Volcanic activity on IO

Volcanic activity on Io

SHARK-VIS observations of the Io surface will allow us to monitor the evolution and characterize the intense activity of many of its volcanic systems, which provides clues on the internal structure of the satellite.

Details. Io is the most volcanically active body in our Solar System. Having studied Io through multiple spacecraft encounters and ground-based monitoring for 40 years, we are now moving from a basic understanding of Io's volcanism to investigations of greater significance, concerning internal structure, volcanic advection, and temporal evolution. Ground-based monitoring programs observing in the M-band have been gradually filling in this picture. Resolution for these programs on 8-10 meter telescopes is about 500 km on Io’s surface. SHARK-VIS will provide a much higher resolution around 50 km, which will enable us to monitor the Io surface in great detail  and identify areas of volcanic activity by changes in surface albedo or color, so as to study the effects induced by volcanic activity. In addition, visible wavelength observations will be able to detect the highest temperature features that are sufficiently bright in nighttime or eclipse images or even in daylight, to reveal volcanic plumes against the blackness of space by both forward- and backscattered light, and to identify the style of eruption (lava flow as opposed to lava lake, for example) for many volcanic systems.

Io image taken by the Galileo spacecraft (credits: NASA).