1.
Summit
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A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. Mathematically, a summit is a maximum in elevation. The topographic terms acme, apex, peak, and zenith are synonymous, the UIAA definition is that a summit is independent if it has a prominence of 30 metres or more, it is a mountain if it has a prominence of at least 300 metres. This can be summarised as follows, A pyramidal peak is an exaggerated form produced by ice erosion of a mountain top, Summit may also refer to the highest point along a line, trail, or route. In many parts of the western United States, the term refers to the highest point along a road, highway. For example, the highest point along Interstate 80 in California is referred to as Donner Summit while the highest point on Interstate 5 is Siskiyou Mountain Summit, geoid Hill List of highest mountains Maxima and minima Nadir Summit accordance Peak finder
2.
Topographic prominence
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It is a measure of the independence of a summit. A peaks key col is a point on this contour line. By convention, the prominence of Mount Everest, the Earths highest mountain, is taken to equal the elevation of its summit above sea level, if the peaks prominence is P metres, to get from the summit to any higher terrain one must descend at least P metres. Together with the convention for Mount Everest, this implies that the prominence of any island or continental highpoint is equal to its elevation above sea level, for every ridge connecting the peak to higher terrain, find the lowest point on the ridge. The key col is defined as the highest of these cols, the prominence is the difference between the elevation of the peak and the elevation of the key col. The following mental exercise may illustrate the meaning of topographic prominence, imagine you are standing at the top of a peak and imagine that an imaginary sea level rises to your feet. Now slowly lower the sea level and an imaginary island appears beneath your feet. Your island will grow and will merge with other islands that emerge, the parent peak may be either close or far from the subject peak. The summit of Mount Everest is the parent peak of Aconcagua at a distance of 17,755 km, the key col may also be close or far from the subject peak. The key col for Aconcagua is the Bering Strait at a distance of 13,655 km, the key col for the South Summit of Mount Everest is about 100 m distant. Prominence is interesting to many mountaineers because it is a measurement that is strongly correlated with the subjective significance of a summit. Peaks with low prominences are either subsidiary tops of some higher summit or relatively insignificant independent summits, peaks with high prominences tend to be the highest points around and are likely to have extraordinary views. Only summits with a sufficient degree of prominence are regarded as independent mountains, for example, the worlds second-highest mountain is K2. While Mount Everests South Summit is taller than K2, it is not considered an independent mountain because it is a subsummit of the main summit, many lists of mountains take topographic prominence as a criterion for inclusion, or cutoff. John and Anne Nuttalls The Mountains of England and Wales uses a cutoff of 15 m, in the contiguous United States, the famous list of fourteeners uses a cutoff of 300 ft /91 m. Also in the U. S.2000 feet of prominence has become a threshold that signifies that a peak has major stature. This generates lists of peaks ranked by prominence, which are different from lists ranked by elevation. Such lists tend to emphasize isolated high peaks, such as range or island high points, one advantage of a prominence-ranked list is that it needs no cutoff, since a peak with high prominence is automatically an independent peak
3.
Marilyn (geography)
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A Marilyn is a mountain or hill in the United Kingdom, Republic of Ireland or Isle of Man with a prominence of at least 150 metres, regardless of absolute height or other merit. The name was coined as a punning contrast to the designation Munro, used of a Scottish mountain with a height of more than 3,000 feet, which is homophonous with Monroe. There are 2,010 Marilyns identified,1,218 in Scotland,454 in Ireland,175 in England,158 in Wales,5 on the Isle of Man. Black Mountain, in the Black Mountains, on the border between England and Wales, was counted in both countries but is now treated as being in Wales only. The list was extended into Ireland by Clem Clements in a booklet, The Hewitts, however, some lower hills such as Seatallan and Watch Hill on the edges of Lakeland and the Long Mynd in Shropshire do qualify because of their isolation from higher hills. At the other extreme are Stac Lee and Stac an Armin, nearly 80% of Marilyns in Great Britain are in Scotland. They logically extend earlier Scottish lists such as the Munros, Corbetts, Grahams, all Corbetts and Grahams,203 of the 282 Munros, and around half of the Donalds are also Marilyns. Some hillwalkers attempt to climb as many Marilyns as possible, some amateur radio operators attempt to operate from the summit of every Marilyn. Eddie Dealtry became the person to achieve Woodalls feat, later on the same day. By 28 September 2016, the Marilyns of Great Britain had been completed by 10 hillwalkers, while 320 had entered the Marilyn Hall of Fame by attaining a count of at least 600
4.
Geographic coordinate system
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A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
5.
County Cork
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County Cork is the largest and southernmost county of Ireland. It lies in the province of Munster and is named after the city of Cork, Cork County Council is the local authority for the county. Its largest settlements are Cork City, Ballincollig and Carrigaline, in 2016, the countys population was 542,196, making it the third most populous county in Ireland. There are two local authorities whose remit collectively encompasses the area of the county and city of Cork. The county, excluding Cork city, is administered by Cork County Council, both city and county are part of the South-West Region. For standardized European statistical purposes both Cork County Council and Cork City Council rank equally as first-level local administrative units of the NUTS3 South-West Region, there are 34 such LAU1 entities in the Republic of Ireland. For elections to Dáil Éireann, the county is divided into five constituencies—Cork East, Cork North–Central, Cork North–West, Cork South–Central, together they return 19 deputies to the Dáil. The county is part of the South constituency for the purposes of European elections, for purposes other than local government, such as the formation of sporting teams, the term County Cork is often taken to include both city and county. County Cork is located in the province of Munster and it borders four other counties, Kerry to the west, Limerick to the north, Tipperary to the north-east and Waterford to the east. Cork is the largest county in the state by land area and it is the largest of Munsters 6 counties by both population and area. The population of Cork city stood at 125,622 in 2016, the population of the entire county is 542,196 making it the states second most populous county and the third most populous county on the island of Ireland. The remit of Cork County Council includes some suburbs of the city not within the area of Cork City Council, there are 24 historic baronies in the county—the most of any county in Ireland. While baronies continue to be officially defined units, they are no longer used for administrative purposes. Their official status is illustrated by Placenames Orders made since 2003, there are 253 civil parishes in the county. Townlands are the smallest officially defined geographical divisions in Ireland, there are approximately 5447 townlands in the county, the Shehy Mountains are on the border with Kerry and may be accessed from the area known as Priests Leap, near the village of Coomhola. The Galtee Mountains are located across parts of Tipperary, Limerick, the upland areas of the Ballyhoura, Boggeragh, Derrynasaggart and the Mullaghareirk Mountain ranges add to the range of habitats found in the county. Important habitats in the uplands include blanket bog, heath, glacial lakes, Cork has the 13th highest county peak in Ireland. The three great rivers, the Bandon, the Blackwater and the Lee, and their valleys dominate central Cork, habitats of the valleys and floodplains include woodlands, marshes, fens and species-rich limestone grasslands
6.
Republic of Ireland
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Ireland, also known as the Republic of Ireland, is a sovereign state in north-western Europe occupying about five-sixths of the island of Ireland. The capital and largest city is Dublin, which is located on the part of the island. The state shares its land border with Northern Ireland, a part of the United Kingdom. It is otherwise surrounded by the Atlantic Ocean, with the Celtic Sea to the south, Saint Georges Channel to the south-east, and it is a unitary, parliamentary republic. The head of government is the Taoiseach, who is elected by the Dáil and appointed by the President, the state was created as the Irish Free State in 1922 as a result of the Anglo-Irish Treaty. It was officially declared a republic in 1949, following the Republic of Ireland Act 1948, Ireland became a member of the United Nations in December 1955. It joined the European Economic Community, the predecessor of the European Union, after joining the EEC, Ireland enacted a series of liberal economic policies that resulted in rapid economic growth. The country achieved considerable prosperity between the years of 1995 and 2007, which known as the Celtic Tiger period. This was halted by a financial crisis that began in 2008. However, as the Irish economy was the fastest growing in the EU in 2015, Ireland is again quickly ascending league tables comparing wealth and prosperity internationally. For example, in 2015, Ireland was ranked as the joint sixth most developed country in the world by the United Nations Human Development Index and it also performs well in several national performance metrics, including freedom of the press, economic freedom and civil liberties. Ireland is a member of the European Union and is a member of the Council of Europe. The 1922 state, comprising 26 of the 32 counties of Ireland, was styled, the Constitution of Ireland, adopted in 1937, provides that the name of the State is Éire, or, in the English language, Ireland. Section 2 of the Republic of Ireland Act 1948 states, It is hereby declared that the description of the State shall be the Republic of Ireland. The 1948 Act does not name the state as Republic of Ireland, because to have done so would have put it in conflict with the Constitution. The government of the United Kingdom used the name Eire, and, from 1949, Republic of Ireland, for the state, as well as Ireland, Éire or the Republic of Ireland, the state is also referred to as the Republic, Southern Ireland or the South. In an Irish republican context it is referred to as the Free State or the 26 Counties. From the Act of Union on 1 January 1801, until 6 December 1922, during the Great Famine, from 1845 to 1849, the islands population of over 8 million fell by 30%
7.
Mountain range
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A mountain range is a geographic area containing numerous geologically related mountains. A mountain system or system of ranges, sometimes is used to combine several geological features that are geographically related. Mountain ranges are usually segmented by highlands or mountain passes and valleys, individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, most geologically young mountain ranges on the Earths land surface are associated with either the Pacific Ring of Fire or the Alpide Belt. The Andes is 7,000 kilometres long and is considered the worlds longest mountain system. The Alpide belt includes Indonesia and southeast Asia, through the Himalaya, the belt also includes other European and Asian mountain ranges. The Himalayas contain the highest mountains in the world, including Mount Everest, mountain ranges outside of these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Altai Mountains and the Hijaz Mountains. If the definition of a range is stretched to include underwater mountains. The mountain systems of the earth are characterized by a tree structure, the sub-range relationship is often expressed as a parent-child relationship. For example, the White Mountains of New Hampshire and the Blue Ridge Mountains are sub-ranges of the Appalachian Mountains, equivalently, the Appalachians are the parent of the White Mountains and Blue Ridge Mountains, and the White Mountains and the Blue Ridge Mountains are children of the Appalachians. The position of mountains influences climate, such as rain or snow, when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the side, it warms again and is drier. Often, a shadow will affect the leeward side of a range. Mountain ranges are constantly subjected to forces which work to tear them down. Erosion is at work while the mountains are being uplifted and long after until the mountains are reduced to low hills, rivers are traditionally believed to be the principle erosive factor on mountain ranges, with their ability of bedrock incision and sediment transport. The rugged topography of a range is the product of erosion. The basins adjacent to a mountain range are filled with sediments which are buried and turned into sedimentary rock. The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example and this mass of rock was removed as the range was actively undergoing uplift
8.
Irish grid reference system
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The Irish grid reference system is a system of geographic grid references commonly used in Ireland. The Irish grid lies within the British grid, but uses a different co-ordinate system with a meridian more suited to the westerly location, in general, neither Ireland nor Great Britain uses latitude or longitude in describing internal geographic locations. Instead grid reference systems are in common usage, the national grid referencing system was devised by the Ordnance Survey, and is heavily used in their survey data, and in maps based on those surveys. Additionally grid references are commonly quoted in publications and data sources. The Ordnance Survey of Ireland has implemented a new system for Ireland called Irish Transverse Mercator, or ITM. In both systems, the origin is at 53°30 N, 8° W — a point in Lough Ree, close to the western shore. The area of Ireland is divided into 25 squares, measuring 100 by 100 km, the squares are numbered A to Z with I being omitted. Seven of the squares do not actually cover any land in Ireland, within each square, eastings and northings from the origin of the square are given numerically. For example, G0305 means square G,3 km east,5 km north, coordinates may also be given relative to the origin of the entire 500 by 500 km grid. For example, the location of the Spire of Dublin on OConnell Street may be given as 315904,234671 as well as O1590434671, coordinates in this format must never be truncated, because, for example,31590,23467 is also a valid location. Ordnance Survey Ireland,185 years of innovation in mapping, archived from the original on September 11,2009. The Irish Grid - A Description of the Co-ordinate Reference System used in Ireland PDF on the Irish Grid from OSi, history and overview of the system, from OSI OSI online coordinate converter tool Clickable webmap that shows Irish grid references
9.
Irish language
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Irish, also referred to as Gaelic or Irish Gaelic, is a Goidelic language of the Indo-European language family originating in Ireland and historically spoken by the Irish people. Irish is spoken as a first language by a minority of Irish people. Irish enjoys constitutional status as the national and first official language of the Republic of Ireland and it is also among the official languages of the European Union. The public body Foras na Gaeilge is responsible for the promotion of the language throughout the island of Ireland and it has the oldest vernacular literature in Western Europe. The fate of the language was influenced by the power of the English state in Ireland. Elizabethan officials viewed the use of Irish unfavourably, as being a threat to all things English in Ireland and its decline began under English rule in the 17th century. In the latter part of the 19th century, there was a decrease in the number of speakers. Irish-speaking areas were hit especially hard, by the end of British rule, the language was spoken by less than 15% of the national population. Since then, Irish speakers have been in the minority, efforts have been made by the state, individuals and organisations to preserve, promote and revive the language, but with mixed results. Around the turn of the 21st century, estimates of native speakers ranged from 20,000 to 80,000 people. In the 2011 Census, these numbers had increased to 94,000 and 1.3 million, there are several thousand Irish speakers in Northern Ireland. It has been estimated that the active Irish-language scene probably comprises 5 to 10 per cent of Irelands population, there has been a significant increase in the number of urban Irish speakers, particularly in Dublin. In Gaeltacht areas, however, there has been a decline of the use of Irish. Údarás na Gaeltachta predicted that, by 2025, Irish will no longer be the language in any of the designated Gaeltacht areas. Survey data suggest that most Irish people think highly of Irish as a marker of identity. It has also argued that newer urban groups of Irish speakers are a disruptive force in this respect. In An Caighdeán Oifigiúil the name of the language is Gaeilge, before the spelling reform of 1948, this form was spelled Gaedhilge, originally this was the genitive of Gaedhealg, the form used in Classical Irish. Older spellings of this include Gaoidhealg in Classical Irish and Goídelc in Old Irish, the modern spelling results from the deletion of the silent dh in the middle of Gaedhilge, whereas Goidelic languages, used to refer to the language family including Irish, comes from Old Irish
