Finn's Take· TL;DRThousands of hikers trek to the summit of Mount Timpanogos every year, passing over a stretch of loose rock and gravel near Emerald Lake without giving it a second thought. They had no idea they were walking on top of a glacier. Geophysicist Michael Thorne says Timpanogos hikers likely wouldn't have known they stood on top of a glacier, because it's covered in rocks, gravel, and debris. Now, thanks to a pair of new studies from the University of Utah, we know exactly what's hiding beneath that rubble — and the scale of it is staggering.
Beneath the rocky slopes of Mount Timpanogos lies far more ice than anyone walking across the surface might suspect. Researchers used gravity measurements to map the buried glacier in 3D and found it is about 83% ice, with enough frozen water to fill 600 Olympic swimming pools. That's also about the same volume as Egypt's largest pyramid. It's one of the most significant hidden water discoveries in the American West in recent memory.
Unlike most glaciers, visibly sprawled across mountaintops or slowly coursing through valleys, Timpanogos is a bit shy. It's a rock glacier — a glacier hidden beneath layers and layers of loose rock that can be tens to hundreds of feet thick. That natural camouflage made it nearly impossible to study with traditional methods, so researchers had to get creative.
By detecting extremely small differences in the gravitational pull of rock and ice, the researchers developed a new way to create a 3D image of the hidden ice within a large rock glacier. Former graduate student Bronson Cvijanovich led field campaigns up Mount Timpanogos while hauling sensitive instruments, including a state-of-the-art gravimeter, to Emerald Lake in 2024, where he took gravity readings from 232 different spots across the glacier. After months of computing that data, the team had a precise picture of what lies below — a body of ice up to 150 feet thick located right above Emerald Lake.
Utah is one of the driest states in the country, and every drop counts. Rock glaciers, it turns out, are uniquely well-suited to help. Because the glacier is covered in rock, its ice melts more slowly than an exposed glacier would. That melt occurs in the summer after most of the snowpack in the Wasatch or the Uinta has already melted away. Rock glaciers provide a sustained late-summer flow into streams and into the groundwater — an important contribution to the watershed. Since the ice is covered, its meltwater is also much cooler and can bring important ecological benefits to cold-water species.
Timpanogos Rock Glacier is one of 836 rock glaciers documented in Utah using satellite imagery. Researchers used their findings on the glacier to identify a relationship between a rock glacier's surface area and the volume of ice beneath, and using that new relationship, experts estimate Utah's rock glaciers may hold 1 gigaton, or 815,000 acre-feet of water. Globally, the findings suggest rock glaciers are important hidden water stores, with researchers estimating that known rock glaciers worldwide may hold about 48 gigatons of water.
A second study found Utah's rock glaciers are not left over from the Ice Age, but are instead water stores that formed thousands of years after Ice Age glaciers melted away. Their findings suggest rock glaciers form as falling debris buries persistent snow and preserves it for thousands of years. That's a remarkable natural process — and one that researchers now believe may be far more widespread than previously understood.
The glacier's slow-melting ice benefits Utah's dry climate but also poses potential flood hazards. Rock glaciers serve as climate-resilient reservoirs of water as well as vital habitats for alpine wildlife — but as global temperatures rise, the balance between those benefits and risks will need careful monitoring. Thorne suspects that there's ice under many of the state's rocky mountain slopes , meaning the Timpanogos discovery may be just the beginning of a much larger reckoning with how much frozen water is silently waiting beneath Utah's peaks.