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Solar System: The Snow Line

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The snow line, also known as the ice line, is a point in our solar system somewhere between Mars and Jupiter which separates the regions for formation of the high-density Terrestrial planets from the low-density Jovian planets. This line refers to the kind of matter that can condense in a particular region depending on the temperature of gas there.

The closer a planet is to the sun, the hotter the temperature, meaning that compounds with high-melting points such as metal oxides and pure metals, which are very dense, are the only materials that could form grains. As you move away from the sun the temperature gets cooler and more materials can form into grains; next in line after metals would be silicates, which are rocky materials. The Terrestrial

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