Volcanic resurfacing of Io between Galileo and New Horizons Observations

Mathematics – Logic

Scientific paper

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[5480] Planetary Sciences: Solid Surface Planets / Volcanism, [6218] Planetary Sciences: Solar System Objects / Jovian Satellites, [6219] Planetary Sciences: Solar System Objects / Io

Scientific paper

Io is the most geologically active object in our solar system. Due to its tumultuous volcanism, determining Io's resurfacing rate will allow better characterization of the subsurface structure, thermal state, and history of tidal heating of this small moon. Numerous active volcanic centers were documented during the Galileo mission in the late 1990's and early 2000's, and the opportunity to discover more of these centers was presented with the flyby of New Horizons in 2007. Previous authors (i.e. Spencer et al. 2007) have compared Galileo SSI and New Horizons LORRI images with similar viewing geometry, and have found multiple new potential features such as dark lava flows and bright plume deposits emplaced between the two flybys. The purpose of this study was to measure the extent of these changes on Io. Because an ISIS camera model does not yet exist for LORRI, a direct ratio image for comparison with the Galileo SSI images could not be created. By changing the stretch of the Galileo SSI images to match those of New Horizons as closely as possible, we were able to create a rough ratio image for the active center locations. We used these ratio images to measure the areal extent of the new deposits, taking careful precautions to measure more changes in shape than brightness, as brightness variations can be caused by certain surface materials being viewed at different phase angles between the Galileo and New Horizons flybys. This presentation will report our measurement findings. We then are able to use our measurements of the total area covered by new volcanic features to make estimates of the resurfacing rate of Io. Spencer, J.R. et al. (2007), Io Volcanism Seen by New Horizons: A Major Eruption of the Tvashtar Volcano, Science, 318, 240, DOI:10.1126/science.1147621.

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