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The Moon
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MOON FACTS Natural satellite of earth Gravity 1/6 of earth - WHY?
No atmosphere - WHY? Temp. difference: 134 C to -170 C -WHY?
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LUNAR SURFACE Light areas - rough highlands
Dark areas - Maria - solidified lava Rilles - long deep channels running through maria. Regolith - layer of dust on surface
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Man on the Moon
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Craters Bowl shaped depressions Most formed millions of years ago
Rays - “splash marks” caused by recent collisions
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Types of Craters Simple Crater Complex Crater
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Moon Rocks
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Basalt Dark colored Fine Grained Rich in magnesium, titanium and iron
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Anorthosites Light-colored coarse-grained rich in calcium and aluminum
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Breccia fragments of several rocks melted together formed impact
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Moon Formation - Stage One
. Mars-size planet hits earth hurling fragments of earth into orbit
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Moon Formation Stage 2 Surface covered with hot molten rock. Densest materials sank to the center.
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Moon Formation - Stage 3 Outer surface cooled forming thick
solid crust. Maria formed as meteorites struck moon surface and molten lava flowed up to the surface.
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INTERIOR OF MOON Crust - 60 to 100 km thick composed mainly of oxygen and silicon. Mantle km thick composed of silica, magnesium, and iron. Core - <700 km composed of iron.
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