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An Meall Dubh
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 that overlooks Leenaun village and Killary Harbour, and which is at the far northeastern sector of the Maumturks mountain range in the Connemara National Park in County Galway, Ireland; this massif is connected to the main range via the "Col of Despondency". Leenaun Hill is the 6th-highest mountain in the Maumturks, and its grassy massif, constructed from sandstone and siltstone, contrasts with the rocky ridges and summits constructed from quartzites, grits, and graphitic, of the middle and southern sectors of the range. Naming Irish academic Paul Tempan records that Leenaun hill has also been called "Bunnaviskaun". The peak has been called Leenaun Mountain. Tempan notes the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Lists of mountains in Ireland#Arderins, Arderin list, and 159th–highest on the Lists of mountains in Ireland#Vandeleur-Lynams, 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 the 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 Enda of Aran, Saint Enda of Aran. Geography Letterbreckaun lies at the northern end of the central sector, of the long north-west to the south-east central spi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartzites
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 resistant h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ben Gorm
Ben Gorm () is a mountain with a height of on the north side of Killary Harbour in County Mayo, Ireland. The Ben Gorm mountains also includes two other peaks: Ben Creggan/''Binn an Charragáin'' (693 m), and Maul Laur/''Meall Láir'' or Ben Creggan South Top (687 m). MountainViews.ie. The Ben Gorm group overlooks Killary Harbour to the south, Fin Lough and Doo Lough (Mayo), Doo Lough to the west (which separate it from the Mweelrea Mountains), Glenummera to the north (which separate it from the Sheeffry Hills), and Glendavock to the east. 
See also *Lists of mountains in Ir ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
University College Galway
The University of Galway () is a public university, public research university located in the city of Galway, Republic of Ireland, Ireland. The university was founded in 1845 as "Queen's College, Galway". It was known as "University College, Galway" (UCG) () from 1908 to 1997 and as "National University of Ireland Galway" (NUI Galway) () from 1997 to 2022. In September 2022, it changed its name to "University of Galway". The 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 Queen's College, Galway, together with University College Cork, Queen's College, Cork, and Queen's University Belfast, Queen's College, Belfast. It opened for teaching on 30 October 1849 with 68 students. In 1850, it became part of the Queen's University of Ireland, and its degrees were conferred in the name of that university. Located close to the city centre, the university campus stretches alon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Galway ( ; , ) is a City status in Ireland, city in (and the county town of) County Galway. It lies on the River Corrib between Lough Corrib and Galway Bay. It is the most populous settlement in the province of Connacht, the List of settleme ... to the Maam Valley which runs from Maum or Maam to Leenaun 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mweelrea
Mweelrea (; ) is a mountain on the Atlantic coast of County Mayo, Ireland. Rising to , it is the highest mountain in the western province of Connacht, and is noted for its southeastern cliff-lined corries, and its views. Mweelrea overlooks Killary Harbour and is at the heart of a "horseshoe-shaped" massif that includes the peaks of Ben Lugmore and Ben Bury. The massif is called the Mweelrea Mountains or the Mweelrea Range. Mweelrea is also the 26th-highest peak in Ireland on the Arderin list, and the 34th-highest on the Vandeleur-Lynam list.Mountainviews, (September 2013), "A Guide to Ireland's Mountain Summits: The Vandeleur-Lynams & the Arderins", Collins Books, Cork, 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'' consists of Ordovician period sandstones originally deposited on large alluvial fans, and distally‐equi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fjord
In physical geography, a fjord (also spelled fiord in New Zealand English; ) is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Antarctica, the Arctic, and surrounding landmasses of the northern and southern hemispheres. 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 when flooded by the ocean. Thresholds above sea level create freshwater lakes. Glacial melting is accompanied by the rebounding of Earth's crust as the ice load and eroded sediment is removed (also called isostasy or gla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 the 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 the south-east central spine of the Maumturks range, in the Connemara National Park; when viewed from the west, the peak has ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 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 Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial ... would be describe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marbles
A marble is a small spherical object often made from glass, clay, steel, plastic, or agate. 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 vary, but usually range from about in diameter. In the north of England the game and objects are called "taws", with larger taws being called "bottle washers", named 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. In modern India the game is called "kanche". Marbles are often mentioned in Roman literature, as in Ovid's poem "Nux" (which mentions playing the game with walnuts), and there are many ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Topographic Prominence
In topography, prominence or relative height (also referred to as autonomous height, and shoulder drop in US English, and drop 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. The key col ("saddle") around the peak is a unique point on this contour line and the ''parent peak'' (if any) is some higher mountain, selected according to various criteria. Definitions The prominence of a peak is 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 manner: for every path connecting the peak to higher terrain, find the lowest point on the path; the ''key col'' (or ''highest saddle (landform), saddle'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting paths; the prominence is the differ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
