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The South Coast Of Iceland

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The harbour of Heimaey, along the south coast of Iceland is a small town named Vestmannaeyjar with a population of 5400 people. Vestmannaeyjar provides some the of the best fishing areas in the North Atlantic. A loss of this fishing harbour would see a fall in Iceland’s economy (Bullard, 1977). Until mid-January in 1973 the island of Heimaey was considered to be volcanically inactive. The last known eruption of Helgafell was inferred to be 5000 – 6000 years ago. (Bullard, 1977) there was no real warning of Helgafell erupting other than two swarms of earthquakes which began on 21 January 1973 and on 22 January a gale of wind which has raged and left 70 ships in the harbour seeking shelter. The Eruption started in the early morning of 23 January 1973 from a 1600 meter long fissure. The fissure was located 200 meters to the East of the town. The lava flowed away from the town due to favourable morphological conditions. Due to favourable conditions such as the wind blowing west, pyroclastics ejected from the fissure were redirected away from the town. These conditions contributed to the safety of the residents as they were evacuated from the town to safer locations via the stranded ships. (Kolbl, 29 June 1996)
A new edifice began to grow where the eruptive activity were focused at a section of the fissure where fountaining became more energetic. Due to the prevailing winds returning to their seasonal directions and the nearest houses of the town located a short distance away

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