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The Geomorphology of Icy Moons

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Page 1: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

The Geomorphology of Icy Moons

Page 2: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Icy Moons in the Solar System

jpl.nasa.gov

Europa Ganymede Callisto Mimas Enceladus

Titan? Miranda Umbriel Triton

Jupiter

Saturn

Uranus

Neptune

Page 3: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

What Makes A Moon Icy?

• Orbit A Giant Planet – Lie Beyond the Solar System’s Frost Line

• Formed Outside of the Inner Region of a Proto-

Satellite Disk – Lie Beyond the Planet’s Frost Line

juno.wisc.edu

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Characterizing Icy Moons

• Size • Albedo – Geometric or Bond

• Surface Age – Cratering

• Surface Temperature

Page 5: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Relative Sizes of Icy Moons

jpl.nasa.gov

Europa Ganymede Callisto Mimas Enceladus

Titan? Miranda Umbriel Triton

Jupiter

Saturn

Uranus

Neptune

Luna

Page 6: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Types of Albedo

• Bond

• Geometric

nc-climate.ncsu.edu

iopscience.iop.org

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Determining Surface Age

• Crater Counting – Hard to Determine True Age – Determines Relative Ages

mars.asu.edu

Page 8: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Surface Temperature

• Indirect Detection – Observed Emitted IR-Spectra – Fitting to Blackbody Curves

• Direct Detection – Orbiters – Thermal Radiation

jpl.nasa.gov

sci.esa.int

Page 9: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Saturnian System

• Extensive Ring System – A-, B-, C-, D-, and E-Ring – 6,630 – 120,700 km Above Equator – 20 km Thick

• 150 Satellites – Moons or Moonlets – At least 1 (Rhea) Has Its Own Ring System

Page 10: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

jpl.nasa.gov

60,000 km 

Page 11: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

jpl.nasa.gov

60,000 km 

Page 12: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

jpl.nasa.gov

60,000 km 

Page 13: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Enceladus

• 6th Largest Moon of Saturn

• Located in the E-Ring

• Only 500km in Diameter (1/13th of Earth)

• Albedo of 0.99 (Bore)

jpl.nasa.gov

Page 14: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

What is Special About Enceladus?

• Surface is Made Almost Entirely of Water Ice

• Over 100 Cryovolcanic Plumes on the South Pole

• Possible Location of Extraterrestrial Life

jpl.nasa.gov

Page 15: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Geography of Enceladus

• 4 Regions – Southern Polar Terrain

(SPT)

jpl.nasa.gov

Page 16: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Southern Polar Terrain (SPT) - Plumes

• Cryovolcanic • Extend 100s of Kilometers into

Space

• Consist of Water Ice, NH3, Na and K Salts, and Various Gases

• Contributing to Saturn’s E-Ring

jpl.nasa.gov

Page 17: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

jpl.nasa.gov

60,000 km 

Page 18: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Southern Polar Terrain (SPT) – Tiger Stripes

• Curvilinear, Nearly Parallel Rifts

• Younger and Warmer than Adjacent Surfaces

• Sources of Plumes

• Located in a Basin

jpl.nasa.gov

Page 19: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Southern Polar Terrain (SPT) – Tiger Stripes

jpl.nasa.gov

Page 20: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

jpl.nasa.gov

Page 21: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

jpl.nasa.gov

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jpl.nasa.gov

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Geography of Enceladus

• 4 Regions – South Polar Terrain

(SPT) – Leading Hemisphere

jpl.nasa.gov

Page 24: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Resurfacing of Hemisphere

• Tidally-Locked with Saturn

• The E-Ring

jpl.nasa.gov

Page 25: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

jpl.nasa.gov

Page 26: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Geography of Enceladus

• 4 Regions – South Polar Terrain

(SPT) – Leading Hemisphere – Northern Hemisphere

jpl.nasa.gov

Page 27: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Northern Hemisphere

• Cratered Terrain

• Some of the Oldest Features on Enceladus

• Particularly Densely Cratered on the Trailing Hemisphere

• Least Geologically Active Region

jpl.nasa.gov

Page 28: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Geography of Enceladus

• 4 Regions – South Polar Terrain

(SPT) – Leading Hemisphere – Northern Hemisphere – Equatorial Region

jpl.nasa.gov

Page 29: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Equatorial Region - Icy Rifts

• 100 to 400 Meters Wide

• Formed by the Tidal

Morphing of the Moon

jpl.nasa.gov

Page 30: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Tidal Morphing

• Enceladus’s Eccentric Orbit: e = 0.0047 – ∆Fg ~ 1017 N

• Similar to Earth’s Tides

nature.com

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Equatorial Region – Transitional Terrain

• Located near Icy Rifts

• Fractures Form Boundaries between Cratered Surfaces and Folded Surfaces

• May be Evidence of Subduction Zones

jpl.nasa.gov

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Equatorial Region – Modified Craters

• Further Evidence of Tectonic Forces

• Craters Show Signs of Crosscutting

jpl.nasa.gov

Page 33: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Jovian System

• Slighter Ring System – Made of Dust

• Strong Magnetosphere – 14x the Strength of Earth’s

• ≥ 67 Moons – Galilean Moons: Ganymede, Callisto, Io, and Europa

Page 34: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

uoregon.edu

115,000 km 

Page 35: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Europa

• 4th Largest Moon of Jupiter − Smallest Galilean Moon

• 3120 km in Diameter (1/4 of Earth)

• Albedo of 0.67 (Bore)

jpl.nasa.gov

Page 36: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Similarities with Enceladus

• Water Ice Crust

• Liquid Subsurface Ocean

• Cryovolcanism

• Tidal Morphing/Heating

• NSR

americaspace.com

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Differences from Enceladus

• Lower Albedo

• 6x in Diameter – 500x More Massive

jpl.nasa.gov

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Courtesy of Katterhorn and Prockter

Page 39: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Courtesy of Katterhorn and Prockter

Page 40: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Courtesy of Katterhorn and Prockter

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Hydrological Cycle on Europa

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Hydrological Cycle on Europa

Page 43: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Hydrological Cycle on Europa

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Hydrological Cycle on Europa

Page 45: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Hydrological Cycle on Europa

Page 46: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Hydrological Cycle on Europa

Page 47: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Hydrological Cycle on Europa

Page 48: The Geomorphology of Icy Moonswray.eas.gatech.edu/physicsplanets2016/LectureNotes/IcyMoons.pdfSouthern Polar Terrain (SPT) - Plumes • Cryovolcanic • Extend 100s of Kilometers into

Hydrological Cycle on Europa

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Hydrological Cycle on Europa

• Cryovolcanic Emissions

• Cosmic Dust Capture

• Refreezing

• Radiolysis

• Subduction

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Astrobiological Implications

• Some Cosmic Dust Contains Organic Molecules

• Oxygenation of the Subsurface Ocean

• Similar to Enceladus

• More Access to Non-Indigenous Molecules

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Any Questions?