NASA's GRAIL Mission Resolves Mystery of Moon's Asymmetrical Hemispheres
Aspect | Details |
---|---|
Event | NASA's GRAIL mission resolves mystery of Moon's asymmetrical hemispheres |
Mission Name | GRAIL (Gravity Recovery and Interior Laboratory) |
Launched | 2011, from Cape Canaveral via Delta II rocket |
Managed by | Jet Propulsion Laboratory (JPL) |
Scientific Lead | Massachusetts Institute of Technology (MIT) |
Components | Two spacecraft -- Ebb and Flow, flown in tandem |
Objective | To map the Moon's gravity field with high precision |
Key Discovery | Gravitational and thermal differences caused by Earth's pull and internal heat sources |
Crustal Differences | Nearside: Thinner crust, volcanic activity, basaltic plains (mare) |
Farside: Thicker crust, rugged, heavily cratered, less volcanic activity | |
Heat Flow and Elements | Nearside: Higher thorium and titanium levels, mantle ~200°C warmer than farside |
Tidal Effects | Nearside experiences greater tidal flexing due to Earth's gravity |
Significance | Solves lunar geological puzzle, aids understanding of planetary formation and evolution |
Future Implications | Supports lunar exploration missions and landing site selections |