At the beginning of the last ice, local mountain glaciers grew and formed large ice sheets, like the one seen here. (CREDIT: Creative Commons)
For quite some time, paleo-climate specialists have been perplexed by two enigmas: What was the origin of the ice sheets that defined the final ice age, and how could they expand so rapidly?
A fresh research conducted by the University of Arizona's experts suggests a plausible explanation for the swift expansion of the ice sheets that coated a considerable portion of the Northern Hemisphere during the last ice age. Furthermore, the study's findings may be applicable to other glacial periods in the Earth's past.
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