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The retreat of glaciers since 1850 is a well-documented effect of climate change. The retreat of mountain glaciers provide evidence for the rise in global temperatures since the late 19th century. Examples include mountain glaciers in western North America, Asia, the Alps in central Europe, and tropical and subtropical regions of South America ...
The Holocene glacial retreat is a geographical phenomenon that involved the global retreat of glaciers (deglaciation) that previously had advanced during the Last Glacial Maximum. Ice sheet retreat initiated ca. 19,000 years ago and accelerated after ca. 15,000 years ago.
The Little Ice Age was a period from about 1550 to 1850 when the world experienced relatively cool temperatures compared to the present. Subsequently, until about 1940 glaciers around the world retreated as the climate warmed. Glacial retreat slowed and even reversed, in many cases, between 1950 and 1980 as a slight global cooling occurred ...
1 Retreat of glaciers since 1850. Toggle Retreat of glaciers since 1850 subsection. 1.1 Review section. 1.2 FARC section. Toggle the table of contents.
Glacier retreat primarily refers to the retreat of glaciers since 1850. It may also refer to: Glacial retreat, a type of glacial motion; Deglaciation, the widespread retreat of glaciers at the end of an ice age; Holocene glacial retreat, a period of deglaciation occurring between 20,000 and 10,000 years ago
Retrieved from "https://en.wikipedia.org/w/index.php?title=Glacial_retreat&oldid=1024723398"This page was last edited on 23 May 2021, at 19:43
The retreat of glaciers since 1850 is a well-documented effect of climate change. The retreat of mountain glaciers provide evidence for the rise in global temperatures since the late 19th century. Examples include mountain glaciers in western North America, Asia, the Alps in central Europe, and tropical and subtropical regions of South America ...
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