Mapping volcanic heat on Io

Jun 11, 2012 By Priscilla Vega and Jia-Rui C. Cook
Thermal emission from erupting volcanoes on the jovian moon, Io. A logarithmic scale is used to classify volcanoes on the basis of thermal emission: the larger the spot, the larger the thermal emission. Credit: NASA/JPL-Caltech/Bear Fight Institute

(Phys.org) -- A new study finds that the pattern of heat coming from volcanoes on Io's surface disposes of the generally-accepted model of internal heating.  The heat pouring out of Io's hundreds of erupting volcanoes indicates a complex, multi-layer source.  These results come from data collected by NASA spacecraft and ground-based telescopes and appear in the June issue of the journal Icarus

A map of hot spots, classified by the amount of heat being emitted, shows the global distribution and wide range of volcanic activity on .  Most of Io's eruptions dwarf their contemporaries on Earth.

"This is the most comprehensive study of Io's volcanic thermal emission to date," said Glenn Veeder of the Bear Fight Institute, Winthrop, Wash., who led the work of a multi-faceted team that included Ashley Davies, Torrence Johnson and Dennis Matson of NASA's Jet Propulsion Laboratory, Pasadena, Calif., Jani Radebaugh of Brigham Young University, in Provo, Utah, and David Williams of Arizona State University, Tempe, Ariz.  The team examined data primarily from the NASA's Voyager and Galileo missions, but also incorporated infrared data obtained from telescopes on Earth.  

"The fascinating thing about the distribution of the heat flow is that it is not in keeping with the current preferred model of tidal heating of Io at relatively shallow depths," said Davies.  "Instead, the main thermal emission occurs about 40 degrees eastward of its expected positions." 

"The pattern that emerges points to a complex heating process within Io," said Matson.  "What we see indicates a mixture of both deep and shallow heating."

A mystery has also emerged.  The team found that active volcanoes accounted for only about 60 percent of Io's heat.  This component mostly emanates from flat-floored volcanic craters called paterae, a common feature on Io.  But where is the "missing" 40 percent?  "We are investigating the possibility that there are many smaller volcanoes that are hard, but not impossible, to detect," said Veeder. "We are now puzzling over the observed pattern of heat flow." 

Understanding this will help identify the tidal heating mechanisms not only within Io, but also may apply to neighboring Europa, a high-priority target for NASA in its search for life beyond Earth. 

Explore further: Computer simulation suggests early Earth bombarded by asteroids and comets

More information: solarsystem.nasa.gov/galileo/

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HannesAlfven
1 / 5 (4) Jun 11, 2012
It's important to note that Galileo's camera was saturated while observing a discharge on Io. Lava flows do not ordinarily saturate cameras, which should lead us to wonder at the inference that these are volcanos, to begin with. An electrical plasma discharge -- in the arc mode -- would, however, be expected to saturate cameras.
aironeous
1 / 5 (2) Jun 12, 2012
nuclearplanet.com it's a nuclear core.