Throughout my time at BGS I was very lucky to be involved in some fascinating and exciting projects. Many of the projects I contributed to involved writing reports and compiling databases, as well as analysing data and conducting research. Most of this work will be used to advise the UK and overseas governments as well as inform and help observatories and other geological surveys that monitor volcanoes and record their hazards and impacts on a regional and worldwide scale. The work involved research along the whole spectrum of Volcanology, from the physical processes that trigger eruptions, and the parameters that control them, to applied volcanology - studying the hazards, risk and impacts on populations, aviation and infrastructure. Below are some highlights from my time at BGS:
As part of an ongoing project assessing potential volcanic hazards on Ascension Island, I was heavily involved in calculating and modelling the potential of re-suspended ash as a volcanic hazard on Ascension (a UK Overseas Territory). Volcanic ash can lie present on and around eruption sites for days, weeks or years, depending on the size of the eruption and volume of extruded ash and tephra. ‘Clean-up’ operations can be disrupted by the entrainment of volcanic ash and can take people and officials by surprise. It is often overlooked as a volcanic hazard as the volcanic activity has ceased. Models considered a number of parameters for ash to be re-suspended and re-entrained into the atmosphere, ultimately posing a threat to public health, infrastructure and aviation. I also plotted wind direction data on rose diagrams to determine the areas of the island that would most likely be affected by re-suspended ash (if the issue were to ever arise on Ascension Island…)
|Ascension Island, photograph by Charlotte Vye-Brown
I compiled an extensive database on the eruptive parameters of Mt. Sinabung in Indonesia since it’s almost continuous eruption starting in 2010, after lying dormant for ~400 years. With the exception of three eruptive hiatus’, (the longest lasting little under three years), it has remained in an unrestful and eruptive state, continuing to extrude large volumes of volcanic ash, tephra and lava and induce pyroclastic density currents, lahars and many other hazardous flows. This involved me studying weekly reports from multiple sources from the past 6 years. I then extracted geological (plume height, shape and colour; ash dispersal distance and direction; lava dome growth; deformation etc.) and volcanic impact (alert level changes, geographic areas impacted, evacuation status etc.) data from the reports and compiled a database. From this, I wrote a report to compare a number of eruptive parameters to see if a correlation between the data sets exists. The information, graphs and database will be used for a detailed report and publication on the eruptive source parameters of Mt. Sinabung.
|Mt Sinabung in 2010.