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The Little Ice Age

The Little Ice Age — abbreviated LIA — was a period of cooler climate in the Northern Hemisphere that began roughly in the late 13th century, peaked in the 17th, and ended in the mid-19th. It is the reason why Chamonix, Grindelwald and Innsbruck all have church records of glaciers reaching their pre-1850 maxima and of villages buying mass against threatening ice.

When it happened

Estimates vary. Most glaciologists date the LIA from around 1300 to 1850, with peaks of cold in the 1650s and 1810s. The cold was not uniform — some decades were nearly modern in warmth — but the overall climate was 1-1.5 degrees cooler than today.

Why it happened

Multiple causes interact:

How glaciers responded

Alpine glaciers grew to their largest extent of the last 9 000 years during the LIA. Many descended into agricultural valleys — the Mer de Glace and the Lower Grindelwald glacier each destroyed villages. Mass services and processions were held to plead with glaciers to retreat.

Why we still see it

The maps and moraine ridges that visitors encounter at most alpine glaciers — the boundary between forested slopes and bare gravel, typically 1-2 km below the current snout — mark the LIA maximum. The "trim line" visible on many cliffsides is the upper limit of LIA ice thickness.

Visiting LIA evidence

Explore on the map

Toggle the "LIA maximum" overlay on the interactive map to see the dramatic difference between 1850 ice cover and today's.