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Which mountain regions experienced glacier advances during the Little Ice Age?

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Line graph showing estimated temperature variations from 1000 to 2000 CE for the Northern Hemisphere and central England, with three lines representing different data sources. The chart highlights the medieval warm period around 1100-1300 and the Little Ice Age from about 1500 to 1850, followed by a sharp temperature rise in the late 20th century. Temperature is shown as deviations from the 1961-1990 average. — Little Ice Age Estimates of temperature variations for the Northern Hemisphere and central England from 1000 to 2000 ce.

During the Little Ice Age (roughly 14th–19th century), mountain glaciers expanded in several regions across the globe. Documented areas of glacier advancement include:

The European Alps: Glaciers in this region advanced significantly, in some cases extending far below their previous and present limits, which impacted local human settlements.12
Alaska: Glacial expansion was recorded in this region during the period.12
New Zealand: Glaciers in New Zealand also experienced periods of advancement.2
The Andes: Advances were observed in the southern Andes, as well as in equatorial latitudes such as the Andes of Colombia.12
Patagonia: Cooler conditions in the Southern Hemisphere initiated the advance of glaciers in this region.2
Japan: Glaciers in Japan also advanced during this climate interval.2
Sierra Nevada: Glacier advances were recorded in this mountain range as well.1

It is important to note that these regional glacial advances did not always occur simultaneously, as the climate interval was characterized by significant spatial and temporal variability in temperature and precipitation.2