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of the Jovian : Satellites of and

• What kinds of moons the jovian planets? • What makes ’s unusual? • What makes 's different from other moons? • Why are small icy moons more geologically active than small rocky planets? 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 , all in the same direction). Small moons: mostly captured and (mildly to extremely elliptical orbits, even retrograde ones). Medium & large moons • L o ts o f ic e • Active resurfacing in the past (some moons even today) • Enough self­ to be spherical: young, `molten' moon rock and ice ran `downhill' [like on ] until it made a sphere [on which there is no more `downhill']

What makes Jupiter’s Galilean moons unusual?

IO ’s Volcanoes

Io is the 's most volcanic world. Tidal stress cracks Europa’s surface ice, which floats to new positions on a subsurface ocean of water or slush. Interiors of Io & Europa are warmed by .

What makes Saturn's moon Titan different from other moons? What makes Saturn's moon Titan different from other moons? • Only moon with an : 90% , plus argon, , (smog!). • Methane & are greenhouse gases. • Still cold: 93 K (­180 degrees C) • Chemical reactions on Titan produce organic, chemicals (hydrocarbons, etc.) • Cassini images show a young surface (few craters) but with evidence of only at the poles. • Possibly a captured ’s Moon K u i p e r b e l t o b j e c t : orbiting Neptune opposite Neptune’s direction of • Neptune's tidal bulges (caused by Triton) are pulling backwards on Triton, slowing it down into a future crash into Neptune. • Smaller than Earth’s Moon, yet has recent geological activity (nitrogen ). ’ small moon shows huge cliffs & tectonic activity, and few craters. 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). What have we learned?

• What kinds of moons orbit the jovian planets? • We can categorize the more than 100 known moons as small, medium­size, or large. • Most medium­size and large moons probably formed with their in the disks of gas that surrounded the young jovian planets. • Small moons are most often captured asteroids or comets. • What makes Jupiter’s Galilean moons unusual? What have we learned? • Io is the most volcanically active object in the solar system. Europa may have a deep, liquid water ocean under its icy . 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. What have we learned?

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