Nathaniel J. Lorentz, Frank A. Corsetti
Abstract
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The concept of a Neoproterozoic “snowball Earth”–an ice age in the tropics ([Kaufman, 1997][1])–has captured the imagination of the public and scientists alike. The idea of global-scale glaciation, indicated by the abundance of Neo-proterozoic glacial deposits (some with low-latitude
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The concept of a Neoproterozoic “snowball Earth”–an ice age in the tropics ([Kaufman, 1997][1])–has captured the imagination of the public and scientists alike. The idea of global-scale glaciation, indicated by the abundance of Neo-proterozoic glacial deposits (some with low-latitude
Key concepts: Geology, Snowball Earth, Earth (classical element), Test (biology), Paleontology, Mathematics, Glacial period, Mathematical physics