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In responce to the Aproaching Iapetus thread (which I have found fascinating & Vogon13 has made it more so with his / her insights & knowledge, I would like to start something on the three different moons of Uranus. <br /><br />Please note that the Uranian system at the time was observed Pole On by the Voyager 2 spacecraft, as the tipped over Uranus system was close to a 'solstice'. <br /><br />This is really for those interested in Planetary Science. <br /><br />1). Does anyone think that Miranda was smashed to pieces than reassembled over time?? Miranda similar in size to the Saturn moons Mimas & Enceladus & appears to be a love child of them both. Sizewise, Miranda is in between them.<br /><br />2). I think not as the surface although jumbled does have a large primitive area & large ordered tectonic faults. Circular 'racetracks' due to former co-orbital moons smashing into Miranda or tidal heating in the remote past (cryovolcanics)? <br /><br />Cryovocanoes erupt slushy ice which then freezes solid, not molten rock as on Earth, Io, Venus, etc. <br /><br />3). Does anyone think that Ariel has displayed evidence of Cryovolcanic activity? Widespread faulting is apparent.<br /><br />4). What about the small channels running along the valley floors (liquid cut or cryovolcanic 'lava tubes')?<br /><br />4). Both Ariel & Umbriel are very similar in size to the Saturn moons Tethys & Dione, yet all four are very different. Tethys & Umbriel I think are the least interesting as they seem to be nothing more than a pair of giant cratered iceballs. <br /><br />5). Why is Umbriel the odd one out? Dark surface, cratered & unevolved.<br /><br />In size order largest first (diameter). <br /><br />Umbriel: 1,170 KM / 727 miles. Uranus system. <br />Ariel: 1,158 KM / 719 miles. Uranus system. <br />Dione: 1,120 KM / 696 miles. Saturn system. <br />Tethys: 1,060 KM / 658 miles. Saturn system. <br />Enceladus: 500 KM / 310 miles. Saturn system. <br />Miranda: 472 KM / 293 mi <div class="Discussion_UserSignature"> <p><font color="#000080">"I suddenly noticed an anomaly to the left of Io, just off the rim of that world. It was extremely large with respect to the overall size of Io and crescent shaped. It seemed unbelievable that something that big had not been visible before".</font> <em><strong><font color="#000000">Linda Morabito </font></strong><font color="#800000">on discovering that the Jupiter moon Io was volcanically active. Friday 9th March 1979.</font></em></p><p><font size="1" color="#000080">http://www.launchphotography.com/</font><br /><br /><font size="1" color="#000080">http://anthmartian.googlepages.com/thisislandearth</font></p><p><font size="1" color="#000080">http://web.me.com/meridianijournal</font></p> </div>