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The Moon
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maria: smooth, dark areas of the moon- reflect little light
Lunar Surface maria: smooth, dark areas of the moon- reflect little light maria are plains of dark solidified lava
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craters: bowl-shaped depressions on the moon
lunar craters are formed from impacts of debris
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regolith: layer of dust and rock that covers the moon’s surface
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Interior of the Moon
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Why does the same side of the moon always face us?
Because the moon rotates and revolves at the same speed (27 1/3)
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Eclipses when one planetary body passes through the shadow of another
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solar eclipse: when the moon is directly between the Earth and the sun
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lunar eclipse: when the Earth is directly between the moon and the sun
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Eclipses don’t occur every month because the moon’s orbit is tilted with respect to the Earth’s orbit
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Moon Phases phases: various shapes of the moon lighted by reflected sunlight
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waxing: when the size of the visible portion of the moon is increasing
waning: when the size of the visible portion of the moon is decreasing
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new moon: no lighted area of the moon is visible from the Earth
full moon: entire half of the side of the moon facing Earth is lit
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crescent: less than half of the side facing the Earth is lit
gibbous: more than half of the side facing the Earth is lit
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New moon Waxing crescent 1st quarter Waxing gibbous
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Full moon Waning gibbous Waning crescent 3rd quarter
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Tides tides: daily changes in the level of the oceans
-caused by the moon’s gravitational pull -tide changes every 6 hours
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Tide animation: The spinning Earth within a slightly elliptical ocean results in the rising and falling of the ocean surface, with respect to the land, over the course of a day. For each 24 hour period there are two high tides and two low tides as the Earth rotates through each of the two bulges of the the ocean surface
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spring tide: tide with maximum daily tidal range that occurs during new and full moons
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neap tides: tides with minimum daily tidal range that occurs during 1st and 3rd quarter moons
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