Our solar system is filled with millions of leftovers – the chunks of rock and ice that weren’t incorporated into the planets and moons. The icy ones are known as comets, while the rocky ones are asteroids. But there’s not that much difference between them. They have similar ingredients, but in different amounts. How we classify them has more to do with where they were born and how close they get to the Sun.
The planets formed from a disk of material that encircled the infant Sun. Small grains of ice and rock stuck together to make larger bodies. These larger objects then stuck together to make the planets and some of their moons.
In the outer solar system, it was cold enough for these building blocks to contain a lot of ice. But closer to the Sun it was hotter, so the building blocks consisted mainly of rock and metal.
The outer planets kicked many of the leftovers deeper into space. One of them occasionally falls toward the Sun. Solar energy vaporizes some of the ice, releasing some of the solid particles as well. The Sun pushes some of this gas and dust away, forming a long, bright tail – a comet.
Many asteroids have a fair amount of ice as well, just not enough to make a tail. Most asteroids are concentrated in a broad belt between Mars and Jupiter. About one-and-a-half million have been cataloged, with millions more awaiting discovery – leftovers from the birth of the solar system.
Script by Damond Benningfield
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