our moon and other moons of the solar system
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Our Moon and other moons of the Solar System. Starter 1/25/13. What do you already know about our Moon?. What is a moon?. A moon is a natural satellite of a planet or dwarf planet There are over 170 moons around the planets and dwarf planets in our solar system. Planets and numbers of moons. - PowerPoint PPT PresentationTRANSCRIPT
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Our Moon and other moons of the Solar System
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Starter 1/25/13
• What do you already know about our Moon?
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What is a moon?
• A moon is a natural satellite of a planet or dwarf planet
• There are over 170 moons around the planets and dwarf planets in our solar system
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Planets and numbers of moonsPlanet Number of known moonsMercury 0Venus 0Earth 1Mars 2Jupiter 63Saturn 63Uranus 27Neptune 13
Dwarf planetPluto 3 (maybe 4)Eris 1
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How do we explain the existence of our Moon?
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Giant Impact Theory• Between 4.4 and 5 billion years ago an object
about the size of Mars struck a very young Earth and blasted material into orbit around Earth– The “youngest” Moon rocks are 4.4 billion years old
• The material from the collision came together by gravity (called accretion) and became our Moon.
• The Moon was much closer to the Earth when it first formed– It was between12,000-18,000 miles away– Now it is 240,000 miles away and moving away from
us by 1.5 inches/year
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Giant Impact
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Why does the Moon look the way it does?
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Impact Cratering
• Most cratering happened soon after the solar system formed – “the Late Heavy Bombardment”
• Craters are about 10 times wider than object that made them.
• Small craters greatly outnumber large ones.
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Impact Craters
Meteor Crater (Arizona) Tycho Crater (Moon)
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Impact Craters on Mars
“Standard” crater Impact into icy ground
Eroded crater
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Thought question
Shouldn’t the Earth be covered in craters too? Why isn’t it?
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Volcanism
• Volcanism happens when molten rock (magma) finds a path through the Earth’s crust (lithosphere) to the surface.
• Molten rock is called lava after it reaches the surface.
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Lava and Volcanoes
Runny lava makes flat lava plains.
Slightly thicker lava makes broad shield volcanoes.
Thickest lava makes steep stratovolcanoes.
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The Lunar Maria were formed by volcanism
• Smooth, dark lunar maria are less heavily cratered than lunar highlands.
• Maria were made by floods of runny lava.
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Formation of Lunar Maria
Large impact crater weakens crust.
Heat build-up allows lava to well up to surface.
Early surface is covered with craters.
Cooled lava is smoother and darker than surroundings.
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The Moon is geologically dead• Moon is considered
geologically “dead” because geological processes have virtually stopped.
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Do the Moon and Mercury have any atmosphere?
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Exospheres of the Moon and Mercury
• Sensitive measurements show that the Moon and Mercury have virtually no atmosphere.
• The little gas there comes from impacts and the solar wind that eject surface atoms.
Earth’s Moon Mercury
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The Moon’s surface conditions
• No atmosphere• No liquid water – frozen
water at the poles• Because of the lack of an
atmosphere the moon experiences extreme temperatures– Daytime = 130C (265°F)– Nighttime = -190C (-310 F)
• The moon has 1/6th of Earth’s gravity
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Starter 2/7
• Identify one similarity and one difference between our Moon and the other moons of the solar system?
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What kinds of moons orbit the other planets of the solar system?
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Sizes of Moons
• Small moons (< 300 km) “irregular”– No geological activity
• Medium-sized moons (300–1500 km) “regular”– Geological activity in the past (mostly)
• Large moons (> 1500 km) “regular”– Ongoing geological activity (mostly)
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Small (or irregular) Moons
• These are far more numerous than the medium and large moons.
• They do not have enough gravity to be spherical: Most are “potato-shaped.”
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• They are captured asteroids or comets, so their orbits do not follow usual patterns – *retrograde and tilted orbits
Small (or irregular) Moons
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Captured Moons
• Mars has two moons (Phobos and Deimos) that are thought to be captured asteroids from the asteroid belt
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Medium and Large (regular)
Moons• Enough self-gravity to be spherical
• Often have substantial amounts of ice
• Except for our Moon they formed in orbit around jovian planets (gas giants) *by accretion
• Circular orbits in same direction as planet rotation *around equator
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Jupiter’s Galilean moons
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Io
• Io is the most volcanically active body in the solar system
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Io’s Volcanoes
• Volcanic eruptions continue to change Io’s surface.
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Europa
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Europa’s interior also warmed by tidal heating producing a possible ocean under the ice.
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Ganymede
• Largest moon in the solar system
• Clear evidence of geological activity
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Callisto
• “Classic” cratered iceball
• No evidence of geologic activity
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Other interesting moons in the solar system
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Titan
• Saturn’s largest moon Titan is the only moon in the solar system to have a thick atmosphere.
• It consists mostly of nitrogen with some argon, methane, and ethane.
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Titan’s Surface
• Huygens probe provided first look at Titan’s surface in early 2005.
• It found liquid methane and “rocks” made of ice.
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Enceladus• Enceladus is a
medium sized moon of Saturn
• Ice fountains of Enceladus suggest it may have a subsurface ocean.
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Charon
• The largest moon of Pluto is also the largest moon relative to the size of its planet
• Charon is ½ the size of Pluto, and is thought to be ice-covered like Pluto as well
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Top 12 largest moons in the solar system
1. Ganymede2. Titan3. Calisto4. Io5. The Moon6. Europa
7. Titania8. Rhea9. Oberon10. Iapetus11. Charon12. Umbriel
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Top 10ish moons in the solar system (with other terrestrial bodies for comparison)