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Ireland
Ireland Ireland Ireland is a country in Europe with a coast on the Atlantic Ocean. It is called the Emerald Isle because of its green color. Its people derived mainly from Great Britain. Most of the population is Roman Catholic. The Climate is much like ours. The republic of Ireland covers 83% of its stand with the other 17% containing the country of Northern Ireland. There are twenty-six counties in the Republic with the over-all capitol of Dublin. The six northeastern counties form the county of Northern Ireland which is actually connected to the republic. Northern Ireland is part of the United Kingdom, where as the republic is not. The whole Island was under British rule before 1922. The island containing the Republic of Ireland and Northern Ireland, is separated by the original ruling country of Great Britain by way of the Irish Sea. Ireland is actually a detached fragment from the European Mainland. Most of the country is 500 ft. above sea level. The surface of the country is covered by glacial drift from the Pleistocene ice age. This period left eskers, or long gavel ridges, and drumlins or small hills that were left behind by the glaciers. You can find the start of this belt in the west of the country by Clew Bay. It continues across the country. In the south of Ireland, there is a series of parallel ridges of Devonian sandstone. The ridges rise in elevation westward and lead up to Carrantuohill, the largest mountain in the country. The famous lakes of Killarney are located at that point. The lakes are famous for their scenic beauty. In the southeast of Ireland, granites from the Devonian age makeup the uplands which travel 80 mi. in a northeasterly direction towards the counties of Wexford and Wicklow, reaching the south shore of Dublin Bay. These uplands are glacier modified valleys. Most of the soil in Ireland have been formed of Glacial Drift. Limestone, as around here, is the most common bedrock in Ireland, Making it even more like our area. Gleyed soils are commonly found where there is poor drainage, such as in the north-central lowland. Because of past wetness and acidity, peat has accumulated to form bogs that now cover thousands of acres in the midlands. These bogs are useless for agricultural purposes, but very useful in the source of peat fuel. Peat covers much of the higher hills and supports much vegetation making it actually an indirect importance to agriculture. It also makes good grazing for sheep. The climate of all of Ireland stays mainly as a cool maritime climate. July has average temperatures ranging from 61 degrees in the south, to 57 degrees in the north. Westerly winds that pick up moisture from the warm Atlantic Ocean and drop it first over the weste... This is ONLY a preview of the article. If you would like to view the entire document, you must subscribe to Academic Library. Please register below now!
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