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Vanderbilt: Geochemical Analysis From the Last Ice Age May Hold Clues for Future Climate Change and Preparedness Strategies
July 15, 2020
NASHVILLE, Tennessee, July 15 -- Vanderbilt University issued the following news:

Stalagmites from Lake Shasta Caverns (LSC) - located in northern California within an important transitional climate zone between the Pacific Northwest and southwestern United States - hold geochemical clues to help researchers understand how climate changed during the end of the last ice age (14,000 - 37,000 years ago) and predict what may happen amid climatic changes in modern times.

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