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Published byCurtis Booker Modified over 9 years ago
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Moons
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Many moons in our Solar System They have craters, volcanoes, possibly underground oceans A radar mapping image made by the Cassini spacecraft of a flyover area on Saturn's giant moon Titan showing an ice volcano
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Satellites Natural (not man made) or artificial bodies that revolve around larger bodies such as planets are called satellites Mercury and Venus have no natural satellites All other planets have moons (satellites)
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Luna: The Moon of the Earth Solar system is 4.6 billion years old Based this data from lunar rocks brought back from Apollo mission
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Surface of the Moon Impact craters on the moon tell the age of the moon If the surface is young, there hasn't been time for many craters to form Different parts of the surface of the Moon exhibit different amounts of cratering and therefore are of different ages
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Lunar Origins Formation of the moon happened in three steps 1 st Impact – large body collided with earth, blasted part of Earth’s mantle in space 2 nd Ejection – sent mantle debris from Earth and from impacting body (including its iron core) 3 rd Formation – debris orbited around Earth and began to join together
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Moon Formation http://vimeo.com/20 15273 http://vimeo.com/20 15273
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Phases of the Moon http://www.sumanasinc.com/webcontent /animations/content/moonphase.html http://www.sumanasinc.com/webcontent /animations/content/moonphase.html Waxing – sunlit fraction is getting larger Waning – sunlit fraction is getting smaller Moon always gets same amount of sun( same as Earth) You always see same side of the moon
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Phases of the Moon Appearance of the moon from its changing position relative to Earth and the sun As moon revolves around Earth, amount of sunlight on the side of the moon that faces Earth changes Called Phases
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Waxing and Waning Waxing – sunlit fraction is getting larger Waning – sunlit fraction is getting smaller Crescent – croissant shaped or fingernail clipping Gibbous – bulging outward
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Phases
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