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At various times in the geologic past, the Earth had dense forests in low-lying wetland areas. Due to natural processes such as flooding, these forests were buried underneath soil. As more and more soil deposited over them, they were compressed.


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Factors that can shape climate are called climate forcings or “forcing mechanisms”. These include processes such as variations in solar radiation, variations in the Earth’s orbit, variations in the albedo or reflectivity of the oceans.

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