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Small Bodies of the Solar System
Dwarf Planets, Asteroids, Meteoroids/ Meteors/Meteorites and Comets
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I. What makes a Planet a Planet??
According to the International Astronomical Union (IAU), “A planet: is a body that orbits the Sun, is massive enough for its own mass (and gravity) to make it round, and has "cleared its neighborhood" of smaller objects around its orbit. ”
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I. What makes a Planet a Planet??
Planetary vs. Dwarf Planet Characteristics What makes a planet, according to the definitions adopted by the IAU - Characteristic Planet Dwarf Planet Is in orbit around the Sun Yes Is in orbit around a planet (satellite) No Has sufficient mass (and gravity) to assume a nearly round shape Has cleared the neighborhood around its orbit
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I. What does a Planet have that a Dwarf Planet does not have??
Planetary vs. Dwarf Planet Characteristics What makes a planet, according to the definitions adopted by the IAU - Characteristic Planet Dwarf Planet Is in orbit around the Sun Yes Is in orbit around a planet (satellite) No Has sufficient mass (and gravity) to assume a nearly round shape Has cleared the neighborhood around its orbit
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II. Earth’s Moon is awfully big: why isn’t it a Dwarf Planet?
Dwarf Planet vs. Moon Characteristics What makes a planet, according to the definitions adopted by the IAU - Characteristic Earth’s Moon Dwarf Planet Is in orbit around the Sun No Yes Is in orbit around a planet (satellite) Has sufficient mass (and gravity) to assume a nearly round shape Has cleared the neighborhood around its orbit N/A
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3A. What does a Dwarf Planet have that an Asteroid does not have??
Dwarf Planet vs. Asteroid Characteristics What makes a planet, according to the definitions adopted by the IAU - Characteristic Asteroid Dwarf Planet Is in orbit around the Sun Yes Is in orbit around a planet (satellite) No Has sufficient mass (and gravity) to assume a nearly round shape Has cleared the neighborhood around its orbit
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The 3rd Dwarf Planet NOT a Dwarf Planet
3A. Ceres – the largest object in the Asteroid Belt: Orbits the sun has enough mass to assume a round shape Will be visited by Dawn mission Feb – July, 2015 The 3rd Dwarf Planet NOT a Dwarf Planet 3B. Vesta – a smaller Asteroid: Also orbits the sun Does not have enough mass to assume a round shape Was visited by Dawn mission in
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Asteroid Vesta As viewed by the Dawn spacecraft
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II. The First 3 Dwarf Planets
Luna – Earth’s Moon Not a dwarf planet – it orbits the Earth! IIA) Eris and its moon Dysnomia (found in the Scattered Disk) II. The First 3 Dwarf Planets IIB) Pluto and its moon Charon (found in the Kuiper Belt)
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IIA) Eris – is the largest object in the Scattered Disk region:
Greek goddess of Strife and Discord Tossed from the Kuiper Belt into the Scattered Disk by gravitational interaction with Neptune. Average distance from the Sun is 67.7 AU Its orbit is highly eccentric – varies from 38.3 AU to 97.7 AU.
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IIA) Eris – is the largest object in the Scattered Disk region:
Takes about 560 years to orbit the sun Discovered in 2003, then classified a Dwarf Planet along with Pluto and Ceres in 2006. Temperature ranges from -217 oC to -243 oC – Brrr!! Has 1 moon – Dysnomia (named for the goddess of lawlessness)
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Eris and Dysnomia Artist’s View Photo from HST
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The Scattered Disk Home to Asteroids, Some Comets
and Dwarf Planet Eris
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Scattered Disk and Eris’ Orbit
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2C) Pluto – is the largest object in the Kuiper Belt:
Discovered in 1930 and named the 9th planet Reclassified as a Dwarf Planet in 2006. Name for the Roman god of the Underworld Temperature hovers around from -225 oC – Still Brrr!! Has 1 large moon – Charon
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2C) Pluto – is the largest object in the Kuiper Belt:
Pluto may have been a moon of Neptune which collided with Triton, which was not a moon of Neptune at first but is now!! (and it orbits backwards)!!
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2C) Pluto – is the largest object in the
Kuiper Belt: Average distance from Sun is AU Orbit highly eccentric – AU AU. Takes about 248 years to orbit the sun Takes 6.4 days to rotate on its axis (and it does so backwards – retrograde )
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2C) Pluto – is the largest object in the
Kuiper Belt: Rocky core surrounded by a mantle of water ice, with methane and nitrogen ice frosting its surface. Pinkish color of surface may be due to complex organic compounds Has a temporary atmosphere when it is closer to the sun, thawing the methane and nitrogen frost. Has 225 mph winds, but thin air makes them feel like 1 mph breeze on Earth.
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The Kuiper Belt Where Some Meteorites and a Few Comets Originate and Where Dwarf Planet Pluto is Found
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Kuiper Belt and Pluto’s Orbit
Pluto will be visited by the New Horizons spacecraft in July, 2015
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Water Ice Mantle Rocky Core
Methane/Nitrogen “Frost” coats the surface. Water Ice Mantle Rocky Core Click on star for Video – “Why Pluto is Not a Planet”
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IID) Trans-Neptunian Objects (TNOs) – Eris, Pluto and other objects found out past the orbit of Neptune in the Kuiper Belt and Scattered Disk regions: Haumea, Makemake and other possible candidates for “dwarf planethood”
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IIE. Ceres - is the largest object in the Asteroid Belt. Ceres:
Originally called a planet when discovered in 1801. Reclassified as the largest Asteroid in 1802. Reclassified again as a dwarf planet in 2006, but (It’s OK to still call it the largest Asteroid.) Contains 1/3 of the total mass of the Asteroid Belt! Is about 2.77 AU from the sun Is about ¼ the diameter of Earth’s Moon - about 950 km in diameter Moon Ceres The 3rd Dwarf Planet Earth
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The 3rd Dwarf Planet IIE. Ceres - is the largest object in the
Asteroid Belt. Ceres: Thought to have a rocky core overlain by an icy mantle and an outer surface of water ice mixed with dust (clay and CO3) May have liquid water under the surface The 3rd Dwarf Planet
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The 3rd Dwarf Planet IIE. Ceres - is the largest object in the
Asteroid Belt. Ceres: May have a thin atmosphere of sublimated water (ice vapor) Much rounder than most Asteroids – due to its mass Will be visited by Dawn mission from February to July, 2015 The 3rd Dwarf Planet
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3A. What does a Dwarf Planet have that an Asteroid does not have??
Planetary Characteristics What makes a planet, according to the definitions adopted by the IAU - Characteristic Dwarf Planet Asteroid Is in orbit around the Sun Yes Has sufficient mass to assume a nearly round shape No Is not a satellite (moon) Has cleared the neighborhood around its orbit Has not cleared the neighborhood around its orbit
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III. The Asteroid Belt Where Meteorites Come From and
Where Dwarf Planet Ceres is Located
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III. The Asteroid Belt IIIA. The asteroid belt contains:
1 dwarf planet (Ceres – 950 km across) 200 large asteroids ( km across) 750,000 medium-sized asteroids (> 1 km across) Millions of tiny asteroids and meteoroids. IIIB. Asteroids are also found: in Neptune’s orbit (called Trojan Asteroids) and a trio of Asteroid groups patrolling the inner solar system known as the Near-Earth Asteroids (including the Apollo Asteroids).
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Other Asteroids – “Space Potatoes”
Lutetia – a smaller Asteroid: Also orbits the sun Does not have enough mass to assume a round shape
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3C. Asteroids vs. Meteoroids
IIIC. The official definition of a meteoroid: “A meteoroid is a solid object moving in interplanetary space, of a size considerably smaller than an asteroid and considerably larger than an atom.” The distinction between meteoroid and asteroid: Traditionally, anything smaller than 10 meters across was called a meteoroid. (A meteoroid would fit inside our classroom.) Anything greater than 10 meters across is called an asteroid (until you get to Dwarf Planet size!!).
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4. Meteoroids vs. Meteors vs. Meteorites
IV. Asteroids and meteoroids both refer to solar system objects that orbit the Sun but are not large enough to be deemed planets. Meteoroid: any Sun-orbiting object smaller than 10 meters across. (still out in space) Meteor: visible path of a meteoroid whose surface is vaporizing as it enters Earth's atmosphere (sometimes called a shooting star). Meteorite: If a meteoroid survives the fall through Earth’s atmosphere as a meteor and lands on Earth’s surface, it becomes a meteorite. Up to 10,000 tons of meteoritic material fall to Earth every day (mostly tiny pieces - micrometeorites.)
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Meteoroid Meteor Meteorite
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4. Meteoroid to Meteor to Meteorite
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Meteor Showers Meteor
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Large Meteoroid Fragmenting In Atmosphere
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Meteors
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February, 2013 – Chelyabinsk Meteorite punches hole in ice in nearby lake.
October, 2013 – 1500 lb chunk of meteorite is retrieved from lake!
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IVE. Three main groups of meteorites
Iron meteorites are almost completely metal Stony-iron meteorites have nearly equal amounts of metal and silicate crystals Stony meteorites are dominated by silicate minerals. There are some rare stony meteorites called Martian meteorites because they were blasted off of the surface of Mars and landed here on Earth!
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Meteorites Stony Iron Iron Stony Iron Iron
A sawed iron meteorite showing criss-crossing Widmanstatten texture. Stony Iron Iron
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To view raw footage of Chelyabinsk meteor and meteorite impact, click:
To view NDGT interview re: Chelyabinsk meteor and meteorite impact, click: To view video of huge 1300 lb meteorite retrieved from lake near Chelyabinsk, click:
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The Oört Cloud Where Comets Come From
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Comet ison Approaching the Sun october - november, 2013
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Comet ison october - november, 2013
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Comet ison october - november, 2013
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Current indications are…no.
Will ISON survive?... Scenario 1: Fizzle: ISON evaporates under intense tidal forces and solar radiation Scenario 2: Break-Up: ISON breaks up into smaller chunks (could happen at any time) Scenario 3: Sizzle: ISON survives and emerges so bright that it may be visible on Earth even if daylight! Current indications are…no. It appears to have broken up into 1000s of pieces as it “grazed” the sun (Scenario 2).
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To view animation of Life Cycle of a typical comet:
To view animation of approach and destruction of Comet Ison, October - December, 2013:
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