News

Montserrat: “MVO Director Stewart fixes UK Guardian, Express newspapers misrepresentation”

It wouldn’t be the first time that UK Newspapers have distorted and published information that turned out unfavourable and detrimental to the Island.

Here MVO director sets the record straight.

Publication of articles like this with this kind of information, is reminiscent of 1997-8 when the UK Government authorities broadcasted and said that there might be a cataclysmic eruption that would cause Montserrat to completely evacuated. The result of that in spite of vehement denial of that situation from the Government and scientists on Montserrat, it was not until 2008 the UK relented on the misinformation.

Very cleverly written, if not with some dishonesty. If one doesn’t read carefully, you will miss that Professor Neuberg is not the one saying, ‘Sadly, Montserratians must continue to wait.’

Statement on the Status of the Soufrière Hills Volcano, Montserrat (Director, Roderick Stewart)

Following the publication on 7 March 2018 of two articles in UK newspapers (The Guardian and The Express), members of the public have expressed concerns about the current status of the Soufrière Hills Volcano, Montserrat (SHV), particularly with reference to ground deformation. Monitoring data recorded and interpreted by Montserrat Volcano Observatory (MVO) shows no changes that suggest that new activity is imminent. The newspaper articles are misleading and, in the case of The Express, alarmist.

Since the end of the last phase of lava extrusion on 11 February 2010, MVO has observed a slow, steady movement of the ground surface across the whole of Montserrat using data recorded by our network of very precise Global Positioning System (GPS) receivers. The news articles in question report on research being carried out by MVO in collaboration with Professor Jurgen Neuberg (University of Leeds, UK) that seeks to understand this trend. The research suggests that, since February 2010, the underground magma system that feeds the SHV has been slowly recharged by the influx of magma at depth. This causes the pressure inside the system to increase, which is then seen as upwards and outwards movement of the ground surface around the volcano.

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