Title: Moons of the Jovian Planets: Satellites of Ice and Rock
1Moons 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?
2What 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).
3Medium 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'
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5What makes Jupiters Galilean moons unusual?
IO EUROPA Ganymede
Callisto
6Ios Volcanoes
- Io is the solar system's most volcanic world.
7Tidal stress cracks Europas surface ice, which
floats to new positions on a subsurface ocean of
water or slush.
8Interiors of Io Europa are warmed by tidal
heating.
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10What makes Saturn's moon Titan different from
other moons?
11What 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.
12Neptunes 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).
13Uranus small moon Miranda shows huge cliffs
tectonic activity, and few craters.
14Why 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).
15What 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.
16What 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.
17What 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.