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Geologic Formation Attractions In Iceland

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Iceland is a Nordic island country in the North Atlantic, with a population of 348,580 and an area of 103,000 km2 , making it the most sparsely populated country in Europe. The capital and largest city is Reykjavík. Reykjavík and the surrounding areas in the southwest of the country are home to over two-thirds of the population. Iceland is volcanically and geologically active. The interior consists of a plateau characterised by sand and lava fields, mountains, and glaciers, and many glacial rivers flow to the sea through the lowlands. Iceland is warmed by the Gulf Stream and has a temperate climate, despite a high latitude just outside the Arctic Cir...
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Geologic Formation Attractions In Iceland

  • 1. Dyrholaey Vik
    Dyrhólaey , formerly known by seamen as Cape Portland, is a small promonotory located on the south coast of Iceland, not far from the village Vík. It was formerly an island of volcanic origin, which is also known by the Icelandic word eyja meaning island. The peninsula has an elevation of 120 feet , and the Dyrhólaey lighthouse sits at the top of the formation facing the sea. The view from Dyrhólaey is broad: To the north is to be seen the big glacier Mýrdalsjökull. To the east, the black lava columns of the Reynisdrangar come out of the sea, and to the west the whole coastline in the direction of Selfoss is visible - depending on weather conditions. In front of the peninsula, there is a gigantic black arch of lava standing in the sea, which gave the peninsula its name .In the summer...
    From Wikipedia, the free encyclopedia.
  • 2. Laki Craters Kirkjubaejarklaustur
    Laki or Lakagígar is a volcanic fissure in the south of Iceland, not far from the volcanic fissure of Eldgjá and the small village of Kirkjubæjarklaustur. The fissure is properly referred to as Lakagígar, while Laki is a mountain that the fissure bisects. Lakagígar is part of a volcanic system centered on the volcano Grímsvötn and including the volcano Thordarhyrna. It lies between the glaciers of Mýrdalsjökull and Vatnajökull, in an area of fissures that run in a southwest to northeast direction. The system erupted violently over an eight-month period between June 1783 and February 1784 from the Laki fissure and the adjoining volcano Grímsvötn, pouring out an estimated 42 billion tons 14 km3 of basalt lava and clouds of poisonous hydrofluoric acid and sulfur dioxide compounds ...
    From Wikipedia, the free encyclopedia.
  • 6. Hoffellsjokull Glacier Hofn
    Hoffellsjökull is an outlet glacier which flows from the ice cap of Vatnajökull. It is located in the municipality of Hornafjörður, southeast Iceland. Hoffellsjökull takes its name from Hoffell; a mountainous area and a farmland. Hoffellsjökull and the Hoffell area are a part of Vatnajökull National Park.
    From Wikipedia, the free encyclopedia.
  • 11. Myrdalsjokull Glacier Vik
    Mýrdalsjökull is an ice cap in the south of Iceland. It is to the north of Vík í Mýrdal and to the east of the smaller ice cap Eyjafjallajökull. Between these two glaciers is Fimmvörðuháls pass. Its peak reaches 1,493 m in height and in 1980 it covered an area of 595 km2 . The icecap of the glacier covers an active volcano called Katla. The caldera of the volcano has a diameter of 10 km and the volcano erupts usually every 40–80 years. The last eruption took place in 1918. Scientists are actively monitoring the volcano, particularly after the eruption of nearby Eyjafjallajökull began in April 2010. Since the year 930, 16 eruptions have been documented. The Eldgjá, a volcanic eruption fissure about 30 km long, which erupted in the year 936, is part of the same volcanic system. ...
    From Wikipedia, the free encyclopedia.

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