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Little Ice Age

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Little Ice Age [′lid·əl ′īs ‚āj]
(geology)
A period of expansion of mountain glaciers, marked by climatic deterioration, that began about 5500 years ago and extended to as late as A.D. 1550-1850 in some regions, as the Alps, Norway, Iceland, and Alaska.


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Glaciers in both the tropics and North Atlantic region reached their most recent maximum extents during the so-called Little Ice Age, about 1650 AD to 1850 AD, according to the scientists conducting the research.
Another Little Ice Age story, presented in one of the book's insets, relates climate change to the special sound of Stradivarius violins.
800 to 1300 and was followed by the Little Ice Age.
 
 
 
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