skip navigation
Astronomy 161
Introduction to Solar System Astronomy
Prof. Paul Martini

Lecture 37: Moons of Saturn


Key Ideas:

Most diverse moon system of any planet
Trojan and co-orbital moons
Large moons
Cratered Hyperion
Two-toned Iapetus
Cryo-geysers on Enceladus
Saturn's Giant Moon Titan
Only moon with a thick atmosphere
Prospects for Life


Trojan Moons

Tethys has two trojan moons: Telesto and Calypso
Located at the L4 and L5 lagrange points


Co-orbital Moons

Epimetheus and Janus are the only examples known
Orbital separation is less than their diameters
Exchange happens every four years
Works because their masses are similar


Large Moons

Tethys, Dione, and Rhea
Densities of ~1 g/cc
Spherical due to gravity
Flattened craters
Mimas
Responsible for the Cassini Division
Herschel Crater is 140km across
Egg-shaped by tidal forces


Hyperion

Covered in deep, sharp-edged craters
Main constituent is dirty water ice
Porosity is about 40%
Craters may form by melting around darker material or compression upon impact


Iapetus

Leading hemisphere has a 3-5% albedo
Trailing hemisphere has a 50-60% albedo
Has a 1300 km equatorial ridge that rises 20 km above the surface
Likely the leading surface is polluted by Phoebe, which may be an object captured from the Kuiper Belt


Titan: Saturn's Giant Moon

Discovered in 1655 by Christian Huygens
Second largest moon in the Solar System
50% larger than our Moon
Larger than Mercury (but less massive)
Composition similar to Pluto
Only moon with a thick atmosphere


Huygens Lander

Part of the Cassini mission to Saturn
The Huygens probed separated from Cassini and parachuted to the surface of Titan on January 14, 2005
Goal to measure surface composition and conditions


Titan's Atmosphere

Composition:
98% N2 (Nitrogen)
2% CH4 (Methane)
Argon, hydrocarbons like Ethane
Cold, dense atmosphere:
Temperature: 94 K (-290 F)
Pressure: ~1.6 Earth atmospheres
Clouds of Nitrogen and methane ices
Hydrocarbon "smog"


Titan's Surface

Young surface with very few impact craters
Varied terrain:
Smooth, dark plains (methane mud flats?)
Rugged highlands
Drainage channels
Impact basins


Is Methane Titan's "Water?"

Methane (CH4) may play the same role on Titan that water does on the Earth:
94 K is between the boiling and freezing points of Methane
Get gaseous methane in the atmosphere
Methane condenses into clouds that rain liquid methane
Signs of drainage flows
Huygens landed in soft methane/water ice mud
Water ice is like sand on Titan


Life in the Outer Solar System?

Europa and Titan are considered the most promising sites to search for life in the Solar System after Mars
Jupiter's Giant Moon Europa
Liquid ocean under the ice?
Life could be present
Saturn's Giant Moon Titan
Methane-based, rather than water-based, life could be present
Enceladus may also harbor microbial life


See A Note about Graphics to learn why some of the graphics shown in the lectures are not reproduced with these notes.

[ Return to the Astronomy 161 Main Page | Unit 6 Page ]


Updated: 2010 February 14 Copyright © Paul Martini All Rights Reserved.