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Asteroid
Small celestial bodies
Planetoids
Asteroid big enough to land spaceship
Trojan
Asteroids that share orbit with a large planet or moon
Comets
Dusty snowballs that orbit the sun
Periodic comets
Comets with eccentric orbits that may bring them to the sun at one point
Non-periodic
Appears more than 200 years or even thousand or million of years
Coma
Unstable atmosphere around the comet formed by the released dust and gas
Meteoroids
Commonly known as “shooting star”
Micrometeoroids
Tiny meteoroids or referred as cosmic dust
Meteorite
Chunk of asteroid that sometimes make it through the atmosphere to the ground
Halley’s Commet
Appears once every 75-76 years
Kuiper Belt and Oort Cloud
Origin of comets
Dust, rocks, metals, ice, ammonia, methane, carbon dioxide
Chemical composition of comets
High eliptical (75-100,000 years)
Orbit of comets
Provides clues to how water was formed on Earth
Importance to research of comets
1-10 nuclei
Size of comets
Asteroid Belt
Origin of meteors
About 1 inch
Size of meteors
Fragments of comets and asteroids, iron, stone, stony-iron, chrondites
Chemical composition of meteors
No orbit because it is in the Earth’s atmosphere
Orbit of meteors
Provides information of star formation
Importance to research of meteors
Asteroid Belt
Origin of asteroids
1-100++
Size of asteroids
Dust rock, silicate, iron, nickel, olive, pyroxene
Chemical composition of asteroids
More rounded (1-100)
Orbit of asteroids
Provides information of Earth’s interior
Importance to research of asteroids
Silicate
Allows celestial bodies to reflect light
Nucleus
“dirty snowball” made of ice
Nucleus, coma, dust tail, ion tail
Parts of comet
Oort Cloud
Located beyond the solar system where long-period comets originate
Kuiper Belt
Located beyond Neptune’s orbit where short-period comets originate
Asteroid Belt
Located between Mars and Jupiter where asteroids originate
lightyear
Unit of measurment for distance in space