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Twelve Bens
, photo=Boats and mountains, Roundstone (6047965086).jpg , photo_caption= View of the range from Roundstone village. , region = Connacht , region_type = Provinces of Ireland , translation = The peaks of Beola , language = Irish language , location = Connemara, County Galway, Ireland , border= , length_km= , length_orientation= , width_km= , width_orientation= , area_km2 = 161.3 , highest= Benbaun , elevation_m= 729 , elevation_ref = , coordinates = , range_coordinates = , geology=quartzites, grits, graphitic , period=Precambrian-Cambrian , map= Ireland , map_caption=Location of the Twelve Bens , topo = OSI ''Discovery'' 37, 44 , normal_route = ) * "Twelve Bens Challenge" The Twelve Bens or Twelve Pins, also called the Benna Beola (), is a mountain range of mostly sharp-peaked quartzite summits and ridges in the Connemara National Park in County Galway, in the west of Ireland. The widest definition of the range includes the Garraun Complex to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roundstone, County Galway
Roundstone () is a village on the west coast of Ireland, in the Connemara region of County Galway. Lying opposite the island of Inishnee on Roundstone Bay, by road it is northwest of Galway and southeast of Clifden. Known as a haven for people in the creative arts, it hosts an annual regatta in July. Etymology The anglicised name is usually considered an error on the part of the British colonial Ordnance Survey, which translated the village name; while ''Cloch'' certainly means "stone" or "rock", ''Rón'' means "seal", not "round". Still, the names Cloch na Rón and Roundstone may be totally independent. The bay is referred to as Round-stone Haven as early as 1684 (Roderick O'Flaherty), and the rock after which it is named stands like a marker at the entrance and is strikingly round. History The area to the north of Roundstone was occupied by the O'Flaherty family, who built a Dominican Priory about to the north of what is now Roundstone in the 15th century. Roundstone was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Garraun (Galway)
Garraun () at , is the 224th–highest peak in Ireland on the Arderin scale, however, while it is just short of the elevation threshold of 600-metres for other classifications (e.g. Vandeleur-Lynam, and Hewitt), it does have the prominence to be a Marilyn.Mountainviews, (September 2013), "A Guide to Ireland's Mountain Summits: The Vandeleur-Lynams & the Arderins", Collins Books, Cork, Garraun lies on an isolated massif near the mouth of Killary Harbour at the far north sector of the Twelve Bens/Garraun Complex Special Area of Conservation in the Connemara National Park in Galway. The southern slopes are a scenic backdrop to Kylemore Abbey and Kylemore Lough. Naming Irish academic Paul Tempan notes that Garraun is clearly a name of Irish origin, either from ga, garrán, meaning "grove", or more likely from ga, géarán, meaning "fang"; while the summit is flat, the eastern ridge leading to it is sharp enough to have merited such a name. Tim Robinson notes that ga, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Topographic Elevation
The elevation of a geographic location is its height above or below a fixed reference point, most commonly a reference geoid, a mathematical model of the Earth's sea level as an equipotential gravitational surface (see Geodetic datum § Vertical datum). The term ''elevation'' is mainly used when referring to points on the Earth's surface, while ''altitude'' or ''geopotential height'' is used for points above the surface, such as an aircraft in flight or a spacecraft in orbit, and '' depth'' is used for points below the surface. Elevation is not to be confused with the distance from the center of the Earth. Due to the equatorial bulge, the summits of Mount Everest and Chimborazo have, respectively, the largest elevation and the largest geocentric distance. Aviation In aviation the term elevation or aerodrome elevation is defined by the ICAO as the highest point of the landing area. It is often measured in feet and can be found in approach charts of the aerodrome. It ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ruaidhrí Ó Flaithbheartaigh
Roderick O'Flaherty ( ga, Ruaidhrí Ó Flaithbheartaigh; 1629–1718 or 1716) was an Irish historian. Biography He was born in County Galway and inherited Moycullen Castle and estate. O'Flaherty was the last ''de jure'' Lord of Iar Connacht, and the last recognised Chief of the Name of Clan O'Flaherty. He lost the greater part of his ancestral estates to Cromwellian confiscations in the 1650s. The remainder was stolen through deception, by his son's Anglo-Irish father-in-law, Richard ''Nimble Dick'' Martin of Ross. As Martin had given service to some captured Williamite officers he was allowed to keep his lands. It was therefore arranged that to protect them from confiscation 200,000 acres of Connemara lands held by O'Flahertys, Joyces, Lees and others were transferred into Martin's name with the trust they would be returned. However, Martin betrayed his former friends and neighbours and kept all of their lands. Uniquely among the O'Flaherty family up to that time, Rode ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
MountainViews
In these lists of mountains in Ireland, those within Northern Ireland, or on the Republic of Ireland – United Kingdom border, are marked with an asterisk, while the rest are within the Republic of Ireland. Where mountains are ranked by height, the definition of the topographical prominence used to classify the mountain (e.g. the change in elevation required between neighbouring mountains), is noted. In British definitions, a height of is required for a mountain, whereas in Ireland, a lower threshold of is sometimes advocated. The lowest minimum prominence threshold of any definition of an Irish mountain is (e.g. the Vandeleur-Lynam), however most definitions, including the International Climbing and Mountaineering Federation (UIAA) criteria, do not consider prominences below as being mountains (e.g. must at least be an Arderin or a Hewitt). Many British definitions consider a peak with a prominence below , as being a ''top'', and not a mountain (e.g. must be a Maril ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ordnance Survey Ireland
Ordnance Survey Ireland (OSI; ga, Suirbhéireacht Ordanáis Éireann) is the national mapping agency of Ireland. It was established on 4 March 2002 as a body corporate. It is the successor to the former Ordnance Survey of Ireland. It and the Ordnance Survey of Northern Ireland (OSNI) are the ultimate successors to the Irish operations of the British Ordnance Survey. OSI is part of the Irish public service. OSI has made modern and historic maps of the state free to view on its website. OSI is headquartered at Mountjoy House in the Phoenix Park in Dublin. Mountjoy House was also the headquarters, until 1922, of the Irish section of the British Ordnance Survey. Organisation Under the Ordnance Survey Ireland Act 2001, the Ordnance Survey of Ireland was dissolved and a new corporate body called Ordnance Survey Ireland was established in its place. OSI is now an autonomous corporate body, with a remit to cover its costs of operation from its sales of data and derived products, w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Queen's University Belfast
, mottoeng = For so much, what shall we give back? , top_free_label = , top_free = , top_free_label1 = , top_free1 = , top_free_label2 = , top_free2 = , established = , closed = , type = Public research university , parent = , affiliation = , religious_affiliation = , academic_affiliation = , endowment = £70.0 million , budget = £395.8 million , rector = , officer_in_charge = , chairman = , chairperson = , chancellor = Hillary Clinton , president = , vice-president = , superintendent = , vice_chancellor = Ian Greer , provost = , principal = , dean = , director = , head_label = , head = , academic_staff = 2,414 , administrative_staff = 1,489 , students = () , undergrad = () , postgrad = () , doctoral = , other = 2,250 (Colleges) , address = , city = Belfast , state = , province = , postalcode = , country = Northern Ireland , campus = Urban , language = , free_label = Newspaper , free = '' The G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anglicized
Anglicisation is the process by which a place or person becomes influenced by English culture or British culture, or a process of cultural and/or linguistic change in which something non-English becomes English. It can also refer to the influence of English culture and business on other countries outside England or the United Kingdom, including their media, cuisine, popular culture, technology, business practices, laws, or political systems. Linguistic anglicisation is the practice of modifying foreign words, names, and phrases to make them easier to spell, pronounce or understand in English. The term commonly refers to the respelling of foreign words, often to a more drastic degree than that implied in, for example, romanisation. One instance is the word "dandelion", modified from the French ''dent-de-lion'' ("lion's tooth", a reference to the plant's sharply indented leaves). The term can also refer to phonological adaptation without spelling change: ''spaghetti'', for example ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dalradian
The Dalradian Supergroup (informally and traditionally the Dalradian) is a stratigraphic unit (a sequence of rock strata) in the lithostratigraphy of the Grampian Highlands of Scotland and in the north and west of Ireland. The diverse assemblage of rocks which constitute the supergroup extend across Scotland from Islay in the west to Fraserburgh in the east and are confined by the Great Glen Fault to the northwest and the Highland Boundary Fault to the southeast. Much of Shetland east of the Walls Boundary Fault is also formed from Dalradian rocks. Dalradian rocks extend across the north of Ireland from County Antrim in the north east to Clifden on the Atlantic coast, although obscured by later Palaeogene lavas and tuffs or Carboniferous rocks in large sections. Historical The land to the southeast of the Great Glen was the old Celtic region of Dál Riata (Dalriada), and in 1891 Archibald Geikie proposed the name Dalradian as a convenient provisional designation for the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schists
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 reflects a high content of platy minerals, such as micas, talc, 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 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 usually given a name reflecting its protolith, such as ''schistose me ... [...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 co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metamorphic
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and distor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
