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Published byLeona James Modified over 8 years ago
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A natural satellite The only moon of the planet Earth One of more than 96 moons in our Solar System
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About 384,000 km (240,000 miles) from Earth Earth’s radius = 6378 km or 3963 miles Moon’s radius = 1738 km or 1080 miles About ¼ size of Earth
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If earth were a basketball, then the moon would be a tennis ball 23.5 feet away
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“Born” 4-5 billion years ago Formed from impact of Mars-sized “planetesimal” on Earth Debris from both objects melted together to form the moon
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No atmosphere No liquid water 1/6 Earth’s gravity Because the moon has less mass than the earth does (1/80 of earth), its gravity is weaker Extreme temperatures Daytime 130 o C (265 o F) Nighttime -190 o C (-310 o F)
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Maria Rilles Craters Highlands Lunar Rocks
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Highlands – mountains up to 7500 meters (25,000 feet) tall Rilles – trenchlike valleys that look somewhat like a dry riverbed. Were probably lava channels when the moon was volcanically active. Some as long as 240 km.
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Originally thought to be “seas” by early astronomers Darkest parts of lunar landscape Filled by lava after crash of huge meteorites on lunar surface 3-4 billion years ago Mostly basalt rock
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Up to 2500 km (1,553 miles) across Most formed by meteorite impact on the Moon Some formed by volcanic action inside the Moon
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The oldest moon rock is 4.3 billion years old Moon rocks contain many of the same elements that occur in the earth’s rocks, but in slightly different proportions Moon surface rocks are deficient in elements with low melting points, such as sodium Minerals in moon rocks do not contain water Surface rocks on the moon are about as dense as those on the surface of the earth
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Crust – average thickness of about 70 km Mantle Made up of dense rock that is probably rich in silica, magnesium, and iron Reaches to a depth of about 1,000 km Core – radius is between 300 and 425 km
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First seen by Luna 3 Russian space probe in 1959 Surface features different from near side More craters Very few maria Thicker crust
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Orbit of moon around the earth forms an ellipse, not a circle The moon rises and sets 50 minutes later each night Moon rises in the east and sets in the west Revolution – Moon orbits the Earth every 27 1/3 days Rotation – Moon turns on its axis every 27 days Same side of moon always faces Earth Observers on Earth can see about 59% of surface of moon
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When the moon is between the Earth and the Sun Moon casts a shadow on part of the Earth Total solar eclipses are rare – only once every 360 years from one location on Earth
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Occurs when the Earth is positioned between the moon and the sun, and the Earth’s shadow crosses the lighted half of the moon This shadow darkens the moon About 2-3 per year Lasts up to 4 hours
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Moonlight is reflected sunlight Half the moon’s surface is always reflecting light From Earth we see different amounts of the Moon’s lit surface The amount seen is called a “phase”
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FULL CRESCENT QUARTER GIBBOUS
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New moon Waxing Crescent moon First Quarter moon Waxing Gibbous moon Full moon Waning Gibbous moon Third Quarter moon Waning Crescent moon New moon
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Tides caused by pull of Moon’s gravity on Earth High tide – Side facing Moon and side away from Moon Every 12 hours, 25 ½ minutes Low tide – On sides of Earth
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1950s to 1960s - probes Neil Armstrong First man on the Moon – July 20, 1969 Six Apollo missions (1969-1972) 382 kg (842 lbs) rocks 12 Americans have walked on the moon
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The 3 basic units of most calendars – day, month, and year – are determined by the movements of the earth and the moon Day – time required for the earth to make one rotation on its axis (about 24 hours) Month – time required for the moon to go through one cycle of phases as it orbits the earth (29.5 days) Year – time required for the earth to make one orbit around the sun (about 365.24 days)
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All planets except Mercury and Venus have moons In addition, Saturn, Jupiter, Uranus, and Neptune have rings Mars has 2 moons (Phobos and Deimos) that revolve around Mars quite rapidly Jupiter has at least 17 moons and most are very small. The 4 largest satellites of Jupiter are called Galilean Moons because they were first seen by Galileo in 1610 Saturn has at least 18 moons. Most are small, icy bodies with many craters Uranus has at least 20 small moons Neptune has 8 known moons (Triton and Nereid are among the 8) Pluto has 1 moon, Charon, that was discovered in 1978
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