http://uanews.org/cgi-bin/WebObjects/UANews.woa/8/wa/SRStoryDetails?ArticleID=11813
Could this thing possibly be a fresh volcanic dike of uprising water/ammonia
ice (like the light-colored dome Huygens imaged that seems to be surrounded
by geothermal methane springs)? If so, however, it must have cooled off by
now.
Its been ruled out as a hotspot, but surely upwelling/cryovolcanism seems the most likely process to have brought any 'different materials' to the surface.
Perhaps there could be some unusual precipitation occuring?
Unfortunately, none of Cassini's flybys during the primary mission will allow any radar mapping of it, except for one that MIGHT allow SAR imaging if fairly extreme side-looking is used. It's a safe bet that this will be one of the prime targets during the extended mission.
It could be anything else. For instance a "threshold" in altitude, from a volcanic cardeira or meteor impact, could be made visible by high altitude snow. What kind of snow, I wonder, there are many candidates, in the list of hydrocarbons.
Maybe if we look among the simple hydrocarbons, the one with the adequate fusion temp, and get its infrared spectra...
It could be also the result of a local snow storm or hail storm. In a previous discution it was sait that, due to the low heat input into the Titan system, and the scarcity of fluids (mainly methane) there could be only a very dry weather with, from times to times, very violent rain falls. Eventually there could be localized hail or snow storms, which result could be still visible years after, as the snow or hail melts only very slowly. But these ices or snows cannot be methane, which cannot freeze on Titan, so it may be something else, eventually more or less mixed with methane.
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