If you have ever hiked in the high peaks of Colorado, the Wasatch Range in Utah or the Tetons in Wyoming, you’ve almost certainly seen a rock glacier, perhaps without even knowing it.

Rock glaciers are slow-moving masses of rock debris and ice that flow downhill the same way that glaciers do, but they are covered by a thick layer of rock and boulders that can easily be mistaken for stable ground.

There are at least 1,500 active rock glaciers across the western U.S., and they’re important. That’s because while the icy white glaciers people typically picture have been shrinking and even disappearing, our new study shows that rock glaciers and their frozen water are remaining mostly stable despite rising temperatures.

The thick debris mantle shades the ice, keeping it colder, similar to how ski areas have started covering their slopes with reflective blankets in summer to stave off melting. The result is that rock glaciers continue to provide meltwater for streams in summer as they always have, but they aren’t disappearing.

We study glaciers around the world. In the new paper, we examine how different types of glaciers are changing beneath the soaring peaks of the Teton Range of Wyoming.

We found that the Tetons’ white, icy glaciers thinned by 2.75 feet per year (0.84 meters per year) between 2014 and 2022, about seven times faster than in the previous half-century. Rock glaciers, on the other hand, were close to stable, losing only about 0.16 feet (0.05 meters) per year in 2014-2022, with no change relative to the 1967-2014 period.

Every year, mountain glaciers partially melt and then rebuild again as snow falls in winter. But as temperature rise, glaciers are losing more ice than they gain. The vast majority of glaciers in temperate mountain ranges like the Tetons are projected to melt away completely by the end of the century, meaning a critical source of water for mountain streams and lakes will disappear. However, where rock glaciers are present, their protected ice will continue to release meltwater into the streams below, buffering the streams against warming temperatures and drying.

Because of this, streams fed by rock glaciers have emerged as potentially critical climate refugia – places likely to stay cooler while everything around them warms – for cold-water wildlife in high-mountain ecosystems.

A wide array of species already live in the cold meltwater that emerges from rock glaciers, from stoneflies to the bull trout that eat them. As glaciers fade, the ties between cold-water animals and rock glaciers will likely only become tighter.

For instance, the meltwater stonefly (Lednia tumana), an aquatic insect listed under the U.S. Endangered Species Act in 2019 due to climate-related habitat loss, relies on the fading glaciers of Glacier National Park. But it can also be found downstream of rock glaciers, which are likely to give the stonefly a chance of survival as other glaciers disappear.

Our study showed that having a major ice source feeding a stream has limited the warming of that stream over the past decade.

We found that streams fed by rock glaciers warmed slowly, by about 1.1 degrees Fahrenheit (0.6 degrees Celsius) over the decade, while icy glaciers warmed by about 1 F (0.9 C). Streams that were fed by seasonal snowpack, small patches of ice and groundwater warmed more rapidly, by 6.1 F (3.4 C) over the same period. In one instance, the small snowfields feeding one of our long-term study sites largely disappeared, causing the stream below it to stop flowing by late summer.

Rock glaciers will not replace the glaciers and snowfields that are disappearing. A recent study estimates that rock glaciers in the region hold the equivalent of 0.6 cubic miles (2.5 cubic kilometers) of water, about one-fifth the amount in mountain glaciers.

And climate projections show that even rock glaciers are not immune to a warming climate. Many could become ice-free by the end of the century under current warming projections.

Understanding how much ice is contained in rock glaciers and how fast they are likely to melt is vital to help natural resource and land managers plan for the landscapes they will be managing later this century.

Rock glaciers also offer unique analogs for studying what appear to be debris-covered glaciers on Mars. Research has sought to better understand these rock glacierlike features on Mars, as well as test technology, such as the use of drone-based radar systems to measure ice and debris thicknesses, here on Earth.

So, the next time you’re out in the mountains, staring off into the distance, look carefully for these large fields of rock that appear to be flowing down the mountainside. And pay attention to that small trickle of meltwater emerging from the toe of the rock glacier.

While meltwater from rock glaciers alone certainly won’t make up for the glaciers lost, it could help mitigate the most severe impacts where rock glaciers persist.

This article is republished from The Conversation, a nonprofit, independent news organization bringing you facts and trustworthy analysis to help you make sense of our complex world. It was written by: Dan McGrath, Colorado State University; Ashlesha Khatiwada, Colorado State University, and Scott Hotaling, Utah State University

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Mountain glaciers may hold less ice than previously thought – here’s what that means for 2 billion downstream water users and sea level rise

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Dan McGrath receives funding from the National Science Foundation, NASA, and US Bureau of Reclamation.

Ashlesha Khatiwada receives funding from the National Science Foundation

Scott Hotaling receives funding from the State of Utah, NSF, USDA, USGS, and similar sources.