Climate Change & Geologic History at Glacier National Park

Black and white photograph of an alpine pass with a small glacier and a moraine in the foreground. A person is on the left in the distance.

This photograph of the Clements Glacier moraine at Logan Pass was taken in 1928 by W.C. Alden for the USGS.

Imagine a cold snap that lasts ten thousand winters.

When that happens, and more snow falls in the winters than can melt in the summers, you are probably in an ice age. For thousands of years this landscape has been shaped by the natural advance and retreat of colossal glaciers carving out the U-shaped valleys we admire today. For about 10,000 years now we have been in a warmer interglacial period.

If left to its own swings, our climate would be poised for another cold period soon (give or take a few thousand years) but human-caused climate change may have already postponed the next ice age.

A squiggly orange line graph that goes up and down from left to right on a white background with no labels.
This orange line shows the natural rise and fall of Earth’s temperature over the past 400,000 years and was adapted from Petit et al. Nature 1999. The left end is 400,000 years ago and the right end is today. Higher is warmer and lower is colder.
A graph showing natural rise and fall of the planet's temperature also illustrates how ice ages have come and gone. When temperatures were warm, glaciers retreated, when they were cold, the glaciers advanced.

The park’s current glaciers probably formed about 7,000 years ago and were at their largest size at the end of the Little Ice Age then started to retreat with the onset of a warming trend.

Logan Pass is an excellent place to get an up-close look at geologic evidence of the Little Ice Age, a cold period that lasted from roughly 1300 to 1850. The park’s current glaciers reached their largest size during that period.
Black and white image of a steep mountainous landscape with a glacier on the left side.

Morton J. Elrod took this image of Clements Glacier (just left of center) in 1914.

Logan Pass is an excellent place to get an up-close look at geologic evidence of the Little Ice Age, a cold period that lasted from roughly 1300 to 1850. The park’s current glaciers reached their largest size during that period.

The onset of a warming trend at the end of the 1800s melted many of this area’s smaller glaciers. Clements Glacier, shown here in 1914, was located near the modern-day trail to Hidden Lake Overlook.

Clements Glacier largely melted away at the end of the Little Ice Age, without much influence from modern climate change. Other glaciers in the park endured after the end of the Little Ice Age, though significantly smaller.

Some of the larger glaciers might have found equilibrium with the 21st century’s climate. Instead, human-caused climate change is melting them away.

While the decrease of glaciers since the end of the Little Ice Age is due to both natural and human-caused climate change, the retreat seen in recent decades can be increasingly attributed to anthropogenic causes. In this way, we have an opportunity to witness and study the power of climate change, both natural and not.

When you view Jackson Glacier from Going-to-the-Sun Road you stand in a valley carved by a Pleistocene glacier and see distant bedrock exposed as ice formed in the Little Ice Age retreats.

Glacier National Park has always been a place of change, and given time, it can adapt. However, the rate of change seen today is fast enough to raise concerns about adaptation, for both ecosystems and societies alike.

A graph of two orange bars, one fading out and the other fading in with black text imposed over the top. Dates are displayed in black text across the x axis on the bottom starting with 1860 and ending at 2000 on the right.
What is causing the glaciers to melt?

This simplified graphic was adapted from a paper published in Science by Marzeion and others in 2014.

The orange bar on the left shows how the park's glaciers naturally melted after the end of the Little Ice Age. The orange bar on the right shows how human-caused climate change has been increasingly the cause of glacier melt.

Glacier National Park’s ice began to retreat after the peak of the Little Ice Age, in the mid-1800s. However, by the 1990s the majority of glacier retreat could be attributed to human-caused climate change. Glaciers melt when more snow melts in the summer than falls in the winter.
a geologist’s hammer resting on a stromatolite fossil

This picture, taken by Richard Rezak (USGS) in 1951, shows a geologist’s hammer resting on a stromatolite fossil.

Humans get a bad rap for altering the atmosphere by burning fossil fuels. There are actually many living things that change the chemistry of the air. Plants photosynthesize, taking in carbon dioxide (CO2) and releasing oxygen (O2).

Animals do the reverse: breathing in oxygen and releasing CO2. One organism you might not have heard of is responsible for the oxygen we breathe today: colonies of cyanobacteria (or blue-green algae) called stromatolites.

Ancient fossils of stromatolites are found throughout the park, including at Logan Pass. Through photosynthesis, they produced the oxygen in our atmosphere today—one tiny bubble at a time.

Burning fossil fuels, which releases many tons of CO2, has changed the composition of our atmosphere in under 200 years, while it took stromatolites over a billion.

The information in this article is featured in exhibits outside the Logan Pass Visitor Center. Check the exhibits out for yourself next time you visit!

Part of a series of articles titled Climate & History at Glacier National Park.

Glacier National Park

Last updated: April 5, 2024