Leenaun Hill
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Leenaun Hill
, photo = File:View north to Leenaun Hill from Letterbreckaun.jpg , photo_caption = View north to Leenaun Hill from Letterbreckaun , photo_size = , elevation_m = 618 , elevation_ref = , prominence_m = 363 , prominence_ref = , listing = Marilyn, Hewitt, Arderin, Simm, Vandeleur-Lynam , translation = Black knoll , language = Irish , location = Leenaun, Galway, Ireland , range = Maumturks , coordinates = , coordinates_ref = , map = island of Ireland , map_relief = yes , map_caption = Location in Ireland , grid_ref_Ireland = L8743259343 , topo = OSi ''Discovery'' 37 , geology = Siltstone & sandstone Bedrock , easiest_route = Via Leenaun village Leenaun Hill () at , is the 201st–highest peak in Ireland on the Arderin scale, and the 243rd–highest peak on the Vandeleur-Lynam scale.Mountainviews, (September 2013), "A Guide to Ireland's Mountain Summits: The Vandeleur-Lynams & the Arderins", Collins Books, Cork, Leenaun Hill lies on a massif t ...
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Letterbreckaun
Letterbreckaun () is one of the Maumturk Mountains of Connemara in County Galway, Ireland. At , it is the second-tallest of the Maumturks, the 129th–highest peak in Ireland on the Arderin list, and 159th–highest on the Vandeleur-Lynam list.Mountainviews, (September 2013), "A Guide to Ireland's Mountain Summits: The Vandeleur-Lynams & the Arderins", Collins Books, Cork, Letterbreckaun is in the middle sector of the long north-west to south-east spine of the Maumturks. Naming The anglicised name "Letterbreckaun" comes from ga, Leitir Bhriocáin or ''Leitir Breacáin'' meaning "Brecan's hillside", and is also the name of a townland on the slope of the mountain. Saint Brecan is a saint associated with Galway county, and is said to be the successor to Saint Enda of Aran. Geography Letterbreckaun lies at the northern end of the central sector, of the long north-west to south-east central spine of the Maumturks range, in the Connemara National Park; when viewed from the west, ...
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Siltstone
Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility.Blatt ''et al.'' 1980, pp.381-382 Although its permeability and porosity is relatively low, siltstone is sometimes a tight gas reservoir rock, an unconventional reservoir for natural gas that requires hydraulic fracturing for economic gas production. Siltstone was prized in ancient Egypt for manufacturing statuary and cosmetic palettes. The siltstone quarried at Wadi Hammamat was a hard, fine-grained siltstone that resisted flaking and was almost ideal for such uses. Description There is not complete agreement on the definition of siltstone. One definition is that siltstone is mudrock ( clastic sedimentary rock containing at least 50% clay and silt) in which at least 2/3 of the clay and silt fraction is composed of silt-sized particles. Silt is defined a ...
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University College Galway
The University of Galway ( ga, Ollscoil na Gaillimhe) is a public research university located in the city of Galway, Ireland. A tertiary education and research institution, the university was awarded the full five QS stars for excellence in 2012, and was ranked among the top 1 percent of universities in the 2018 ''QS World University Rankings''. The university was founded in 1845 as "Queen's College, Galway". It was known as "University College, Galway" (UCG) (Irish: ''Coláiste na hOllscoile, Gaillimh''), until 1997 and as "National University of Ireland, Galway" (NUI Galway) (Irish: ''Ollscoil na hÉireann, Gaillimh; OÉ Gaillimh''), until 2022. In late April 2022, it was announced that NUI Galway would be renamed "Ollscoil na Gaillimhe – University of Galway" in summer 2022, amid confusion over its proper title. University of Galway is a member of the Coimbra Group, a network of 40 long-established European universities. History The university was established in 1845 as ' ...
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Maam Cross
Maam Cross () is a crossroads in Connemara, County Galway, Ireland. It lies within the townland of Shindilla, at the junction of the N59 from Galway to Clifden and the R336 from Galway to the Maam Valley which runs from Maum or Maam to Leenaun Leenaun (), also Leenane, is a village and 1,845 acre townland in County Galway, Ireland, on the southern shore of Killary Harbour and the northern edge of Connemara. Location Leenaun is situated on the junction of the N59 road, and the R336 ... or Leenane. station, on the Galway - Clifden line, opened on 1 January 1896. It finally closed on 29 April 1935. The station facilities and a short section of railway line have been restored in a project launched in 2017 and ongoing as of 2022. The location has a service station and hotel, with dining facilities and a gift shop. It is also home to a weekly agricultural mart, handling sheep, cattle and Connemara ponies. See also * List of towns and villages in Ireland References E ...
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Mweelrea
Mweelrea (; ) at , is the 26th-highest peak in Ireland on the Arderin scale, and the 34th-highest peak on the Vandeleur-Lynam scale.Mountainviews, (September 2013), "A Guide to Ireland's Mountain Summits: The Vandeleur-Lynams & the Arderins", Collins Books, Cork, Mweelrea is situated near the apex of a "horseshoe-shaped" massif that includes the peaks of Ben Lugmore and Ben Bury, and which is located between Killary Harbour and Doo Lough, in Mayo, Ireland. Mweelrea is the provincial top for Connacht, and is noted for its southeastern cliff lined corries, and its views. The massif is called the Mweelrea Mountains or the Mweelrea Range. Naming Mweelrea is an anglicisation of the , which translates as "bald hill with the smooth top", which describes the profile of the mountain. Geology The geology of what is known as the ''Mweelrea Formation'' is very different from that of the Twelve Bens, on the other side of Killary Harbour. At a summary level, the ''Mweelrea Formation'' ...
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Fjord
In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Iceland, Ireland, Kamchatka, the Kerguelen Islands, Labrador, Newfoundland, New Zealand, Norway, Novaya Zemlya, Nunavut, Quebec, the Patagonia region of Argentina and Chile, Russia, South Georgia Island, Tasmania, United Kingdom, and Washington state. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords wh ...
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Maam Turk
Letterbreckaun () is one of the Maumturk Mountains of Connemara in County Galway, Ireland. At , it is the second-tallest of the Maumturks, the 129th–highest peak in Ireland on the Arderin list, and 159th–highest on the Vandeleur-Lynam list.Mountainviews, (September 2013), "A Guide to Ireland's Mountain Summits: The Vandeleur-Lynams & the Arderins", Collins Books, Cork, Letterbreckaun is in the middle sector of the long north-west to south-east spine of the Maumturks. Naming The anglicised name "Letterbreckaun" comes from ga, Leitir Bhriocáin or ''Leitir Breacáin'' meaning "Brecan's hillside", and is also the name of a townland on the slope of the mountain. Saint Brecan is a saint associated with Galway county, and is said to be the successor to Saint Enda of Aran. Geography Letterbreckaun lies at the northern end of the central sector, of the long north-west to south-east central spine of the Maumturks range, in the Connemara National Park; when viewed from the west, ...
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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 met ...
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Metavolcanic Rock
Metavolcanic rock is volcanic rock that shows signs of having experienced metamorphism. In other words, the rock was originally produced by a volcano, either as lava or tephra. The rock was then subjected to high pressure, high temperature or both, for example by burial under younger rocks, causing the original volcanic rock to recrystallization (geology), recrystallize. Metavolcanic rocks are sometimes described informally as ''metavolcanics''. When it is possible to determine the original volcanic rock type from the properties of the metavolcanic rock (particularly if the degree of metamorphism is slight), the rock is more precisely named by appylying the prefix ''meta-'' to the original rock type. For example, a weakly metamorphosed basalt would be described as a ''metabasalt'', or a weakly metamorphosed tuff as a ''metatuff''. Metavolcanic rock is commonly found in greenstone belts. See also * References

{{petrology-stub Metamorphic rocks Volcanic rocks Metamorphic pe ...
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Marbles
A marble is a small spherical object often made from glass, clay, steel, plastic, or agate. They vary in size, and most commonly are about in diameter. These toys can be used for a variety of games called ''marbles'', as well being placed in marble runs or races, or created as a form of art. They are often collected, both for nostalgia and for their aesthetic colors. Sizes may range from less than to over , while some art glass marbles for display purposes are over wide. In the North of England the objects and the game are called "taws", with larger taws being called "bottle washers" after the use of a marble in Codd-neck bottles, which were often collected for play. Games History In the early twentieth century, small balls of stone from about 2500 BCE, identified by archaeologists as marbles, were found by excavation near Mohenjo-daro, in a site associated with the Indus Valley civilization. Marbles are often mentioned in Roman literature, as in Ovid's poem "Nux" (which ...
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Topographic Prominence
In topography, prominence (also referred to as autonomous height, relative height, and shoulder drop in US English, and drop or relative height in British English) measures the height of a mountain or hill's summit relative to the lowest contour line encircling it but containing no higher summit within it. It is a measure of the independence of a summit. A peak's ''key col'' (the highest col surrounding the peak) is a unique point on this contour line and the ''parent peak'' is some higher mountain, selected according to various criteria. Definitions The prominence of a peak may be defined as the least drop in height necessary in order to get from the summit to any higher terrain. This can be calculated for a given peak in the following way: for every path connecting the peak to higher terrain, find the lowest point on the path; the ''key col'' (or ''key Saddle point, saddle'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting pat ...
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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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