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Attraction · Yellowstone National Park, Wyoming

Mammoth Hot Springs

Mammoth Hot Springs sits near Yellowstone's North Entrance and is built from limestone rather than the volcanic rock found elsewhere in the park, which is why its terraces form in ever-shifting, travertine-white and mineral-stained layers. Hot water dissolves the limestone underground and deposits it on the surface as it cools, so the terraces are constantly changing shape, sometimes within months. Boardwalks wind through both the Lower and Upper Terraces, and the area is also a common spot to see elk grazing right in the historic Fort Yellowstone grounds nearby.

Photos of Mammoth Hot Springs

Visitor guide

About Mammoth Hot Springs

Mammoth Hot Springs is a complex of steaming white terraces in the north of Yellowstone National Park, built not from the silica that surrounds most of the park's geysers but from travertine, a calcium carbonate rock. It sits at about 6,735 feet (2,053 metres) beside the buildings of Fort Yellowstone.

How the terraces form

The National Park Service explains that most of Yellowstone's thermal formations are siliceous sinter and geyserite, while the Mammoth terraces are travertine. Hot water carrying dissolved carbon dioxide forms a weak acid that dissolves limestone underground. When the water reaches the surface, carbon dioxide escapes and calcium carbonate settles out as chalky white rock. Wikipedia adds that the water travels along a fault from the Norris Geyser Basin area and cools to about 170 degrees Fahrenheit (80 degrees Celsius) before emerging; the NPS notes that scientists have suggested either the main Yellowstone magma chamber or a smaller nearer heat source.

The deposits grow quickly. A 2010 article in the NPS publication Yellowstone Science reported travertine forming at about 5 millimetres per day, with one monitored site gaining 0.3 to 0.6 metres in ten months, and described the terraces as up to 73 metres thick and covering more than 4 square kilometres. Wikipedia describes Terrace Mountain as considered the largest carbonate-depositing spring in the world, a superlative worth treating with caution.

White travertine terraces and a blue pool at Mammoth Hot Springs

Constant change

Individual springs here switch on and off, and their flow can wander from one part of the hillside to another. The NPS notes that Mound Terrace was inactive for decades before it began flowing again. Dry terraces turn grey as they weather while active ones stay bright white, so the hillside looks different from one trip to the next. Colour in the warm runoff comes from algae and bacteria that tint the travertine brown, orange, red and green.

People and the landscape

The NPS reports that for hundreds of years Shoshone and Bannock people collected minerals from the terraces to make white paint. Fort Yellowstone and the Mammoth Hotel stand on Hotel Terrace, an older terrace formation, and sinkholes on the Parade Ground are a reminder that the ground beneath is still thermally active. Wikipedia lists around 70 named springs and terraces, among them Liberty Cap, Cleopatra Terrace and Orange Mound Spring.

Walking the terraces

Boardwalks cover both the Lower and Upper Terraces. The NPS describes the Upper Terrace trailhead as giving close views of Dryad, Canary, Grassy and Cupid springs. The NPS advises that most of these boardwalks are not maintained during winter, so check its pages for current access, trail conditions and any closures. Stay on the boardwalks: the travertine is fragile and the ground can be hot and unstable.

For a private tour, a Voyzo vehicle and driver with door-to-door pickup can make the northern part of the park straightforward to combine with other stops, and your group can walk the terraces at its own pace.

Frequently Asked Questions About Mammoth Hot Springs

The terraces are travertine, a rock made of calcium carbonate. The NPS notes that most other Yellowstone thermal formations are siliceous sinter and geyserite.
Hot water charged with carbon dioxide dissolves limestone underground, then deposits calcium carbonate when carbon dioxide escapes at the surface. The result is chalky white travertine.
A 2010 NPS Yellowstone Science article reported rates of about 5 millimetres per day, with up to 0.3 to 0.6 metres of growth at a monitored site over ten months.
Individual springs switch on and off and their flow shifts across the hillside. Active terraces stay white, while dry ones weather to grey.
Algae and bacteria living in the warm runoff tint the travertine brown, orange, red and green.
Yes, boardwalks cover the Lower and Upper Terraces. The NPS advises that most are not maintained in winter, so check it for current access.
Yes, Voyzo can arrange a private vehicle and driver with door-to-door pickup. Check the NPS for current access and conditions.
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