Ireland

Location of Ireland within the continent of Europe

300px Map of Ireland

Flag Description of Ireland:The flag of Ireland was officially adopted on January 21, 1919. dot Modeled after the French Tricolore, Ireland's flag uses color to symbolize religions. Green is representative of Catholics; orange is representative of Protestants, and the white is symbolic of the union of both.

Wars of ancient history were about possessions, territory, power, control, family, betrayal, lover's quarrel, politics and sometimes religion. But we are in the Modern era and supposedly more educated and enlightened . Think about this. Don't just brush off these questions. Why is RELIGION still involved in WARS? Isn't religion supposed to be about PEACE? Ask yourself; What religion always campaign to have its religious laws be accepted as government laws, always involved in wars and consistently causing WARS, yet insists that it's a religion of peace? WHY?? There are only two kinds of people who teach tolerance: The Bullies. They want you to tolerate them so they can continue to maliciously deprive you. Do not believe these bullies teaching tolerance, saying that it’s the path to prevent hatred and prejudice. The victims who are waiting for the right moment to retaliate. They can’t win yet, so they tolerate.

Official name Éire (Irish); Ireland1 (English)
Form of government unitary multiparty republic with two legislative houses (Senate [602]; House of Representatives [166])
Head of state President: Michael D. Higgins
Head of government Prime Minister: Enda Kenny
Capital Dublin
Official languages Irish; English
Official religion none
Monetary unit euro (€)
Population (2013 est.) 4,594,000COLLAPSE
Total area (sq mi) 27,133
Total area (sq km) 70,273
Urban-rural population

Urban: (2011) 62%

Rural: (2011) 38%

Life expectancy at birth

Male: (2012) 77.5 years

Female: (2012) 82.6 years

Literacy: percentage of population age 15 and over literate

Male: 100%

Female: 100%

GNI per capita (U.S.$) (2012) 38,970

1As provided by the constitution.

2Includes 11 nonelective seats.

Background of Ireland

Celtic tribes arrived on the island between 600 and 150 B.C. Invasions by Norsemen that began in the late 8th century were finally ended when King Brian BORU defeated the Danes in 1014. Norman invasions began in the 12th century and set off more than seven centuries of Anglo-Irish struggle marked by fierce rebellions and harsh repressions. The Irish famine of the mid-19th century saw the population of the island drop by one third through starvation and emigration. For more than a century after that the population of the island continued to fall only to begin growing again in the 1960s. Over the last 50 years, Ireland's high birthrate has made it demographically one of the youngest populations in the EU. The modern Irish state traces its origins to the failed 1916 Easter Monday Uprising which touched off several years of guerrilla warfare resulting in independence from the UK in 1921 for 26 southern counties; six northern counties remained part of the UK. Unresolved issues in Northern Ireland erupted into years of violence known as the "Troubles" that began in the 1960s. The Government of Ireland was part of a process along with the UK and US Governments that helped broker what is known as The Good Friday Agreement in Northern Ireland in 1998. This initiated a new phase of cooperation between Irish and British governments. Ireland was neutral in World War II and continues its policy of military neutrality. Ireland joined the European Community in 1973 and the Eurozone currency union in 1999. The economic boom years of the Celtic Tiger (1995-2007) saw rapid economic growth, which came to an abrupt end in 2008 with the meltdown of the Irish banking system. Today the economy is recovering, fueled by large and growing foreign direct investment, especially from US multi-nationals.

Ireland, Irish Éire, country of western Europe occupying five-sixths of the westernmost island of the British Isles.

The magnificent scenery of Ireland’s Atlantic coastline faces a 2,000-mile- (3,200-km-) wide expanse of ocean, and its geographic isolation has helped it to develop a rich heritage of culture and tradition that was linked initially to the Gaelic language. Washed by abundant rain, the country’s pervasive grasslands create a green-hued landscape that is responsible for the popular sobriquet Emerald Isle. Ireland is also renowned for its wealth of folklore, from tales of tiny leprechauns with hidden pots of gold to that of the patron saint, Patrick, with his legendary ridding the island of snakes and his reputed use of the three-leaved shamrock as a symbol for the Christian Trinity. But while many may think of Ireland as an enchanted land, the republic has been beset with perennial concerns—emigration, cultural and political identity, and relations with Northern Ireland (comprising the 6 of Ireland’s 32 counties within the province of Ulster that remain part of the United Kingdom). At the beginning of the 21st century, however, Ireland’s long-standing economic problems were abating, owing to its diverse export-driven economy; however, calamity struck again in 2008 when a new financial and economic crisis befell the country, culminating in a very costly bailout of the Irish economy by the European Union and the International Monetary Fund.

The emergence of Ireland as an independent country is a fairly recent phenomenon. Until the 17th century, political power was widely shared among a rather loosely constructed network of small earldoms in often-shifting alliances. Following the so-called “Flight of the Earls” after an unsuccessful uprising in the early 17th century, Ireland effectively became an English colony. The island was an integral part of the United Kingdom from 1800 to 1922, when, by virtue of the Anglo-Irish Treaty of December 6, 1921, the Irish Free State was established as a self-governing dominion of the British Empire. Independence came in 1937, but Ireland remained a member of the British Commonwealth until 1948. Since then, Ireland has become integrated with the rest of western Europe, joining the European Union in 1987, though the country generally retained a neutral role in international affairs. In 2008 Ireland became an impediment to the enactment of the Lisbon Treaty—an agreement aimed at streamlining the EU’s processes and giving it a higher international profile—when the Irish voted against the passage of the treaty in a national referendum. The treaty, however, was approved by Irish voters in a second referendum, held the following year.

Dependent on agriculture and subject to extremes of climate, Ireland was long among Europe’s poorest regions, a principal cause of mass migration from Ireland, especially during the cycle of famine in the 19th century. Some 40 million Americans trace their ancestry to Ireland as a result of that traumatic exodus, as do millions of others throughout the world. Every year members of this diaspora visit their ancestral homeland and forge connections with long-lost family.

Ireland’s capital is Dublin, a populous and affluent city whose metropolitan area is home to more than one-fourth of the country’s total population. The city’s old dockside neighbourhoods have given way to new residential and commercial development. Cork, Ireland’s second largest city, is a handsome cathedral city and port in the southwest. Other principal centres include Waterford, Wexford, and Drogheda on the east coast, Sligo in the northwest, and Limerick and Galway in the west.

Although Ireland is now both urbanized and Europeanized, its culture retains many unique characteristics, and its people prize folkloric and social traditions that largely derive from and celebrate the country’s rural past. In “Meditations in Time of Civil War” William Butler Yeats, perhaps Ireland’s best-known poet, evokes the idyllic and idealized countryside, a place central to the memories of the country’s millions of expatriates and their descendants:

An acre of stony ground,

Where the symbolic rose can break in flower,

Old ragged elms, old thorns innumerable,

The sound of the rain or sound

Of every wind that blows;

The stilted water-hen

Crossing stream again

Scared by the splashing of a dozen cows.

Geography of Ireland

The Land

The republic of Ireland occupies the greater part of an island lying to the west of Great Britain, from which it is separated—at distances ranging from 11 to 120 miles (18 to 193 km)—by the North Channel, the Irish Sea, and St. George’s Channel. Located in the temperate zone between latitudes 51°30′ and 55°30′ N and longitudes 6°00′ and 10°30′ W—as far north as Labrador or British Columbia in Canada and as far west as the West African state of Liberia—it constitutes the westernmost outpost of the Atlantic fringe of the Eurasian landmass. Ireland, which, like Great Britain, once formed part of this landmass, lies on the European continental shelf, surrounded by seas that are generally less than 650 feet (200 metres) deep. The greatest distance from north to south in the island is 302 miles (486 km), and from east to west it is 171 miles (275 km).

Relief

The territory of the republic consists of a broad and undulating central plain underlain by limestone. This plain is ringed almost completely by coastal highlands, which vary considerably in geologic structure. The flatness of the central lowland—which lies for the most part between 200 and 400 feet (60 and 120 metres) above sea level—is relieved in many places by low hills between 600 and 1,000 feet (180 to 300 metres) in elevation. With many lakes, large bog areas, and low ridges, the lowland is very scenic. The principal mountain ranges are the Blue Stack Mountains in the north, the Wicklow Mountains in the east (topped by Lugnaquillia, at 3,039 feet [926 metres]), the Knockmealdown and Comeragh mountains in the south, the Macgillycuddy’s Reeks in the southwest, and the Twelve Pins in the west. Carrantuohill, at 3,414 feet (1,041 metres) in the Macgillycuddy’s Reeks, is the highest point in the republic. In the west and southwest the wild and beautiful coast is heavily indented where the mountains of Donegal, Mayo, Galway, and Kerry thrust out into the Atlantic, separated by deep wide-mouthed bays, some of which—Bantry Bay and Dingle Bay, for example—are, in fact, drowned river valleys. By contrast, the east coast is little indented, but most of the country’s trade passes through its ports because of their proximity to British and Continental markets.

The coastal mountain fringe illustrates the country’s complex geologic history. In the west and northwest as well as in the east, the mountains are composed mainly of granite. Old Red Sandstone predominates in the south, where the parallel folded mountain ridges trend east-west, separated by limestone river valleys. Ireland experienced at least two general glaciations—one covering most of the country and the other extending as far south as a line linking Limerick, Cashel, and Dublin—and the characteristic diversity of Irish scenery owes much to this glacial influence. The large areas of peat bog to be found throughout the country are a notable feature of the landscape.

Drainage

The rivers that rise on the seaward side of the coastal mountain fringe are naturally short and rapid. The inland streams, however, flow slowly, often through marshes and lakes, and enter the sea—usually by way of waterfalls and rapids—long distances from their sources. The famed River Shannon, for example, rises in the plateau country near Sligo Bay and flows sluggishly south-southwestward for some 160 miles (260 km), reaching tidewater level at Limerick and draining a wide area of the central lowland on its way. Other major inland rivers—some of them renowned for their salmon fisheries—are the Slaney, Liffey, and Boyne in the east; the Nore, Barrow, and Suir in the southeast; the Blackwater, Lee, and Bandon in the south; and the Clare and the Moy in the west. Because of the porosity of the underlying Carboniferous limestones, an underground drainage system has developed, feeding the interlacing surface network of rivers and lakes. The government has implemented major arterial drainage projects, preventing flooding—and making more land available for cultivation—by improving the flow of water in the rivers and thereby lowering the levels of lakes. There are also state-aided farm-drainage schemes designed to bring wasteland and marginal land into production.

Soils

Most Irish soils originate from drift, the ice-scoured waste formerly frozen to the base of the advancing glaciers. Some older rocks in the country’s geologic formation—quartzites, certain granites, and shales—weather into infertile and unproductive soils. In many places, however, these have been overlaid by patches of the ice-borne drift, mostly limestone-bearing, which are farmed with considerable success. The bare limestone regions remaining in western areas show how much glacial drift cover has meant to the Irish agricultural economy.

Climate

Ireland’s climate is classified as western maritime. The predominant influence is the Atlantic Ocean, which is no more than 70 miles (113 km) from any inland location. The mild southwesterly winds and warm waters of the North Atlantic Current contribute to the moderate quality of the climate. Temperature is almost uniform over the entire island. Average air temperatures lie mainly between limits of 39 and 45 °F (4 and 7 °C) in January and February, the coldest months of the year. In July and August, the warmest months, temperatures usually range between 57 and 61 °F (14 and 16 °C), although occasionally considerably higher readings are recorded. The sunniest months are May and June, when there is sunshine for an average duration of 5.5 and 6.5 hours a day, respectively, over most of the country, and the ancient patchwork of fields and settlements making up the landscape glows under a clear, vital light. Average annual precipitation varies from about 30 inches (760 mm) in the east to more than 100 inches (2,533 mm) in the western areas exposed to the darkening clouds that often come sweeping in from the Atlantic. The precipitation, combined with the equable climate, is particularly beneficial to the grasslands, which are the mainstay of the country’s large livestock population. Snow is infrequent except in the mountains, and prolonged or severe snowstorms are rare.

Plant and animal life

Ireland was almost completely covered by glaciers during the Ice Age, and its plant and animal life are thus mainly—but not entirely—the result of the subsequent migration of species from other areas. As long as there was a land connection between Ireland and what was to become the rest of the British Isles, most species arrived overland from northern Europe. Irish plant and animal life nevertheless possess certain unique features owing partly to climatic conditions and partly to the fact that Ireland became separated from Britain by the Irish Sea sometime before Britain itself became separated from the European continent.

Disclaimer

This is not the official site of this country. Most of the information in this site were taken from the U.S. Department of State, The Central Intelligence Agency, The United Nations, [1],[2], [3], [4], [5],[6], [7], [8], [9], [10], [11], [12], [13], [14],[15], [16], [17], [18], [19], [20], [21], [22], [23], [24],[25], [26], [27], [28], [29], [30],[31], [32], [33], [34], and the [35].

Other sources of information will be mentioned as they are posted.