Mayotte Volcanoes and Earthquakes: scientific missions
SISMAORE oceanographic campaign
REFMAORE mission in Mayotte
Volcano Week: the MAYOBS15 oceanographic campaign
Results of the MAYOBS 13-1 and 2 oceanographic missions off the coast of Mayotte
Transcript of the video
Mayotte Volcano Mission
After the discovery of a new volcano in Mayotte, in May 2019, an observation network was set up: REVOSIMA. This network brings together several institutes: Ifremer, IPGP, BRGM and several CNRS laboratories. Our aim is to carry out several missions at sea every year, to monitor volcanic activity. We recuperate geophysical and seismic seabed data. The last mission was in August 2019 and we noted that the eruption was continuing and fluids continued to flow off the coast of Petite-Terre. The seismicity continues in Mayotte and the island is being deformed. So it is important to continue these missions. One was programmed for May 2020, aboard the Marion Dufresne. But the Covid crisis led to it being cancelled. We found another solution.
To monitor seismo-volcanic activity, despite present sanitary conditions, we have carried out remote acoustic monitoring using a ship's multi-beam echosounder while monitoring the seismicity on land and at sea with a monitoring campaign, MAYOBS13-1. Data acquisition took place in May, to the east of Mayotte, from Petite-Terre to the active underwater volcano discovered last year. We had two main objectives: the first was to map the seabed to follow the morphological evolution of the relief linked to the new lava flows since the August 2019 mission. Our second objective was to search for fluids or gases rising from the seabed, which can indicate volcanic activity. Each project manager worked from home, in shifts, a first for us. It was a success because we are used to these missions and could count on excellent teams both on land and at sea.
The MAYOBS13-2 campaign enabled us to photograph the seabed and the water column over a surface of 1,500 km2 to the east of Mayotte. A huge quantity of geophysical data was retrieved. This data must now be treated and analysed. We can, however, announce two major results. The first is a change in the morphology of the seabed to the northwest of the volcano discovered in May 2019, 50 km from Mayotte. We interpret this to be a new flow. The volcanic eruption thus continued after the last oceanographic campaign in August 2019. The second result is the presence of two new acoustic plumes that indicate the emission of fluids or gases from an old volcanic structure a dozen kilometres from Petit-Terre, at the drip line of the present main seismic swarm. These observations must now be carefully analysed and added to other data, such as the seismic data recuperated during the MAYOBS13-1 campaign. Thank you to all those who helped to obtain these results. Take care of yourselves.