Cryogenian oor Viëtnamees
Cryogenian
en
(geology) of a geologic period within the Neoproterozoic era from about 850 to 600 million years ago
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Kỷ Cryogen
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In contrast to most other time periods, the beginning of the Cryogenian is not linked to a globally observable and documented event.
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During the Cryogenian period, however, Earth's continents were all at tropical latitudes, which made this moderating process less effective, as high weathering rates continued on land even as Earth cooled.
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The deposits of glacial tillite also occur in places that were at low latitudes during the Cryogenian, a phenomenon which led to the hypothesis of deeply frozen planetary oceans called "Snowball Earth".
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