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Hekla, Katla, Krafla, Vestmanneyjar, Krafla, Askja, Grímsvötn, Eyjafjallajökull, Öræfajökull, Bárðarbunga, Snæfellsjökull and Kverkfjöll to name a few.
Krafla volcano in Iceland is formed due to the movement of the North American and Eurasian tectonic plates, which intersect along the Mid-Atlantic Ridge. This movement creates volcanic activity as magma rises to the surface, leading to the formation of the Krafla volcanic system. The volcano has a history of both explosive eruptions and effusive lava flows.
Even if its a volcano everything around it or most of it is ice,snow and mountains.
Mount Krafla, located in Iceland, is a volcanic system that has been active for approximately 2.4 million years. The most significant eruptive activity occurred in the 18th century, particularly between 1724 and 1729, and again from 1975 to 1984. The age of the current volcanic features, including the caldera and craters, is much younger, formed during these more recent eruptions.
The name of Mt. Krafla was extended over the high temperature area after the geothermal power station was built in 1974. The colourful mountain Leirhnjukur is situated at the southern end of the 40 km long and 15 km wide eruptive area, Gjastykki, which erupted 9 times between 1975 and 1984. The average depth of the boreholes feeding the power station is 2000 m. They are lined with pipes down to 700 - 1000 m to prevent collapsing. The steam pressure from the separators in the grey building equals 7,7 bars when it is pipelined to the generators in the red building. The output is about 70 MW and the power station is directly connected to the national grid. At the onset of the so-called Myvatn fires 1724 -1729 the explosion crater Viti (Hell) was created. Because of the latest Myvatn fires, 1975 - 1984, and the consequent plate tectonics the boreholes caved in and prevented the operation of the power station until 1979. East of it and south of Mt. Krafla is the obsidian ridge, Hrafntinnuhryggur. The Krafla- and Leirhnjukur areas offer various hiking possibilities through unique and unbelievable landscapes.
Geothermal energy
Europe is a continent, not a country. Japan is a country, in the continent of Asia.Europe is a continent, not a country. Japan is a country, in the continent of Asia.Europe is a continent, not a country. Japan is a country, in the continent of Asia.Europe is a continent, not a country. Japan is a country, in the continent of Asia.Europe is a continent, not a country. Japan is a country, in the continent of Asia.Europe is a continent, not a country. Japan is a country, in the continent of Asia.Europe is a continent, not a country. Japan is a country, in the continent of Asia.Europe is a continent, not a country. Japan is a country, in the continent of Asia.Europe is a continent, not a country. Japan is a country, in the continent of Asia.Europe is a continent, not a country. Japan is a country, in the continent of Asia.Europe is a continent, not a country. Japan is a country, in the continent of Asia.
To seperate the country from its neighbory country
Spain is a country ^-^ it can be located near France and Portugal.
You do not have to be from the country to date a country girl.
basically a country can control another country by spreading their culture in the foreign country. If country A has a large of effect by the culture and ideas of country B, then we can say that country B controls country A socially.