Views on the Future of Montserrat. There were many primary impacts of the volcanic eruption that occurred on Montserrat in 1997. Large areas were covered with volcanic material;

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September 24th 1977

Report to British Government              

Views on the future of Montserrat

In July 1995, the dormant volcano known as the Soufriere Hills’ volcano showed some signs of small eruptions. On  18th July 1995, thousands were forced to evacuate and temporarily reside in the so-called “safe areas” or flee to neighboring Caribbean islands, New York and Britain. In August, the government declared a state of Emergency. Approximately four months later, Britain offered their help to assist with rehabilitation programs. Not only did they help in this way but they also granted millions of pounds to help aid development of the victimized island. In April 1996, the British government settled on granting Montserratians residency and the right to work in the UK for up to two years.  On June 25th 1997, the Soufriere Hills’ Volcano finally erupted, releasing 4.5 million metres cubed of rocks and gas and also killing a total of 19 people (even after evacuation). Two-thirds of the island was left uninhabitable and Plymouth, the capital, was abandoned. Montserrat's airport was declared closed; the island was accessible only by helicopter or boat.

The eruption was explained to have many causes, which could all be agreed on. Montserrat is right above a destructive plate margin. A destructive plate margin is basically where two plates are moving towards each other. It is when an oceanic plate meets a continental plate; the denser oceanic plate is then forced down into the mantle. Then small Earthquakes occur due to friction. The denser plate melts in the subduction zone due to the friction and increase in temperature.  The oceanic crust melts and rises and causes explosive volcanoes. This is what is meant by destructive plate margins. In Montserrat’s case, the Atlantic plate acted as the oceanic plate and was forced under the Caribbean plate. Magma eventually rose up through weak points under the Soufriere Hills, forming an “underground pool of magma”.  The rock above the “pool of magma” had collapsed opening a vent big enough to cause an eruption.

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There were many primary impacts of the volcanic eruption that occurred on Montserrat in 1997. Large areas were covered with volcanic material; the capital city of Plymouth was buried under 12 metres of mud and ash. Secondly, over 20 villages and two thirds of homes on the island were destroyed by pyroclastic flows which are fast-moving clouds of super-heated gas and ash.  Also, most of the schools, hospitals, airports and the ports were destroyed. Lastly, vegetation and farmland were destroyed as well.  The immediate responses were that people were evacuated from the South (Plymouth) to safe areas in the ...

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