History Coursework Northern Ireland

History Coursework Northern Ireland-78
Mesolithic middle stone age inhabitants arrived some time after 8000 , is the Giant's Ring, a henge monument at Ballynahatty, near [Belfast, which consists of a circular enclosure, 590 feet (200 meters) in diameter, surrounded with an 15 feet (four-meter) high earthwork bank with five entrances, and a small neolithic passage grave slightly off-center.Ireland was organized into a number of independent petty kingdoms, or tuatha (clans), each with an elected king.During the Ice Age, until about 9000 years ago, and most of Ireland was covered with ice. || Mesolithic middle stone age inhabitants arrived some time after 8000 , is the Giant's Ring, a henge monument at Ballynahatty, near [Belfast]], which consists of a circular enclosure, 590 feet (200 meters) in diameter, surrounded with an 15 feet (four-meter) high earthwork bank with five entrances, and a small neolithic passage grave slightly off-center. ]]

Mesolithic middle stone age inhabitants arrived some time after 8000 , is the Giant's Ring, a henge monument at Ballynahatty, near [Belfast, which consists of a circular enclosure, 590 feet (200 meters) in diameter, surrounded with an 15 feet (four-meter) high earthwork bank with five entrances, and a small neolithic passage grave slightly off-center.Ireland was organized into a number of independent petty kingdoms, or tuatha (clans), each with an elected king.During the Ice Age, until about 9000 years ago, and most of Ireland was covered with ice. || Mesolithic middle stone age inhabitants arrived some time after 8000 , is the Giant's Ring, a henge monument at Ballynahatty, near [Belfast]], which consists of a circular enclosure, 590 feet (200 meters) in diameter, surrounded with an 15 feet (four-meter) high earthwork bank with five entrances, and a small neolithic passage grave slightly off-center. ]]

The weather is unpredictable at all times of the year, and although the seasons are distinct, they are considerably less pronounced than in interior Europe or the eastern seaboard of North America.

Average daytime maximums in Belfast are 43.7°F (6.5°C) in January and 63.5°F (17.5°C) in July.

With heavy urbanization and industrialization along the Lagan Valley and both shores of Belfast Lough, it is the largest city in Northern Ireland and the province of Ulster, and the second-largest city on the island of Ireland (after Dublin).

Other cities include Armagh, Londonderry, Lisburn, and Newry.

Northern Ireland covers 5,459 square miles (14,139 square kilometers), about a sixth of the island's total area, or a little larger than the U. Strangford Lough is the largest inlet in the British Isles, covering 150 square kilometers.

Extensive drumlins in Counties Fermanagh, Armagh, Antrim and particularly Down, result from ice coverage for most of the last Ice age.

There are substantial uplands in the Sperrin Mountains (an extension of the Caledonian fold mountains) with extensive gold deposits, granite Mourne Mountains, and basalt Antrim Plateau, as well as smaller ranges in South Armagh and along the Fermanagh–Tyrone border.

None of the hills are especially high, with Slieve Donard in the dramatic Mournes reaching 2782 feet, (848 meters), Northern Ireland's highest point. The whole of Northern Ireland has a temperate maritime climate, rather wetter in the west than the east, although cloud cover is persistent across the region.

The volcanic activity which created the Antrim Plateau also formed the eerily geometric pillars of the Giant's Causeway on the north Antrim coast.

Also in north Antrim are the Carrick-a-Rede Rope Bridge, Mussenden Temple and the Glens of Antrim.

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