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Theories:Origin of Earth and Moon
Scientists look for
Evidenceand an
Explanation
Facts - Evidence Searching for an explanation
• Earth has a iron core• Moon rocks do not have iron
• Earth’s average density is 5.5 grams/cm• Moon’s average density is 3.3 grams/cm
• Earth has a specific isotope of oxygen• Moon has the same unique isotope of oxygen
• Earth has a large Moon compared to it’s size
Theory #1Accretion Theory
The moon is a sister world that formed in orbit around Earth at the same time as the Earth formed.
Pros
• We know there was plenty of material to clump together (accrete)
Cons
• Why doesn’t the Moon have iron like Earth has?
• Why no other large moons around Mars, Venus, Mercury?
Theory #2Moon Capture Theory
• Moon was somewhere in space, and was captured into orbit around Earth
Pros
• Explains why Moon has no iron (it came from somewhere else)
Cons
• Moon has the same isotope composition as Earth
• Capturing a body as big as the Moon takes some tricky physics. Unlikely to happen.
Theory #3Fission
• Early Earth spun so fast that it spun off the moon
Pros• Explains why the Moon has no iron - it
came from just Earth’s mantle. The Moon’s density is similar to the Earth’s outer layers.
Cons• The energy in the system does not add up; Earth would have to spin too fast.
• Moon would orbit Earth’s equator - it does not.
• Rock density is similar, but composition is not.
• Why don’t other planets have big moons too?
Theory #4 Giant Impact Hypothesis
A very large body crashed into the Earth. Debris from the impact made a moon.
Pros• A collision is possible • Explains the lack of iron core on the Moon• Explains why both have the same isotope of oxygen (Moon rocks came from Earth)• Computer models - show physics is possible• Explains why Earth axis is tilted!
Cons• The physics don’t exactly work out - Roche limit problem (not enough angular momentum in today’s Earth-Moon system).
• Why only one moon?
• The limit around a body where gravity will rip apart another body.
• If a body gets too close to the Roche limit it will break up.
• Outside the Roche limit debris tends to clump together.
Roche Limit
Moon
A quiet landscape awaits!
Credits
• “The Formation of the Moon”, Dept of Astronomy, Case Western Reserve, February 22, 2006
http://burro.astr.cwru.edu/.../SolarSys/lunaform.html
• Hartmann, William K. and Davis, Donald, “Origin of the Moon”, Planetary Science Institute, February 22, 2006
http://www.psi.edu/projects/moon/moon.html
• Wikipedia, “Roche limit”, Wikimedia Foundation, Inc., February 20, 2006, February 22, 2006
http://en.wikipedia.org/wiki/Roche_limit