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Non-clastic sedimentary rocks form from the precipitation (Precipitation is the separating of a solid from a solution) of minerals from ocean water or from the breakdown of the shells and bones of sea creatures. Igneous material erupts onto the floor of the continents or onto the seafloor to kind volcanic rocks, which might react with seawater to vary the chemical composition of both. The hot button is that Earth’s mantle has been step by step cooling because the planet fashioned, and because it cools, it releases fewer volcanic gases comparable

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