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Site symmetry, Phoebe exogenic example. Favor endogenic model ... Probably not from Phoebe material. Strong evidence of some type of exogenic origin ... – PowerPoint PPT presentation

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Title: The%20Two%20Faces%20of%20Iapetus


1
The Two Faces of Iapetus
  • The Brightness Contrast Explored
  • Colleen Milbury

2
Overview
  • Discovery of Iapetus
  • Pictures
  • Observations
  • Endogenic Models
  • Exogenic Models
  • Summary/Conclusions

3
Discovery of Iapetus
  • In Greek mythology Iapetus was a Titan, the son
    of Uranus, the father of Prometheus and Atlas and
    an ancestor of the human race.
  • Discovered by Giovanni Cassini in 1671
  • He said the following about Iapetus in 1673
  • One part of Iapetus surface is not so
    capable of reflecting the light to us the light
    of the Sun which maketh it visible, as the other
    part is
  • Cassini was able to observe Iapetus during
    western elongation, he could not detect it during
    eastern elongation.

4
Pictures of Iapetus
5
(No Transcript)
6
Table of Parameters
7
Nice Diagram of Saturn System
8
Observations
  • Order of magnitude contrast
  • Geometric albedo is 0.04-0.5
  • Centered about apex of motion
  • Low albedo inconsistent with silicates

9
More Observations
  • Low albedo (dark) material is Red (albedo
    increases at longer ?s)
  • -Does not match C-type (carbonaceous) asteroid
    similar to Phoebe, only redder D-type asteroids
  • Dark floored craters imply dark material is
    younger
  • Absence of bright craters imply
  • -deposit is thick (gt10 km), or
  • -bright material darkened/buried with 100
    million year period

10
Endogenic Model-Smith et al. 1982
  • Site symmetry, Phoebe exogenic example
  • Favor endogenic model
  • Dark floored craters as strong endogenic evidence
  • Site examples of other hemispheric alignments in
    solar system (Mars, Moon, and Io)

11
Exogenic Model-Owen et al. 2000
  • Use mixing models of pure substances
  • Satisfied 1,3, and 4 with amphorus carbon and
    water-ice
  • Turned to organic compounds to satisfy 2 and stay
    consistent with 4
  • Conclude that component comes from Titans
    nitrogen rich atmosphere
  • Titan impact that could have sprayed particles
    onto Hyperion and Iapetus and even produced
    Hyperion

12
Exogenic Model-Buratti et al. 2001
  • Three nights of measurement from Hale telescope
    on Palomar Mountain
  • Three D-type asteroids and icy Saturn satellites
  • Range is 0.33-0.92 µm

13
Exogenic Model-Buratti et al. 2001
  • F-normalized Fluxes
  • IcyIcy Bodies
  • IapIapetus
  • DD-type asteroids
  • A-coefficient (percent of material)
  • Dont combine spectra of pure substance
  • Use spectra of typical icy bodies, D-type
    asteroids

14
Exogenic Model-Buratti et al. 2001
  • Apply to albedo
  • Conclude that dark side Iapetus created by
    collision of proto-Hyperion and D-type asteroid

p geometric albedo
15
Exogenic Model-Buratti et al. 2001
  • Hyperion - irregular shape and chaotic rotation
    imply it is remnant of larger body
  • Also note discovery of 5 new satellites that
    appear to be created from this impact
  • Most particles are accreted by Titan

16
Summary and Conclusions
  • Iapetus is somewhat of a rarity in the solar
    system
  • Probably not of endogenic origin
  • Probably not from Phoebe material
  • Strong evidence of some type of exogenic origin
  • Buratti et al. most likely

17
References
  • Buratti et al. (2001). High Resolution 0.33-0.92
    µm Spectra of Iapetus, Hyperion, Rhea, Dione, and
    D-Type Asteroids. Icarus, 155, 375-381.
  • Morrison et al. (1974). The Two Faces of Iapetus.
    Icarus, 24, 157-171.
  • Owen et al. (2000). Decoding the Domino. Icarus,
    149, 160-172.
  • Smith et al. (1982). A New Look at the Saturn
    System. Science, Vol. 215, No. 4532, 504-537.
  • Satellites. Edited by Joseph A. Burns, Mildred
    Shapley Matthews Tucson University of Arizona
    Press, c1986.
  • Saturn. Edited by Tom Gehrels, Mildred Shapley
    Matthews. Tucson, Ariz. University of Arizona
    Press, c1984
  • Soter, S. 1974. Brightness of Iapetus. Paper
    presented at IAU Colloq. 28, Cornell University,
    August 1974.
  • Squyres et al. (1984). Voyager Photometry of
    Iapetus. Icarus, 59, 426-435.

18
The End!
19
The Facts
Inconsistencies
  • Phoebe exogenic models (Soter 1974) - fact 4
  • Endogenic models - fact 3
  • Superficial layer of ice covering underlying dark
    surface - fact 5

Saturn book p. 853
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