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Tuesday, November 4, 2025

Mammoth Hot Springs

Mammoth Hot Springs 

Mammoth Hot Springs, located near Yellowstone National Park’s northern entrance, stands as one of the park’s most fascinating geothermal marvels—a living sculpture shaped by heat, water, limestone, and time. Unlike the colorful pools and explosive geysers found elsewhere in the park, Mammoth is a landscape of white travertine terraces that seem to flow down the mountainside like frozen waterfalls. 


These formations are created as hot water, rich in dissolved calcium carbonate, rises from deep underground and cools at the surface, depositing minerals layer by layer. Over thousands of years, this process has sculpted an otherworldly terrain that constantly evolves, shifting in shape and color with changes in water flow and temperature.

Mammoth Hot Springs
Mammoth Hot Springs

Mammoth Hot Springs
Mammoth Hot Springs


Quick Reference: Mammoth Hot Springs

Feature / Aspect

Details


Location

Northern Yellowstone National Park, near Gardiner, Montana (North Entrance)


Type

Travertine Hot Springs (formed from dissolved limestone deposits)


Main Areas

Lower Terraces and Upper Terraces


Famous Features

Minerva Terrace, Canary Spring, Palette Spring, Jupiter Terrace, White Elephant Back Terrace, Orange Spring Mound


Water Temperature

Typically ranges from 160°F to 180°F (70°C–82°C)


pH Level

Approximately 6.0 to 7.0 (slightly acidic to neutral)


Water Source

Heated groundwater from Yellowstone’s hydrothermal system dissolving limestone (calcium carbonate)


Accessibility

Boardwalks for Lower Terraces, one-way scenic drive for Upper Terraces


Best Time to Visit

Year-round; most active and colorful during spring and fall


Nearest Facilities

Mammoth Hot Springs Hotel, General Store, Visitor Center, restrooms, and picnic areas


Unique Characteristic

Constantly changing terraces—some dry up while new ones form, creating a dynamic landscape


Wildlife Commonly Seen

Elk, bison, pronghorn, and small mammals often seen around the terraces


Entry Point

North Entrance (Gardiner, Montana)


Nearby Attractions

Fort Yellowstone Historic District, Boiling River (temporarily closed), Roosevelt Arch


Safety Note

Stay on boardwalks—hot water and unstable ground can be dangerous


Fun Fact

The travertine terraces at Mammoth grow faster than any other geothermal formations in the park due to abundant limestone in the region



The main terrace complex is divided into two sections—Upper and Lower Terraces—each offering distinct sights and experiences. The Lower Terraces are easily accessible by boardwalks and include famous formations like Minerva Terrace, Palette Spring, and Canary Spring. Minerva Terrace, often regarded as the most photogenic of them all, displays beautiful shades of orange, gold, and white, especially when its hot water flow is active. Palette Spring, on the other hand, showcases a rainbow of mineral hues as hot water cascades over rippling stone shelves. Canary Spring glows in rich yellow tones, named for the thermophilic microorganisms that thrive in its scalding environment. Each terrace tells its own story of change—sometimes vibrant and active, sometimes dry and ghostly white as the water shifts elsewhere.


The Upper Terraces, accessible by a scenic drive, provide a more elevated view of Mammoth’s geothermal network. Here, formations like New Blue Spring, White Elephant Back Terrace, and Orange Spring Mound dominate the landscape, with steamy vents and bubbling pools dotting the hillside. These features offer a glimpse into Yellowstone’s dynamic underground system—proof that the earth beneath Mammoth is constantly in motion. 


One of the unique aspects of Mammoth Hot Springs is that it sits atop a massive limestone deposit, unlike the rhyolitic rock found in much of the park. This geological difference allows the hot water to dissolve and deposit calcium carbonate more easily, creating Mammoth’s signature travertine formations.


Beyond its geological beauty, Mammoth Hot Springs is also rich in human history. The nearby Mammoth Hot Springs Historic District was once the site of Fort Yellowstone, established in the late 19th century to protect the park before the National Park Service was created. Many of the old fort buildings still stand today and serve as administrative offices and visitor facilities. The Mammoth area remains a hub for visitors, offering lodging at the Mammoth Hot Springs Hotel, a general store, and several hiking trails that wind through the terraces and surrounding hills.


What makes Mammoth so special is its unpredictability. Water channels shift, terraces grow and die, and new springs appear where old ones go dormant. This constant transformation is a reminder that Yellowstone is alive beneath the surface, reshaping itself daily in subtle and spectacular ways. Standing at the edge of Canary Spring or watching steam rise from the ancient terraces, visitors can witness the living pulse of the Earth in motion—an ever-changing masterpiece millions of years in the making.

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