Mauritius like nobody has seen it before

Written by Jérôme Dyment, Dass Bissessur, Christine Deplus on Monday, 02 December 2013. Posted in Cruise 2013

A new bathymetric view of Mauritius Island

Mauritius like nobody has seen it before


While the second leg of cruise Rhum-Rum 2 is on its way, researchers who left at the end of the first leg have started to work on the data collected during this leg. Of particular interest is the bathymetric survey achieved around Mauritius. A preliminary analysis of the raw swath data has been undertaken and the resulting digital elevation model was merged with those resulting from multibeam bathymetric data collected during previous cruises. Together, they reveal a view of Mauritius that nobody has seen so far.

Showing Mauritius as a whole, standing almost 5000 m above the seafloor (4000 m below sea level added to the 828 m of the highest mountain of the island), this new bathymetry offers a much more complete picture of the volcanic edifice than any map or photography limited to the island. Erosion gullies run down the slope from both the east and west coasts. Successive fronts of debris and sediment accumulation are clearly imaged at the foot of the southwestern slope. South of the island, many submarine volcanic edifices continue the N20°E volcanic alignment that cut across the island and produced the most recent "younger series" described by the geologists on land. Volcanic aprons observed east and southwest of the island may represent the "rift zones" which focused the volcanic activity at the origin of the shield volcano.

This preliminary map will be completed by data collected during the second leg. The older data will be reprocessed to achieve a better resolution. Although further work is required to propose a complete interpretation, it is already clear that these data will provide a new vision of Mauritius geological history.

Dass Bissessur, Christine Deplus, and Jerôme Dyment.


Mauritius bathy1



Perspective views of Mauritius from azimuths 150°E (top) and 250°E (bottom), elevation 30°, and vertical exaggeration 2.5. Different bathymetric data show various resolutions: the largest, pale colored pixels correspond to bathymetry derived from satellite altimetry (Smith and Sandwell, Science, 1997), whereas the bright colored pixels correspond to multibeam bathymetry of different resolutions (Magofond 2 (1998), Gimnaut (2000), Forever (2006), Knox11rr (2007), Rhum-Rum 1 (2012), Rhum-Rum 2 (2013)). 


About the Author

Jérôme Dyment

Jérôme Dyment

Directeur de recherche au CNRS, géophysique marine.

Institut de Physique du Globe de Paris

Dass Bissessur

Dass Bissessur is researcher at the Mauritius Oceanography Institute. He is a marine geophysicists and a significant part of his work focuses on the Indian Ocean.

Christine Deplus

Christine Deplus is  researcher at the Institut de Physique du Globe de Paris.

She is marine geophysicists and a significant part of her work focuses on the Indian Ocean.

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