ch 12-2 Saturn rings and moons

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Last updated 1:55 AM on 6/9/26
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62 Terms

1
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saturn’s spectacular ring system

  • has an extraordinarily large and complex ring system, which was visible even to the first telescope

  • 282,000 km from planet

  • 10 m thick

  • thought to be secondary objects

2
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overview of the Ring System

  • consists of main rings and faint outer rings

  • billions of dust like particles from tiny to large

<ul><li><p>consists of main rings and faint outer rings</p></li><li><p>billions of dust like particles from tiny to large</p></li></ul><p></p>
3
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what are the main rings?

  • A, B, C

  • Cassini division (rings composed of rings between A&B)

  • largest and most visible

  • ordered by discovery

  • B is the brightest

  • CBA is actual order in closeness

<ul><li><p>A, B, C</p></li><li><p>Cassini division (rings composed of rings between A&amp;B)</p></li><li><p>largest and most visible</p></li><li><p>ordered by discovery</p></li><li><p><em>B is the brightest</em></p></li><li><p>CBA is actual order in closeness</p></li></ul><p></p>
4
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what are the faint outer rings?

  • D, E, F, G

5
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what is the ring particles range in size?

  • form fractions of a millimeter of tens of meters

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what is the ring composition?

  • water ice—like snowballs

  • trace: rocky metallic material (colour variation)

  • high reflectivity

7
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how do particles travel?

  • travel at different speeds and collide and break down into smaller pieces and then fall into atm.

8
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for any given planet and any given moon…

  • the critical distance inside of which the moon is destroyed is known as tidal stability limit or Roche limit

9
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What is the Roche Limit?

  • The closest distance a moon can orbit a planet without being torn apart by tidal forces.

10
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Why can't large moons exist inside the Roche Limit?

  • The planet's tidal forces become stronger than the moon's self-gravity and pull it apart.

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Why are most Jovian rings found inside the Roche Limit?

  • Material inside the Roche Limit cannot form a large moon and instead remains as ring particles.

12
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How can a ring system form?

  • A moon that moves within the Roche Limit can be torn apart, producing ring material.

13
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zone that is too close to the planet for moon formation…

  • bc of tidal forces would overcome gravity and tear it apart

14
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what did voyager probes show?

  • Saturn’s rings to be much more complex than originally thought

    • composed of thousands of ringlets

      • spokes

      • shepherds moons

<ul><li><p>Saturn’s rings to be much more complex than originally thought</p><ul><li><p>composed of thousands of ringlets</p><ul><li><p>spokes</p></li><li><p>shepherds moons </p></li></ul></li></ul></li></ul><p></p>
15
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ringlets are not actually separated from one another by empty space

  • instead rings contain concentric regions of alternating high and low concentration of ring particles

16
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what is the pattern of Saturn’s ring?

  • spiral density waves

    • narrow gaps kept clear by action of small moonlets embedded in them

17
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list the rings from closest to farthest

  • D, C, B, Cassini Division, A, F, G, E

18
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F ring

  • narrow and dynamic

  • kinked and clumpy due to gravitational interaction with Shepard Moon

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G ring

  • further from F

  • lots of micro-dust

20
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E ring

  • outermost

  • far beyond orbit of moon titan

  • lots of micro ice and dust

21
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why is F ring considered the strangest ring?

  • it appears to have braids and kinks → dense core

  • Shepherded by Ephesus and Pandora → channels and snowballs of ice

22
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2 small dark satellites

  • Prometheus and Pandora

    • orbit around F ring

    • produce braid

23
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what else did Voyager find?

  • radial “spokes” that formed and then dissipated; this probably happens frequently

  • freshly formed spokes revolve same rotation of magnetic field and interior of Saturn → tiny dust electrically charged

24
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spokes apperance

  • sharp, narrow, suggest short formation times

25
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what is the unofficial theory of spokes?

  • think caused by small particles suspended by ring plane and electromagnetic forces responsible for features

26
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What causes divisions (gaps) in Saturn's rings?

  • Gravitational resonances with Saturn's moons.

27
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What is orbital resonance?

  • A situation where two objects have orbital periods related by a simple ratio, causing repeated gravitational interactions.

28
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How do resonances create gaps in rings?

  • Repeated gravitational tugs from moons disturb ring particles and remove them from certain orbits.

29
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What moon is associated with the Cassini Division?

  • Mimas.

30
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What causes the Cassini Division in Saturn's rings?

  • A 2:1 orbital resonance between ring particles and Saturn's moon Mimas.

    • mimas = 1 orbit

    • ring particle = 2 orbits

31
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what is a “Shepherd” moon?

  • defines outer edge of Ring A through gravitational interactions

32
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moon pulls on ring particles to?

  • prevent them from dispersing outward by orbiting out

  • nudge stray particles back into ring

33
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ring formation: details of formation are unknown

  • probably too active to have lasted since birth of solar system

  • not all rings may be the same age

  • either must be continually replenished or are the result of a catastrophic event

34
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35
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what are Saturn’s many moods appear to be made of?

  • water ice

36
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in addition to the small moons, Saturn has

  • 6 medium-sixed moons (Mimas, Enceladus, Tethys, Dione, Rhea, and Iapetus)

  • 1 large moon (Titan), almost as large as Jupiter Ganymede

37
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3 groups of Saturn’s moon

  1. “small” moons - irregularly shaped ice

  2. “medium” moons - spherical bodies - clues of past and present

  3. “large” moon - Titan

38
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Titans atmosphere

  • thicker and denser than Earth’s; mostly nitrogen 95% and argon

  • only moon with substation atm.

  • 50% denser than Earth

39
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what does Titans thick atmosphere impact?

  • makes surface impossible to see

<ul><li><p>makes surface impossible to see</p></li></ul><p></p>
40
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characteristics of Titan’s atmosphere

  • unique, chemically complex due to trace chemicals

  • Nitrogen, Methane, Hydrocarbon

  • organic rich environment

  • more extended than Earth because low gravity

  • thick and dense

  • unseen surface covered in organic material settled from clouds

  • low surface temperatures = thick atm.

  • weak gravitational pull

<ul><li><p>unique, chemically complex due to trace chemicals</p></li><li><p>Nitrogen, Methane, Hydrocarbon</p></li><li><p>organic rich environment</p></li><li><p>more extended than Earth because low gravity</p></li><li><p>thick and dense</p></li><li><p>unseen surface covered in organic material settled from clouds</p></li><li><p>low surface temperatures = thick atm.</p></li><li><p>weak gravitational pull</p></li></ul><p></p>
41
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Cassini Huygens observations

  • some surface features are visible in infrared image\not possible to see in visible spectrum

  • dense rich Nitrogen atm.

<ul><li><p>some surface features are visible in infrared image\not possible to see in visible spectrum</p></li><li><p>dense rich Nitrogen atm.</p></li></ul><p></p>
42
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what surface features are seen on Cassini?

  • internal liquid ocean beneath surface → H2O and Ammonia

  • has lakes and liquid methane

    • replenished from rain

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Huygens spacecraft landed on Titan

  • confirmed presence of liquid ethane in lakes

  • methane rain feed lakes

  • revealed ice pebbles, icey plains, river like drainage channels

<ul><li><p>confirmed presence of liquid ethane in lakes</p></li><li><p>methane rain feed lakes</p></li><li><p>revealed ice pebbles, icey plains, river like drainage channels</p></li></ul><p></p>
44
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lakes on Titan

  • Cassini detected dark reflective smooth regions thought to be lakes

  • Northern latitudes (liquid methane and ethane)

  • back to radar

    • smooth surface

<ul><li><p>Cassini detected dark reflective smooth regions thought to be lakes</p></li><li><p>Northern latitudes (liquid methane and ethane)</p></li><li><p>back to radar</p><ul><li><p>smooth surface</p></li></ul></li></ul><p></p>
45
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Titan’s interior: “Water World”

  • based on measurements made by Cassini and Huygens, this is the current bets understanding as to what the interior of Titan looks like

    • highly differentiated ocean world

    • thick icey outer crust

    • subsurface liquid ocean

    • rocky core

    • inner may be slushy water instead of open sea

46
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what are Saturn’s Mid-sized moons?

  • Mimas

  • Enceladus

  • Tethys

  • Dione

  • Iapetus

  • Rhea

  • orbit between 3 and 9 planetary radii from Saturn

47
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Iapetus

  • extreme 2 tone coloration

  • 2 km equatorial ridge

  • orbits 59 radii away from Saturn

<ul><li><p>extreme 2 tone coloration</p></li><li><p>2 km equatorial ridge</p></li><li><p><em>orbits 59 radii away from Saturn</em></p></li></ul><p></p>
48
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Mimas

  • Hershel crater

  • “inner icey moons”

  • intermediate sized

  • orbit between ring system and Titan

  • heavily cratered

  • water ice

<ul><li><p>Hershel crater</p></li><li><p>“inner icey moons”</p></li><li><p>intermediate sized </p></li><li><p>orbit between ring system and Titan</p></li><li><p>heavily cratered</p></li><li><p>water ice</p></li></ul><p></p>
49
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Enceladus

  • active geysers

    • heat and potentially habitable

<ul><li><p>active geysers </p><ul><li><p>heat and potentially habitable </p></li></ul></li></ul><p></p>
50
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Tethys

  • large canyon system

51
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Dione

  • tectonic features

  • potential subsurface ocean

<ul><li><p>tectonic features</p></li><li><p>potential subsurface ocean</p></li></ul><p></p>
52
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Rhea

  • largest of group

  • brightest, heavily cratered

  • weak ring system

<ul><li><p>largest of group</p></li><li><p>brightest, heavily cratered</p></li><li><p>weak ring system</p></li></ul><p></p>
53
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all mid-sized moons are tidally locked

  • heave “leading” and “trailing” surfaces

54
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enceladus

  • surface seems oddly youthful

  • inset shows icy jets

  • large ocean believed to exist under the ice

  • white and reflective surface with water ice

  • heavily cratered Northern region

  • tectonic deformed younger southern

  • small

<ul><li><p>surface seems oddly youthful</p></li><li><p>inset shows icy jets</p></li><li><p>large ocean believed to exist under the ice</p></li><li><p>white and reflective surface with water ice</p></li><li><p>heavily cratered Northern region</p></li><li><p>tectonic deformed younger southern</p></li><li><p>small</p></li></ul><p></p>
55
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Janus and Epimetheus share a single orbit

  • irregularly shape

  • unique gravitational dance every 4 years

    • swap positions to avoid collision

  • one moves to higher, slower orbit and the other drops lower to faster orbit

<ul><li><p>irregularly shape</p></li><li><p>unique gravitational dance every 4 years </p><ul><li><p>swap positions to avoid collision</p></li></ul></li><li><p>one moves to higher, slower orbit and the other drops lower to faster orbit</p></li></ul><p></p>
56
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telesto and calypso

  • two more are at the same Lagrangian points of Saturn’s moon Tethys (trojan moons, 60° behind)

  • stable gravitational positions

<ul><li><p>two more are at the same Lagrangian points of Saturn’s moon Tethys (trojan moons, 60° behind)</p></li><li><p>stable gravitational positions</p></li></ul><p></p>
57
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what did the Cassini spacecraft use to make multiple close passes around Saturn’s moons?

  • gravitational slingshots

    • precise orbits are decided on the fly

<ul><li><p>gravitational slingshots</p><ul><li><p>precise orbits are decided on the fly</p></li></ul></li></ul><p></p>
58
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Saturn and Jupiter rotate

  • differentially and is significantly flattened

59
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saturn generates its own heat through?

  • helium raindrops

60
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interactions with medium and small moons determine?

  • ring structure

61
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the rings are entirely within the?

  • Roche limit, where larger bodies would be torn apart by tidal forces

62
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several of he small moons share orbits with?

  • either each other or with larger moons