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Possible Cryovolcano Discovered on Titan

Rei writes "NASA's Jet Propulsion Laboratory is reporting that the Cassini spacecraft has observed what appears to be a cryovolcano on Saturn's moon Titan. Given the absense of a global methane sea on Titan, the snail-shaped structure with what appears to be a caldera on top could explain how Titan's methane stays replenished. It could further explain the dry drainage channels discovered by the Huygens lander as being formed by heavy methane rainfall after eruptions."

10 of 116 comments (clear)

  1. Guess what... by Trollstoi · · Score: 4, Informative

    ... methane can be found at Jupiter and Saturn, Oberon, Miranda and Titania... Neptune, Titan...
    astronomy dominee

  2. Re:Titan Climatology by youngerpants · · Score: 5, Informative
    Not necessarily, pyroclastic flows on Earth are flows of solid matter (rocks) that can occur during periods of volcanic activity.


    Although they are made out of "solid" matter the flows seem almost liquid in nature. Don't think of the methane as one huge frozen lump, but rather many solid lumps in motion.

  3. Re:Titan Climatology by Ford+Prefect · · Score: 4, Informative

    Actually, they decided the creme brulee hypothesis was wrong - the first thing the lander hit was a rock, which it then slid off, which gave a similar reading to the impactometer as creme brulee.

    ... And before anyone asks, yes, they did indeed test the sensor against real crème brûlée!

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    Tedious Bloggy Stuff - hooray?
  4. Definition of Cryovolcano by httpamphibio.us · · Score: 5, Informative

    "Cryovolcanoes are pseudo-volcanoes believed to be present on Titan, the largest moon of Saturn. Unlike volcanoes on Earth which spew hot lava, cryvolcanoes bring super-cool "lava" to the surface of their planets. They are volcanic-like vents that spew forth ice, water or vapor-phase volatiles, with some gas driven solid fragments instead of lava. It is suggetsed that they could be present on Titan, one of Saturn's moons. However it has only been seen on Triton, the biggest of Neptune's moons. Also it is said that they might be active in Europa and Enceladus.

    This term was coined by NASA in late 2004, when the Cassini space probe observed cryvolcanoes and cryogenic lakes for the first time."


    definition quoted from explore-dictionary.com

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    sig.
  5. Take a look for yourself by Chris84000000 · · Score: 5, Informative

    Today's Astronomy Picture of the Day show a nice picture of this.

    If you're interested in this stuff, bookmark http://antwrp.gsfc.nasa.gov/apod/astropix.html, which just points to the current picture of the day.

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    Please stop misusing Catch-22 to describe chicken-egg problems or other paradoxes that are not Catch-22.
  6. Re:Titan Climatology by Anonymous Coward · · Score: 3, Informative

    While a lot of things are possible (at least until we have more data), most of these gas giant moons seem to derive whatever internal heat they have from tidal deformation. It's the same thing that happens when you take a wire and bend it back and forth really fast.

    I haven't seen the numbers crunched that would tell how much energy Titan could derive from it's orbital eccentricity, but it wouldn't take much to drive methane ice at cryogenic temperatures.

  7. Cryoclastic eruptions? by amightywind · · Score: 4, Informative

    Titan is the only moon in the solar system to have a substantial atmosphere

    Triton, Neptune's large moon also has a substantial Nitrogen atmosphere, enough to entrain geyser plumes that move downwind. Ganymede has a thin atmosphere as well.

    the hypothesis is that this feature is probably formed by plumes of frozen methane, forced from underground, which then slowly evaporate into methane gas.

    It will be interesting to see what style of volcanism dominates on Titan - "cryoclastic" eruptions of methane gas and ammonia-hydrate ice crystals, or gooey water/hydrocarbon flows. The light colored lobate features surrounding the caldera in the TIMS image suggests the later. The apparent ring faults surrounding the caldera also suggest that this is a shield profile volcano built by effusive eruptions. It will be interesting to measure its profile with Cassini's radar to find out for sure.

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    an ill wind that blows no good
    1. Re:Cryoclastic eruptions? by amightywind · · Score: 2, Informative

      What about Iapetus? It has what looks like wind blown streaks, but it doesn't appear to have an atmosphere.

      Iapetus, Dione, Rhea all have bright wispy terrains that may have an impact or tectonic origin. There is no evidence at all that these features were disbursed by an atmosphere. But Triton's dark geyser plumes have been observed actively rising and disbursing downwind at altitude.

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      an ill wind that blows no good
  8. Re:What a nerd. by Anonymous Coward · · Score: 2, Informative

    Cryptovolcano

    A volcano-like feature on a planet or moon, that may or may not be an actual volcano. Examples have been found, for example, on the surface of Ganymede.

    http://www.google.com/search?hl=en&q=cryptovolcano &btnG=Google+Search

  9. Re:no ocean? by Tablizer · · Score: 2, Informative

    TFA says there is no methane ocean on Titan. I thought that's what the "large black Lake-like" features were. I think I missed something... When was it established that those weren't hydrocarbon lakes?

    The Hyugens probe appearently landing on one of those "lakes". They speculate that it is a dried-out lake-bed. Appearently it fills up when the vocanos errupt.