Sect 9.3
Speculations on the Origin and Evolution of Continental Crust Earths thermal evolution poorly understood - parameterized models yield contrasting predictions.
Notes 28.1 Earth’s Moon Std 1F: Know the evidence for the dramatic effects that asteroid impacts have had in shaping the surface of planets and their moons.
STRUCTURE OF THE MOON BY SEISMIC DATA V.Yu. Burmin Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia.
An Inquiry about Evidence for the Late Heavy Bombardment Clark R. Chapman & David H. Grinspoon SwRI, Boulder CO 65th Meteoritical Society Meeting (2002)
What are the Astrobiological Constraints from What is Known about the Late Heavy Bombardment? What are the Astrobiological Constraints from What is Known.
The Moon Satellite – Any body orbiting a central mass No Atmosphere No temperature regulation Daytime temperature = 400 K (266 F) Nighttime temperature.
1 ESS200C Planetary Ionospheres Lecture 16. 2 Interactions with the Moon The Moon has no significant atmosphere and no ionosphere. The lunar crust is.
Roger D. Launius National Air and Space Museum Smithsonian Institution.
Center for Lunar Origin and Evolution (CLOE) Center for Lunar Origin and Evolution (CLOE) PI: William Bottke, Southwest Research Institute “Understanding.
Late Heavy Bombardment: Evidence From Cratering Histories of the Moon, Planets, Satellites, and Asteroids Clark R. Chapman Southwest Research Institute,
Chapter 28 Chapter 28 Minor Bodies of the Solar System The Moon.