1.
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%
2.
Munster
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Munster is one of the provinces of Ireland situated in the south of Ireland. In early Ireland, it was one of the fifths ruled by a king of over-kings Irish, following the Norman invasion of Ireland, the ancient kingdoms were shired into counties for administrative and judicial purposes. In later centuries, local government legislation has seen further sub-division of the historic counties, Munster has no official function for local government purposes. For the purposes of the ISO, the province is listed as one of the provincial sub-divisions of the State, geographically, Munster covers a total area of 24,675 km2 and has a population of 1,246,088 with the most populated city being Cork. Other significant urban centres in the province include Limerick and Waterford, in the early centuries AD, Munster was the domain of the Iverni peoples and the Clanna Dedad familial line, led by Cú Roí and to whom the king Conaire Mór also belonged. In the 5th century, Saint Patrick spent several years in the area and founded Christian churches, during the Early Middle Ages, most of the area was part of the Kingdom of Munster, ruled by the Eóganachta dynasty. Prior to this, the area was ruled by the Dáirine and Corcu Loígde overlords from the early 7th century onwards, later rulers from the Eóganachta who would dominate a greater part of Ireland were Cathal mac Finguine and Feidlimid mac Cremthanin. Notable regional kingdoms and lordships of Early Medieval Munster were Iarmuman, Osraige, Uí Liatháin, Uí Fidgenti, Éile, Múscraige, Ciarraige Luachra, Corcu Duibne, Corcu Baiscinn, around this period Ossory broke away from Munster. The 10th century saw the rise of the Dalcassian clan, who had earlier annexed Thomond and their leaders were the ancestors of the OBrien dynasty and spawned Brian Boru, perhaps the most noted High King of Ireland, and several of whose descendants were also High Kings. By 1118 Munster had fractured into the Kingdom of Thomond under the OBriens, the Kingdom of Desmond under the MacCarthy dynasty, the three crowns of the flag of Munster represent these three late kingdoms. The OBrien of Thomond and MacCarthy of Desmond surrendered and regranted sovereignty to the Tudors in 1543 and 1565, the impactful Desmond Rebellions, led by the FitzGeralds, soon followed. By the mid-19th century much of the area was hit hard in the Great Famine, the province was affected by events in the Irish War of Independence in the early 20th century, and there was a brief Munster Republic during the Irish Civil War. The Irish leaders Michael Collins and earlier Daniel OConnell came from families of the old Gaelic Munster gentry, noted for its traditions in Irish folk music, and with many ancient castles and monasteries in the province, Munster is a tourist destination. During the fifth century, St. Patrick spent seven years founding churches and ordaining priests in Munster, but a fifth century bishop named Ailbe is the patron saint of Munster. In Irish mythology, a number of goddesses are associated with the province including Anann, Áine, Grian, Clíodhna, Aimend, Mór Muman, Bébinn, Aibell. Each is historically associated with certain septs of the nobility, the druid-god of Munster is Mug Ruith. The province has long had trading and cultural links with continental Europe, the tribe of Corcu Loígde had a trading fleet active along the French Atlantic coast, as far south as Gascony, importing wine to Munster. The Eóganachta had ecclesiastical ties with Germany, which show in the architecture of their capital at the Rock of Cashel
3.
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
4.
National secondary road
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A national secondary road is a category of road in Ireland. These roads form an important part of the route network. National secondary roads are designated with route numbers higher than used for primary roads. Routes N51 and higher are all national secondary roads, National secondary roads have a default speed limit of 100 km/h, as along with national primary routes, they fall into the speed limit category of national roads. There are 2657 km of secondary roads in Ireland, making up slightly over 50% of the entire national route network. National secondary routes are more poorly maintained than primary routes. Typically, national roads are of a similar standard or higher than regional roads although some are of lower quality than the better sections of regional roads. Many of them have been resurfaced with higher quality pavements in recent years with smooth surfaces and good road markings. However, road widths and alignments are often inadequate, with many narrow, the former N8 bypass of Mitchelstown was re-classified as the N73 when the Fermoy to Kilbehenny section of the M8 was completed. Most national secondary roads were originally Trunk Roads under the old system of classification in Ireland. In addition, a section of the N60 between Castlebar and Westport became part of the N5, some national secondary roads, though not arterial routes between major cities, connect scenic areas to major population centres. For example, the N59 through County Galway and County Mayo, the N70 road through County Kerry, for this reason, many national secondary roads are well-traveled by tourists. = Junction with road XXXX, e. g. = Junction with N21 road N57 road – Defunct route designation, swinford – Ballina route prior to its redesignation as the N26 National primary road. N64 road – Defunct route designation, oranmore – Claregalway route prior to its redesignation as the N18 National primary road. N79 road – Defunct route designation, enniscorthy – New Ross route prior to its redesignation as the N30 National primary road. I. 209/1994, Roads Act,1993 Order,1994 Roads Act 1993 Order 2006 – Department of Transport - National Roads Authority, National Route Lengths 2007
5.
Fortification
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Fortifications are military constructions or buildings designed for the defense of territories in warfare, and also used to solidify rule in a region during peace time. Humans have constructed defensive works for many thousands of years, in a variety of increasingly complex designs, the term is derived from the Latin fortis and facere. From very early history to modern times, walls have been a necessity for cities to survive in a changing world of invasion. Some settlements in the Indus Valley Civilization were the first small cities to be fortified, in ancient Greece, large stone walls had been built in Mycenaean Greece, such as the ancient site of Mycenae. A Greek Phrourion was a collection of buildings used as a military garrison. These construction mainly served the purpose of a tower, to guard certain roads, passes. Though smaller than a fortress, they acted as a border guard rather than a real strongpoint to watch. The art of setting out a camp or constructing a fortification traditionally has been called castramentation since the time of the Roman legions. Fortification is usually divided into two branches, permanent fortification and field fortification, there is also an intermediate branch known as semi-permanent fortification. Castles are fortifications which are regarded as being distinct from the fort or fortress in that they are a residence of a monarch or noble. Roman forts and hill forts were the antecedents of castles in Europe. The Early Middle Ages saw the creation of towns built around castles. Medieval-style fortifications were made obsolete by the arrival of cannons in the 14th century. Fortifications in the age of black powder evolved into much lower structures with greater use of ditches and earth ramparts that would absorb, Walls exposed to direct cannon fire were very vulnerable, so were sunk into ditches fronted by earth slopes. The arrival of explosive shells in the 19th century led to yet another stage in the evolution of fortification, steel-and-concrete fortifications were common during the 19th and early 20th centuries. However the advances in warfare since World War I have made large-scale fortifications obsolete in most situations. Demilitarized zones along borders are arguably another type of fortification, although a passive kind, many military installations are known as forts, although they are not always fortified. Larger forts may be called fortresses, smaller ones were known as fortalices
6.
Ireland
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Ireland is an island in the North Atlantic. It is separated from Great Britain to its east by the North Channel, the Irish Sea, Ireland is the second-largest island of the British Isles, the third-largest in Europe, and the twentieth-largest on Earth. Politically, Ireland is divided between the Republic of Ireland, which covers five-sixths of the island, and Northern Ireland, in 2011, the population of Ireland was about 6.4 million, ranking it the second-most populous island in Europe after Great Britain. Just under 4.6 million live in the Republic of Ireland, the islands geography comprises relatively low-lying mountains surrounding a central plain, with several navigable rivers extending inland. The island has lush vegetation, a product of its mild, thick woodlands covered the island until the Middle Ages. As of 2013, the amount of land that is wooded in Ireland is about 11% of the total, there are twenty-six extant mammal species native to Ireland. The Irish climate is moderate and classified as oceanic. As a result, winters are milder than expected for such a northerly area, however, summers are cooler than those in Continental Europe. Rainfall and cloud cover are abundant, the earliest evidence of human presence in Ireland is dated at 10,500 BC. Gaelic Ireland had emerged by the 1st century CE, the island was Christianised from the 5th century onward. Following the Norman invasion in the 12th century, England claimed sovereignty over Ireland, however, English rule did not extend over the whole island until the 16th–17th century Tudor conquest, which led to colonisation by settlers from Britain. In the 1690s, a system of Protestant English rule was designed to materially disadvantage the Catholic majority and Protestant dissenters, with the Acts of Union in 1801, Ireland became a part of the United Kingdom. Northern Ireland saw much civil unrest from the late 1960s until the 1990s and this subsided following a political agreement in 1998. In 1973 the Republic of Ireland joined the European Economic Community while the United Kingdom, Irish culture has had a significant influence on other cultures, especially in the fields of literature. Alongside mainstream Western culture, an indigenous culture exists, as expressed through Gaelic games, Irish music. The culture of the island shares many features with that of Great Britain, including the English language, and sports such as association football, rugby, horse racing. The name Ireland derives from Old Irish Eriu and this in turn derives from Proto-Celtic *Iveriu, which is also the source of Latin Hibernia. Iveriu derives from a root meaning fat, prosperous, during the last glacial period, and up until about 9000 years ago, most of Ireland was covered with ice, most of the time
7.
Castle
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A castle is a type of fortified structure built in Europe and the Middle East during the Middle Ages by European nobility. Scholars debate the scope of the castle, but usually consider it to be the private fortified residence of a lord or noble. Usage of the term has varied over time and has applied to structures as diverse as hill forts. Over the approximately 900 years that castles were built, they took on a great many forms with different features, although some, such as curtain walls. A European innovation, castles originated in the 9th and 10th centuries, after the fall of the Carolingian Empire resulted in its territory being divided among individual lords and princes. Although their military origins are often emphasised in castle studies, the structures served as centres of administration. Many castles were built from earth and timber, but had their defences replaced later by stone. Early castles often exploited natural defences, lacking features such as towers and arrowslits, in the late 12th and early 13th centuries, a scientific approach to castle defence emerged. This led to the proliferation of towers, with an emphasis on flanking fire, many new castles were polygonal or relied on concentric defence – several stages of defence within each other that could all function at the same time to maximise the castles firepower. These changes in defence have been attributed to a mixture of castle technology from the Crusades, such as concentric fortification, not all the elements of castle architecture were military in nature, so that devices such as moats evolved from their original purpose of defence into symbols of power. Some grand castles had long winding approaches intended to impress and dominate their landscape, while castles continued to be built well into the 16th century, new techniques to deal with improved cannon fire made them uncomfortable and undesirable places to live. As a result, true castles went into decline and were replaced by artillery forts with no role in civil administration, and country houses that were indefensible. From the 18th century onwards, there was a renewed interest in castles with the construction of castles, part of a romantic revival of Gothic architecture. The word castle is derived from the Latin word castellum, which is a diminutive of the word castrum, meaning fortified place. The Old English castel, Old French castel or chastel, French château, Spanish castillo, Italian castello, the word castle was introduced into English shortly before the Norman Conquest to denote this type of building, which was then new to England. In its simplest terms, the definition of a castle accepted amongst academics is a fortified residence. Feudalism was the link between a lord and his vassal where, in return for service and the expectation of loyalty. Castles served a range of purposes, the most important of which were military, administrative, as well as defensive structures, castles were also offensive tools which could be used as a base of operations in enemy territory
8.
Pembrokeshire
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Pembrokeshire is a county in the south west of Wales. It borders Carmarthenshire to the east and Ceredigion to the north east, Pembrokeshire County Councils headquarters are in the county town of Haverfordwest. Over the years Pembrokeshires beaches have received many International Blue Flag Awards, Green Coast Awards. In 2011 it had 39 beaches recommended by the Marine Conservation Society, industry is nowadays focused on agriculture and tourism, but historically mining and fishing were important activities. The county has a geography and a complex history. Pembrokeshires population was 122,400 at the 2011 census, an increase of 7. 2% from the 2001 figure of 114,131, Pembrokeshire is bordered by the sea on three sides, and by the counties of Ceredigion to the north east and Carmarthenshire to the east. Other towns include Pembroke, Pembroke Dock, Milford Haven, Fishguard, Tenby, Saundersfoot, Narberth, Neyland, St Davids, in the west of the county, is the United Kingdoms smallest city with a population of 2,000. Saundersfoot is the biggest village in Pembrokeshire with a population of well over 2,500, see List of places in Pembrokeshire for a comprehensive list of settlements in Pembrokeshire. The countys coastline includes internationally important seabird breeding sites and numerous bays, Pembrokeshire contains a predominantly coastal park, Pembrokeshire Coast National Park, which includes a 186-mile walking trail, the Pembrokeshire Coast Path. A large estuary and natural harbour at Milford Haven cuts deeply into the coast, this inlet is formed by the confluence of the Western Cleddau, the Eastern Cleddau, and rivers Cresswell and Carew. The estuary is bridged by the large Cleddau Bridge which carries the A477 between Neyland and Pembroke Dock, upstream bridges span the Cleddau at Haverfordwest and Canaston Bridge, large bays are Newport Bay, Fishguard Bay, St Brides Bay and a portion of Carmarthen Bay. There are several islands off the Pembrokeshire coast, the largest of which are Ramsey Island, Grassholm Island, Skomer Island. Pembrokeshires diverse range of features was a key factor in the establishment of the Pembrokeshire Coast National Park. Younger rocks have been lost by subsequent geological processes, the land on which Pembrokeshire is today was established approximately 60 million years ago by a combination of uplift and falling sea levels. The sea cliffs and inland tors that are now a feature of the county were those that were resistant to weathering that has taken place since. The landscape was subject to change as a result of the ice ages over the last several thousand years. About 20,000 years ago the Irish Sea ice sheet deposited areas of clays, while Pembrokeshire is not a seismically active area, two periods of activity were noted in the 19th century. In 1873 there was a shock in the west of the county
9.
Outcrop
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An outcrop or rocky outcrop is a visible exposure of bedrock or ancient superficial deposits on the surface of the Earth. However, in places where the cover is removed through erosion or tectonic uplift. In Finland, glacial erosion during the last glacial maximum, followed by scouring by sea waves, bedrock and superficial deposits may also be exposed at the Earths surface due to human excavations such as quarrying and building of transport routes. Outcrops allow direct observation and sampling of the bedrock in situ for geologic analysis, in situ measurements are critical for proper analysis of geological history and outcrops are therefore extremely important for understanding the geologic time scale of earth history. Outcrops are also important for understanding fossil assemblages, paleo-environment. An outcrop example in California is the Vasquez Rocks, familiar from location shooting use in many films, list of rock formations Geological formation Geologic time scale Media related to Outcrops at Wikimedia Commons
10.
Rock (geology)
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Rock or stone is a natural substance, a solid aggregate of one or more minerals or mineraloids. For example, granite, a rock, is a combination of the minerals quartz, feldspar. The Earths outer solid layer, the lithosphere, is made of rock, rock has been used by mankind throughout history. The minerals and metals found in rocks have been essential to human civilization, three major groups of rocks are defined, igneous, sedimentary, and metamorphic. The scientific study of rocks is called petrology, which is a component of geology. At a granular level, rocks are composed of grains of minerals, the aggregate minerals forming the rock are held together by chemical bonds. The types and abundance of minerals in a rock are determined by the manner in which the rock was formed, many rocks contain silica, a compound of silicon and oxygen that forms 74. 3% of the Earths crust. This material forms crystals with other compounds in the rock, the proportion of silica in rocks and minerals is a major factor in determining their name and properties. Rocks are geologically classified according to such as mineral and chemical composition, permeability, the texture of the constituent particles. These physical properties are the end result of the processes that formed the rocks, over the course of time, rocks can transform from one type into another, as described by the geological model called the rock cycle. These events produce three general classes of rock, igneous, sedimentary, and metamorphic, the three classes of rocks are subdivided into many groups. However, there are no hard and fast boundaries between allied rocks, hence the definitions adopted in establishing rock nomenclature merely correspond to more or less arbitrary selected points in a continuously graduated series. Igneous rock forms through the cooling and solidification of magma or lava and this magma can be derived from partial melts of pre-existing rocks in either a planets mantle or crust. Typically, the melting of rocks is caused by one or more of three processes, an increase in temperature, a decrease in pressure, or a change in composition, igneous rocks are divided into two main categories, plutonic rock and volcanic. Plutonic or intrusive rocks result when magma cools and crystallizes slowly within the Earths crust, a common example of this type is granite. Volcanic or extrusive rocks result from magma reaching the surface either as lava or fragmental ejecta, the chemical abundance and the rate of cooling of magma typically forms a sequence known as Bowens reaction series. Most major igneous rocks are found along this scale, about 64. 7% of the Earths crust by volume consists of igneous rocks, making it the most plentiful category. Of these, 66% are basalts and gabbros, 16% are granite, only 0. 6% are syenites and 0. 3% peridotites and dunites
