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Chapter 25 – The Moon Section 25.1
Astronomy The study of the universe
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Origin of the moon A planet-sized object impacted/collided with Earth Moon’s is made of same materials as Earth’s Crust Moon has a core – more dense materials at the core, less dense materials on the surface
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Moon’s Surface Meteoroids(icy/rocky fragments in space) impacted the moon, leaving craters Craters are depressions in Earth’s Surface
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Most all impacts are from micrometeoroids (very, very small) about the size of a sand grain
The moon today
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Moon’s Structure Iron Core, partially molten area around the core, surrounds by a solid region and a crust Density is 3.3g/cm3 whereas Earth is 5.5g/cm3. Therefore, the moon formed from mostly crust materials from Earth
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Moon Properties We only see the front side of the moon The moon rotates on its axis at the same period that it make one complete orbit around the Earth
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Features of the Moon Maria
Rille Lunar (moon) highlands Regolith dark areas (latin for Sea) Not water but actually dark basalt rock Trench-like valleys Areas of Lighter colored rock - breccia Lunar soil
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