Moons of the Jovian Planets: Satellites of Ice and Rock - PowerPoint PPT Presentation

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Moons of the Jovian Planets: Satellites of Ice and Rock

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... pulling backwards on Triton, slowing it down into a future crash into Neptune. Smaller than Earth's Moon, yet has recent geological activity (nitrogen geysers) ... – PowerPoint PPT presentation

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Title: Moons of the Jovian Planets: Satellites of Ice and Rock


1
Moons of the Jovian Planets Satellites of Ice
and Rock
  • What kinds of moons orbit the jovian planets?
  • What makes Jupiters Galilean moons unusual?
  • What makes Saturn's moon Titan different from
    other moons?
  • Why are small icy moons more geologically active
    than small rocky planets?

2
What kind of moons orbit the jovian planets?
  • Two kinds
  • Medium and large moons
    mostly formed at the same time as their
    planets (nearly circular orbits, all in the same
    direction).
  • Small moons
    mostly captured asteroids and comets
    (mildly to extremely elliptical orbits, even
    retrograde ones).

3
Medium large moons
  • Lots of ice
  • Active resurfacing in the past (some moons even
    today)
  • Enough self-gravity to be spherical young,
    molten' moon rock and ice ran downhill' like
    water on Earth until it made a sphere on which
    there is no more downhill'

4
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5
What makes Jupiters Galilean moons unusual?
IO EUROPA Ganymede
Callisto
6
Ios Volcanoes
  • Io is the solar system's most volcanic world.

7
Tidal stress cracks Europas surface ice, which
floats to new positions on a subsurface ocean of
water or slush.
8
Interiors of Io Europa are warmed by tidal
heating.
9
(No Transcript)
10
What makes Saturn's moon Titan different from
other moons?
11
What makes Saturn's moon Titan different from
other moons?
  • Only moon with an atmosphere 90 nitrogen, plus
    argon, methane, hydrocarbons (smog!).
  • Methane ethane are greenhouse gases.
  • Still cold 93 K (-180 degrees C)
  • Chemical reactions on Titan produce organic,
    chemicals (hydrocarbons, etc.)
  • Cassini spacecraft images show a young surface
    (few craters) but with evidence of hydrocarbon
    lakes only at the poles.

12
Neptunes Moon Triton
  • Possibly a captured Kuiper belt object orbiting
    Neptune opposite Neptunes direction of rotation
  • Neptune's tidal bulges (caused by Triton) are
    pulling backwards on Triton, slowing it down into
    a future crash into Neptune.
  • Smaller than Earths Moon, yet has recent
    geological activity (nitrogen geysers).

13
Uranus small moon Miranda shows huge cliffs
tectonic activity, and few craters.
14
Why are small icy moons more geologically active
than small rocky planets?
  • Hot interiors needed for geological activity.
  • Ice deforms more easily than solid rock
  • Less internal heat is required
  • Smaller objects can be geologically active.
  • Tidal heating important for some icy moons, but
    not for rocky planets (example the Moon's tides
    are slowing down the Earth, but not heating it up
    by any significant amount).

15
What have we learned?
  • What kinds of moons orbit the jovian planets?
  • We can categorize the more than 100 known moons
    as small, medium-size, or large.
  • Most medium-size and large moons probably formed
    with their planet in the disks of gas that
    surrounded the young jovian planets.
  • Small moons are most often captured asteroids or
    comets.

16
What have we learned?
  • What makes Jupiters Galilean moons unusual?
  • Io is the most volcanically active object in the
    solar system. Europa may have a deep, liquid
    water ocean under its icy crust. Ganymede also
    thought to have a subsurface ocean.
  • What makes Titan different from other moons?
  • Titan is the only moon in our solar system with a
    thick atmosphere. It has a young surface with
    lots of contrasting features, but we don't yet
    know what they are.

17
What have we learned?
  • Why are small icy moons more geologically
    active than small rocky planets?
  • Ices deform and melt at much lower temperatures
    than rock, allowing icy volcanism and tectonics
    at surprisingly low temperatures.
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