier of the English Civil War and following the English Restoration of 1660 w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Giant (mythology)
In folklore, giants (from Ancient Greek: '' gigas'', cognate giga-) are beings of human-like appearance, but are at times prodigious in size and strength or bear an otherwise notable appearance. The word ''giant'' is first attested in 1297 from Robert of Gloucester's chronicle. It is derived from the ''Gigantes'' ( grc-gre, Γίγαντες) of Greek mythology. Fairy tales such as '' Jack the Giant Killer'' have formed the modern perception of giants as dimwitted ogres, sometimes said to eat humans, while other giants tend to eat the livestock. The antagonist in ''Jack and the Beanstalk'' is often described as a giant. In some more recent portrayals, like those of Jonathan Swift and Roald Dahl, some giants are both intelligent and friendly. Literary and cultural analysis Giants appear in the folklore of cultures worldwide as they represent a relatively simple concept. Representing the human body enlarged to the point of being monstrous, giants evoke terror and remind humans ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Last Glacial Maximum
The Last Glacial Maximum (LGM), also referred to as the Late Glacial Maximum, was the most recent time during the Last Glacial Period that ice sheets were at their greatest extent. Ice sheets covered much of Northern North America, Northern Europe, and Asia and profoundly affected Earth's climate by causing drought, desertification, and a large drop in sea levels. Based on changes in position of ice sheet margins dated via terrestrial cosmogenic nuclides and radiocarbon dating, growth of ice sheets commenced 33,000 years ago and maximum coverage was between 26,500 years and 19–20,000 years ago, when deglaciation commenced in the Northern Hemisphere, causing an abrupt rise in sea level. Decline of the West Antarctica ice sheet occurred between 14,000 and 15,000 years ago, consistent with evidence for another abrupt rise in the sea level about 14,500 years ago. Glacier fluctuations around the Strait of Magellan suggest the peak in glacial surface area was constrained to betwee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boulder
In geology, a boulder (or rarely bowlder) is a rock fragment with size greater than in diameter. Smaller pieces are called cobbles and pebbles. While a boulder may be small enough to move or roll manually, others are extremely massive. In common usage, a boulder is too large for a person to move. Smaller boulders are usually just called rocks or stones. The word ''boulder'' derives from ''boulder stone'', from the Middle English ''bulderston'' or Swedish ''bullersten''. Online Etymology Dictionary. Retrieved December 9, 2011, from Dictionary.com website. In places covered by s during s, s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cloughmore
Cloughmore or Cloghmore (), known locally as "The Big Stone", is a huge granite boulder perched on a mountainside almost above the village of Rostrevor, County Down, Northern Ireland. It sits on the slopes of Slieve Martin in Kilbroney Park, overlooking Rostrevor Forest, Carlingford Lough and the Cooley Peninsula. It is popular destination for visitors, and is part of a National Nature Reserve and Area of Special Scientific Interest. The granite boulder, which has a calculated mass of 50 tonnes, is a glacial erratic, thought to have been transported from Scotland (from an island in Strathclyde bay) and deposited about 10,000 years ago by retreating ice during the last Ice Age. It sits on a relatively flat area of Silurian metasedimentary rock. Local legend has it that the stone was thrown from the Cooley Mountains, on the other side of Carlingford Lough, by the giant Fionn mac Cumhaill Fionn mac Cumhaill ( ; Old and mga, Find or ''mac Cumail'' or ''mac Umaill''), of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iveagh
Iveagh ( ; ) is the name of several historical territorial divisions in what is now County Down, Northern Ireland. Originally it was a Gaelic Irish territory, ruled by the ''Uí Echach Cobo'' and part of the overkingdom of Ulaid. From the 12th century the Magennises (''Mag Aonghusa'') were chiefs of Iveagh. They were based at Rathfriland and were inaugurated at Knock Iveagh. Following the Nine Years' War, the rulers of Iveagh submitted to the English Crown and the territory was divided between them. Iveagh became a barony, which was later split into Iveagh Lower and Iveagh Upper. The territory of Iveagh was also the basis of the Roman Catholic Diocese of Dromore. Uí Echach Cobo Iveagh derives its name from the Cruithin tribe ''Uí Echach'' (modern Irish: ''Uíbh Eachach''), or "descendants of Echu", and referred to an ancient Irish túath (district). It is also known more fully as ''Uí Echach Cobo'' (modern Irish: ''Uíbh Eachach Cobha'', meaning Echu of Cobo), and equivalent w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Magennis
Magennis ( ga, Mac Aonghusa), also spelled Maguiness, Maginnis, Magenis, McGinnis, or McGuinness, is an Celtic_onomastics#Surnames, Irish surname, meaning the "son of Angus", which in eastern Ulster was commonly pronounced in Irish as ''Mac Aonghusa''. A prominent branch of the ''Uíbh Eachach Cobha'', the Magennises would become chiefs of the territory of Iveagh, which by the 16th century comprised over half of modern County Down, Northern Ireland. By the end of the 17th century, their territory had been divided up between them, the McCartan chiefs and British prospectors. The four main branches of the Magennis clan were: Castlewellan, Corgary, Kilwarlin, and Rathfriland, between whom there was some rivalry. The ''Mac Artáin'' McCartan chiefs of Kinelarty, descend from the same genealogical line as the Magennis clan, through ''Artán'', the son of ''Faghártagh'', the son of ''Mongán'' Mac Aonghusa. Early history The Magennis clan were a sept of the ''Ui hAitidhe'', and desce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Archbishop Of Armagh
In Christian denominations, an archbishop is a bishop of higher rank or office. In most cases, such as the Catholic Church, there are many archbishops who either have jurisdiction over an ecclesiastical province in addition to their own archdiocese ( with some exceptions), or are otherwise granted a titular archbishopric. In others, such as the Lutheran Church of Sweden and the Church of England, the title is borne by the leader of the denomination. Etymology The word archbishop () comes via the Latin ''archiepiscopus.'' This in turn comes from the Greek , which has as components the etymons -, meaning 'chief', , 'over', and , 'seer'. Early history The earliest appearance of neither the title nor the role can be traced. The title of "metropolitan" was apparently well known by the 4th century, when there are references in the canons of the First Council of Nicæa of 325 and Council of Antioch of 341, though the term seems to be used generally for all higher ranks of bishop, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Henry Ussher
Henry Ussher (1550 – 2 April 1613) was an Irish Protestant churchman, a founder of Trinity College, Dublin, and Church of Ireland Archbishop of Armagh. Life The second of five sons of Thomas Ussher by Margaret (d. January 1597), daughter of Henry Geydon, alderman of Dublin, he was born in Dublin about 1550. Ambrose Ussher and James Ussher, sons of his brother Arnold, were his nephews, while his sister Rose married John Garvey, his predecessor as Archbishop. Henry Ussher entered at Magdalene College, Cambridge, matriculating on 2 May 1567, and graduating B. A. in the first quarter of 1570. His studies continued at Paris and at Oxford, where he entered University College, was incorporated B.A. 1 July 1572, and graduated M.A. 11 July 1572. His first preferment was the treasurership of Christ Church, Dublin (1573); on 12 March 1580 he was made archdeacon of Dublin by Adam Loftus, with whom he was connected by marriage. The project of converting St. Patrick's Cathedral, Dublin int ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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