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Little Sugar Loaf
Little Sugar Loaf () is a hill in the far northeastern sector of the Wicklow Mountains in Ireland. It does not have the elevation to rank on Arderin, Hewitt, or Vandeleur-Lynam scales,Mountainviews, (September 2013), "A Guide to Ireland's Mountain Summits: The Vandeleur-Lynams & the Arderins", Collins Books, Cork, however, its prominence of ranks it as a Marilyn. The Little Sugar Loaf is situated northeastwards from the Great Sugar Loaf, but separated by the N11 dual carriageway. The northern side of Little Sugar Loaf directly overlooks the town of Bray; the eastern side (see photo) looks across the R761 between Bray and Greystones to the western slope of Bray Head. Little Sugar Loaf has a distinctive profile of a rocky double summit. Like the Great Sugar Loaf, it consists of Cambrian Period quartzite bedrock. Irish academic Paul Tempan notes that the Irish name ''Giolspar'' is likely a translation of the English "gilt spur", based on a record of a 12th-century ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Irish Language
Irish ( Standard Irish: ), also known as Gaelic, is a Goidelic language of the Insular Celtic branch of the Celtic language family, which is a part of the Indo-European language family. Irish is indigenous to the island of Ireland and was the population's first language until the 19th century, when English gradually became dominant, particularly in the last decades of the century. Irish is still spoken as a first language in a small number of areas of certain counties such as Cork, Donegal, Galway, and Kerry, as well as smaller areas of counties Mayo, Meath, and Waterford. It is also spoken by a larger group of habitual but non-traditional speakers, mostly in urban areas where the majority are second-language speakers. Daily users in Ireland outside the education system number around 73,000 (1.5%), and the total number of persons (aged 3 and over) who claimed they could speak Irish in April 2016 was 1,761,420, representing 39.8% of respondents. For most of recorded ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greystones
Greystones () is a coastal town and seaside resort in County Wicklow, Ireland. It lies on Ireland's east coast, south of Bray, County Wicklow, Bray and south of Dublin city centre and has a population of 18,140 (2016). The town is bordered by the Irish Sea to the east, Bray Head to the north and the Wicklow Mountains to the west. It is the second biggest town in County Wicklow (after Bray, County Wicklow, Bray). The town was named after a half-mile or one-kilometre stretch of grey stones between two beaches on the seafront. The harbour area and Greystones railway station are at the northern and southern ends respectively. The North Beach, which begins at the harbour, is a stony beach, and some of its length is overlooked by the southern cliffs of Bray Head, which are subject to erosion. The South Beach is a broad sandy beach about one kilometre long. It is a Blue Flag beach and receives many visitors and tourists, mainly in the summer. In 2008, Greystones was named as the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marilyns Of Ireland
This is a list of Marilyn hills and mountains in the United Kingdom, Isle of Man and Ireland by height. Marilyns are defined as peaks with a prominence of or more, regardless of height or any other merit (e.g. topographic isolation, as used in Munros). Thus, Marilyns can be mountains, with a height above , or relatively small hills. there were 2,011 recorded Marilyns. Definition The Marilyn classification was created by Alan Dawson in his 1992 book ''The Relative Hills of Britain''. The name Marilyn was coined by Dawson as a punning contrast to the ''Munro'' classification of Scottish mountains above , but which has no explicit prominence threshold, being homophonous with (Marilyn) '' Monroe''. The list of Marilyns was extended to Ireland by Clem Clements. Marilyn was the first of several subsequent British Isles classifications that rely solely on prominence, including the P600s, the HuMPs, and the TuMPs. Topographic prominence is a more difficult to estimate than t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
DoBIH
The mountains and hills of the British Isles are categorised into various lists based on different combinations of elevation, prominence, and other criteria such as isolation. These lists are used for peak bagging, whereby hillwalkers attempt to reach all the summits on a given list, the oldest being the 282 Munros in Scotland, created in 1891. A height above 2,000 ft, or more latterly 610 m, is considered necessary to be classified as a mountain – as opposed to a hill – in the British Isles. With the exception of Munros, all the lists require a prominence above . A prominence of between (e.g. some Nuttalls and Vandeleur-Lynams), does not meet the International Climbing and Mountaineering Federation (UIAA) definition of an "independent peak", which is a threshold over . Most lists consider a prominence between as a "top" (e.g. many Hewitts and Simms). Marilyns, meanwhile, have a prominence above , with no additional height threshold. They range from small hills to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Marilyns In The British Isles
This is a list of Marilyn hills and mountains in the United Kingdom, Isle of Man and Ireland by height. Marilyns are defined as peaks with a prominence of or more, regardless of height or any other merit (e.g. topographic isolation, as used in Munros). Thus, Marilyns can be mountains, with a height above , or relatively small hills. there were 2,011 recorded Marilyns. Definition The Marilyn classification was created by Alan Dawson in his 1992 book ''The Relative Hills of Britain''. The name Marilyn was coined by Dawson as a punning contrast to the ''Munro'' classification of Scottish mountains above , but which has no explicit prominence threshold, being homophonous with (Marilyn) '' Monroe''. The list of Marilyns was extended to Ireland by Clem Clements. Marilyn was the first of several subsequent British Isles classifications that rely solely on prominence, including the P600s, the HuMPs, and the TuMPs. Topographic prominence is a more difficult to estimate than t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains Of The British Isles By Height
This is a list of mountains in Britain and Ireland by height and by prominence. Height and prominence are the most important metrics for the classifications of mountains by the UIAA; with isolation a distant third criterion. The list is sourced from the ''Database of British and Irish Hills'' ("DoBIH") for peaks that meet the consensus height threshold for a mountain, namely ; the list also rules out peaks with a prominence below and thus, the list is therefore precisely a list of the 2,756 Simms in the British Isles (as at October 2022). Many classifications of mountains in the British Isles consider a prominence between as being a "top", and not a mountain; however, using the prominence threshold gives the broadest possible list of mountains. For a ranking of mountains with a higher prominence threshold use: * List of Marilyns in the British Isles, for ranking by height and by prominence, of peaks with prominence over ; or * List of P600 mountains in the British Isles, for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diarmait Mac Murchada
Diarmait Mac Murchada (Modern Irish: Diarmaid Mac Murchadha), anglicised as Dermot MacMurrough, Dermod MacMurrough, or Dermot MacMorrogh (c. 1110 – c. 1 May 1171), was a King of Leinster in Ireland. In 1167, he was deposed by the High King of Ireland, Ruaidrí Ua Conchobair (Rory O'Connor). The grounds for the deposition were that Mac Murchada had, in 1152, abducted Derbforgaill, the wife of the king of Breifne, Tiernan O'Rourke ( ga, Tighearnán Ua Ruairc). To recover his kingdom, Mac Murchada solicited help from King Henry II of England. His issue unresolved, he gained the military support of the 2nd Earl of Pembroke (Richard de Clare, nicknamed "Strongbow"). At that time, Strongbow was in opposition to Henry II due to his support for Stephen, King of England against Henry's mother in the Anarchy. In exchange for his aid, Strongbow was promised in marriage to Mac Murchada's daughter Aoife with the right to succeed to the Kingship of Leinster. Henry II then mounted a la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Irish Mountaineering Club
The Irish Mountaineering Club (in Irish language, Irish, ''Cumann Sléibhteoireachta na hÉireann'', usually called "The IMC") is a mountaineering club whose activities include climbing. The club has over 200 members. History The IMC was founded in 1942 by Bill Perrott and a group of other climbers in south Dublin, within easy reach of Dalkey Quarry. They established several climbs in Dalkey and at other locations around Dublin such as The Scalp, Bray Head, and Ireland's Eye; these were the first steps in the development of climbing in Ireland. This group, now known as "The Old IMC", disbanded in 1944. In 1948, the IMC was revived on a more formal basis by Perrott, Joss Lynam, and others, with the intention that it become a national club drawing its membership from all around Ireland, with local branches in the major cities. The first president was the naturalist Robert Lloyd Praeger. During the 1950s branches of the IMC were established in Dublin and Belfast, and one for the "Fl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cambrian
The Cambrian Period ( ; sometimes symbolized C with bar, Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ago (mya) to the beginning of the Ordovician Period mya. Its subdivisions, and its base, are somewhat in flux. The period was established as "Cambrian series" by Adam Sedgwick, who named it after Cambria, the Latin name for 'Cymru' (Wales), where Britain's Cambrian rocks are best exposed. Sedgwick identified the layer as part of his task, along with Roderick Murchison, to subdivide the large "Transition Series", although the two geologists disagreed for a while on the appropriate categorization. The Cambrian is unique in its unusually high proportion of sedimentary deposits, sites of exceptional preservation where "soft" parts of organisms are preserved as well as their more resistant shells. As a result, our understanding of the Ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Double Summit
A double summit, double peak, twin summit, or twin peak refers to a mountain or hill that has two summits, separated by a col or saddle. One well-known double summit is Austria’s highest mountain, the Großglockner, where the main summit of the Großglockner is separated from that of the Kleinglockner by the Glocknerscharte col in the area of a geological fault. Other double summits have resulted from geological folding. For example, on Mont Withrow in British Columbia, resistant sandstones form the limbs of the double summit, whilst the softer rock in the core of the fold was eroded.{{cite web , url=http://gsc.nrcan.gc.ca/natmap/cf/intro_e.php , title=Mt. Withrow syncline , archive-url=https://web.archive.org/web/20060404185911/http://gsc.nrcan.gc.ca/natmap/cf/intro_e.php , archive-date=2006-04-04 , access-date=2009-05-12 Triple peaks occur more rarely; one example is the Rosengartenspitze in the Dolomites. The Illimani in Bolivia is an example of a rare quadruple summit. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
