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Twelve Bens
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 north as well as several isolated peaks to the west, and is designated a Special Area of Conservation. The highest point is Benbaun at . The range is a popular location for hill-walking activities with the 16–kilometre 8–9 hour Glencoaghan Horseshoe, considered one of the best ridge-walks in Ireland. Topographically, the range is partnered with the Maumturks range to the east of the Inagh valley (a Western Way route); and both share a common geology being largely composed of metamorphic marine rocks, being predominantly resistant quartzite but with deposits of schists in the valleys (known as ''Connemara Dalradian'' rocks). Naming "Ben" is an anglicized form of the Irish word ''binn'', meani ...
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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 ruled by the Chiefs of Clan O'Flaherty, who built a Dominican Priory about to the north of what is now Roundstone in the 15th-century. Rounds ...
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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 County 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 , meaning "grove", or more likely from , 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 , meaning "bald hill", ...
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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 aerodro ...
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Ruaidhrí Ó Flaithbheartaigh
Roderick O'Flaherty (; 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'' Tigerna, Lord of Iar Connacht, and the last recognised Chief of the Name of Irish clan, Clan O'Flaherty. He lost the greater part of his ancestral estates to Plantations of Ireland#Cromwellian land confiscation (1652), 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 from confiscation 200,000 acres of Connemara lands held by O'Flahertys, Joyces, Lees, and others that 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 th ...
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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 Lists of mountains and hills in the British Isles#Vandeleur-Lynams, 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 Lists of mountains and hills in the British Isles#Arderins, Arderin or a Lists of mounta ...
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Ordnance Survey Ireland
Ordnance Survey Ireland (OSI; ) was the national mapping agency of the Republic of Ireland. It was established on 4 March 2002 as a body corporate. It was the successor to the former Ordnance Survey of Ireland. It and the Ordnance Survey of Northern Ireland (OSNI) were themselves the successors to the Irish operations of the British Ordnance Survey. OSI was part of the Irish public service. OSI was headquartered at Mountjoy House in the Phoenix Park in Dublin, which had previously been the headquarters of the British Ordnance Survey in Ireland until 1922. In March 2023, the Ordnance Survey was dissolved and its functions transferred to a new body called Tailte Éireann, which also incorporates the Property Registration Authority and the Valuation Office. 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 was an autonomous corporate bo ...
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Queen's University Belfast
The Queen's University of Belfast, commonly known as Queen's University Belfast (; abbreviated Queen's or QUB), is a public research university in Belfast, Northern Ireland, United Kingdom. The university received its charter in 1845 as part of the Queen's University of Ireland and opened four years later, together with University of Galway (as ''Queen's College, Galway'') and University College Cork (as ''Queen's College, Cork''). Queen's offers approximately 300 academic degree programmes at various levels. The current president and Chancellor (education), vice-chancellor is Ian Greer (obstetrician), Ian Greer. The annual income of the institution for 2023–24 was £474.2 million, of which £105.2 million was from research grants and contracts, with an expenditure of £345.9 million. Queen's is a member of the Russell Group of research-intensive universities, the Association of Commonwealth Universities, the European University Association, Universities UK and ...
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Anglicized
Anglicisation or anglicization is a form of cultural assimilation whereby something non-English becomes assimilated into or influenced by the culture of England. It can be sociocultural, in which a non-English place adopts the English language or culture; institutional, in which institutions are influenced by those of England or the United Kingdom; or Anglicisation (linguistics), linguistic, in which a non-English term or name is altered due to the cultural influence of the English language.Bridge, Carl, and Fedorowich, Kent. ''The British World: Diaspora, Culture, and Identity'', 2003, p. 89. "Beyond gaps in our information about who or what was affected by anglicisation is the matter of understanding the process more fully in terms of agency, periodisation, and extent and limitations." It can also refer to the influence of English soft power, which includes media, cuisine, popular culture, technology, business practices, laws and political systems. Anglicisation first occurre ...
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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 younger 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 com ...
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Schists
Schist ( ) is a medium-grained metamorphic rock generally derived from fine-grained sedimentary rock, like shale. It shows pronounced ''schistosity'' (named for the rock). 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 mica, 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 ...
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Quartzite
Quartzite is a hard, non- foliated metamorphic rock that 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, and hence quartzite is a metasandstone. 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 resist ...
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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 distort ...
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