3552 x 5344 px | 30,1 x 45,2 cm | 11,8 x 17,8 inches | 300dpi
Data acquisizione:
2006
Ubicazione:
Little Rann of Kutch, Bhuj Gujarat India
Altre informazioni:
The Giant's Causeway is an area of 40, 000 interlocking basalt columns resulting from a volcanic eruption. It is located about 2 miles (3 km) north of the town of Bushmills in County Antrim, Northern Ireland along the northeast coast of Ireland. It was declared a World Heritage Site by UNESCO in 1986, and a National Nature Reserve in 1987 (by the Department of the Environment for Northern Ireland). In a 2005 poll of Radio Times readers, Giant's Causeway was named as the fourth greatest natural wonder in the United Kingdom. It's the centerpoint of many famous photos, notably the cover of the Led Zeppelin album Houses of the Holy. The Giant's Causeway is owned and managed by the National Trust. The tops of the columns form stepping stones that lead from the cliff foot and disappear under the sea. Most of the columns are hexagonal, however there are some with four, five, seven and eight sides. The tallest are about 12 metres (36 ft) high, and the solidified lava in the cliffs is 28 metres thick in places. Contents Legend has it that the Irish giant Fionn mac Cumhail (Finn McCool) built the causeway to walk to Scotland to fight his Scottish counterpart Benandonner. One version of the legend tells that Finn McCool fell asleep before he got to Scotland. When he didn't arrive, the much larger Benandonner crossed the bridge looking for him. To protect Fionn, his wife Oonagh laid a blanket over Fionn and pretended he was actually Fionn's baby son (in a variation, Fionn fled after seeing Benandonner's great bulk, and asked his wife to disguise him as the baby.) In both versions, when Benandonner saw the size of the 'infant', he assumed the alleged father, Fionn, must be gigantic indeed. Therefore, Benandonner fled home in terror, ripping up the Causeway in case he was followed by Fionn. The Scottish side of the causeway on the isle of Staffa has similar basalt formations at the site of Fingal's Cave that are part of the same ancient lava flow.
