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8/9/2019 Lunar Geology Traverse
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Lunar Geology Traverse
http://www.marcusmoon2022.org/
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Lunar Geology
Through the Looking Glass
Return humankind to the moon
Establish semi-permanent structures
Give back to the scientific community
Observatories
Traverse with multiple stops for geological studies
Each phase studies additional areas
Invaluable experience for future Mars projects
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Lunar Geology
Lunar Geology
Discover location of
resources for ISRU
Lunar formation
Earth and otherplanetary meteorite
remains
Origin of life/Astrobiology
History of planetaryformation
Samples for lunar
machinery developmentSouth Pole Region Source: Lunar and Planetary Society
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South Pole-Aitken Basin
Largest impact basin in the solar system
Different element concentration from the rest of the Lunar
surface
Thinner crust
Mantle may be present
Compositionally different from crust
Lunar Geology
South Pole-
Aitken
Basin
Topology
Source:
Lunar and
Planetary
Institute
South Pole-
Aitken BasinIron and
Titanium
Concentration
Source: Lunar
and Planetary
Institute
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Lunar Geology
Why Manned Exploration?
Humans versus robots debate
Humans have greater versatility than robots
Flexibility of tasks that can be accomplished Maneuverability/Range of motion
On site decision-making
Ability to reason to solve unexpected problems
No time delay from telerobotics
Engages public interest
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LunarSS
Traverse Phase I
Start: Landing Zoneat Mons Malapert
Prepare Rovers
Begin star-tracking First Stop:De Gerlache Crater
Second Stop:Shackleton Crater
Resupply Setup observatory
Lunar South Pole
Source: Space.com
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LunarSSEarth-set image taken by KAGUYA Source: JAXA
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Return Route
Lunar Geology
Return trip to Mons Malapert along
different route to cover additional
terrain
Third Stop: Faustini Crater
Fourth Stop: Shoemaker CraterFifth Stop: Malapert Crater
End: Mons Malapert
Top/Right: Shoemaker-Faustini and Shackleton Craters Source: Space.com NASA, Left (Right) South Pole Cold Traps Source: Cornell University
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LunarSS
0. Mons Malapert
1. De Gerlache Crater2. Shackleton Crater
3. Faustini Crater
4. Shoemaker Crater
5. Malapert Crater
Source: NASA-JPL
Clementine Elevation and
Slope Maps
Main Traverse Path
Excursions
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Lunar Geology
Support
Twin rovers in case of a malfunction oraccident
Main Rover
Basic tools and drill for geological sampling
Storage for Earthbound samples
Small quarters for multi-day traverses or sitestudies
Pressurized Lab for preliminary on-site testing
CEV passes overhead approximatelyevery 90 minutes
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Lunar Geology
Further Studies: Phase II
Power System
Links
Schrdinger Basin
(Crater) SetupSPIDAR Array
Explore
Lava tubes
Above: Elevation map of South Pole-Aitken Basin
Left:Dark-halo crater located within Schrdinger Basin
Source: Lunar and Planetary Institute, Clementine Images
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Lunar Geology
Future Studies:
Ideally the entirety of the Lunar surface will
be traversed and compositionally mapped
Heavy duty drilling operations to studydeeper layers of the lower crust and mantle
Very long traverses
Completely equipped Mobile Lab (orpermanent base) for thorough on-site
testing
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Lunar Geology
References Japan Aerospace Exploration Agency (JAXA)
KAGUYA (SELENE), Image Taking of Earth-Rise by HDTV
NASA-JPL
NASA Views Landing Site Through Eyes of Future Moon Crew
Lunar Mission Pilot Case Studies
NASA
Enhanced Radar Imagery of Lunar South Pole: Media Briefing, 02.27.08
SPACE.com
Lunar South Pole Landing Sites Studied
Lunar and Planetary Institute
Digital Lunar Orbiter Photographic Atlas of the Moon
Planetary Science Research Discoveries. The Biggest
Hole in the Solar System, G. Jeffrey Taylor, Hawai'i Institute of Geophysics and Planetology
Innovations Report
New lunar south polar maps from SMART-1, 12.03.2008
X Prize
Target Aitken Basin, South Pole
Lunar Astrobiology: Potential for pre-biotic chemistry at the poles of the Moon, Lucey, Paul
Cornell News
Radar provides first 3-D views of moon's frigid poles