Ireland is a country in europe
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Ireland
Ireland
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Island, New Caledonia.
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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. It was formally incorporated into the United Kingdom in 1801. A 1914 Home Rule Act was passed but never implemented due to pro-union militancy in the north, the onset of World War I, and the subsequent Irish War of Independence. In 1920 the island was effectively partitioned with the creation of Northern Ireland, a six-county area with devolved powers within the United Kingdom, whereas under the Anglo-Irish Treaty of December 6, 1921, the other 26 counties became the Irish Free State, a self-governing dominion within the British Commonwealth and Empire. In 1937 the southern state passed a new constitution that offered a more robust expression of sovereignty, and in 1949 it formally left the Commonwealth as the Republic of Ireland.
Since then Ireland has become integrated with the rest of western Europe. It joined the European Economic Community (forerunner of the EU) in 1973. 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.
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Irish people
Irish people
Overview of the people of Ireland, with a focus on the impact of the mass emigration to the United States during the 19th century.
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Dependent on agriculture, 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.
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.
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