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Over Two Decades at Mono Domes: Slow Changes to Potential Analogs to Martian Aeolian Bedforms. - PowerPoint PPT Presentation
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Over Two Decades at Mono Domes:Slow Changes to Potential Analogs to Martian
Aeolian Bedforms
Williams, Steven H., Chair, Education Division, National Air and Space Museum, MRC 305, P.O. Box 37012, Washington, DC 20013-7012, [email protected]; Zimbelman, James R., Chair, Center for Earth and Planetary Studies, National Air and Space Museum, MRC 315, Box 37012, Washington, DC 20013-7012, [email protected]; Peterfreund, Alan R., Peterfreund Associates, 30 Boltwood Walk, Amherst, MA 01002; and Greeley, Ronald, Department of Geological Sciences, Arizona State University, Box 871404, Tempe, AZ 85287-1404
NOTE: View this presentation in “Notes Page” mode to see commentary. This is not a transcript of the talk as delivered at GSA 2003 in Seattle, but the Notes comments convey the content and flavor of the remarks as delivered at GSA!
Over Two Decades at Mono Domes:
Slow Changes in Potential Analogs to Martian Aeolian
BedformsSteven H. Williams
James R. ZimbelmanAlan R. Peterfreund
Ronald Greeley
Large “Ripples”
Large Ripples on Mars
• Hinted At in Viking Images
• Common and Widespread
• Overlain by Dunes and Debris
• Some Atop Dunes
Dunes Override Ripples
Floor of Crater Kaiser
Ripples Override Dunes
M2000635 excerpt
?
Previous Work
Large (“Granule-” / “Deflation-) Ripples:
• Kelso Dunes (California)• Coachella Valley• Rogers Dry Lake @ Edwards AFB• Great Sand Dunes National Monument• Coyote Playa
All involve granules or coarser materials
Problem!
• Terrestrial Granule Ripples are fragile– Prone to removal– Prone to burial by mobile sand
• BUT: On Mars, at least some large ripples appear to be older and more durable than their terrestrial counterparts
So – do we have the “best” analogs?
Mars “Ripples” Are Old (?)
• Note debris apron overlies ripples• Implies ripples long-lived• Implies they are more durable than typical terrestrial granule ripple
Not All Large Ripples Involve Granules!
• What if particles involved are distinguished by density, not by size?
• Candidate examples: Pumice
• Low density allows larger particles to move and create bedforms
• Field Example: Mono Domes, California
Large ripples in pumice/obsidian
South Mono Dome, California
Minimal changes over ~22+ years
June, 2003
May, 1981
June, 2003
Bedform Comparison
May, 1981
June, 2003
May, 1981
Bedform Comparison
Ripple Crest Alteration
Raked
Stomped
Typical Bedform Profile
Sedimentary Characteristics• Bedform Crests (D = 1.2 cm)
– Pumice 66 wt % = 1.8– Obsidian 11 wt % = 2.1
• Windward Slope (D = ~5 mm)
– Pumice 74 wt % = 1.6– Obsidian 11 wt % = 2.1– More poorly sorted; skewed to fines
• Leeward Slope (D = ~5 mm)
– Pumice 26 wt % = 1.6– Obsidian 37 wt % = 2.2
Conclusions
• Some terrestrial large ripple bedforms are very long-lived
• Larger, but lighter, particles may be more mobile