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Traveling Huntleys

Inspiring travel stories, tips, and guides from a couple exploring the world one destination at a time.

Snow at Bryce Canyon National Park

January 29, 2021 by Michael Huntley

Last Updated: July 31, 2026

Seeing a national park under fresh snow has always been one of those experiences we have chased from a distance — stunning in photographs, rarely practical when you are traveling in a 40,000-pound motorhome. Snow and big rigs don’t mix well without chains or a dumped tag axle, and we have learned over the years that the best approach is simply to stay put and let the Jeep do the work. After the snowfall that hit us in Kanab in January 2021, we did exactly that — loaded Jake into the Jeep and drove an hour north to Bryce Canyon National Park to see whether the hoodoos looked as extraordinary under snow as we had always imagined. They did.

Fresh snow blanketing the hoodoo formations and rim of Bryce Canyon National Park, Utah, in January

Bryce Canyon National Park is located at Highway 63, Bryce Canyon City, Utah 84764, in Garfield County in southern Utah. Hours: The park is open year-round, 24 hours a day. The visitor center is generally open daily 8:00 a.m. – 4:30 p.m. in winter, with extended hours in summer. Admission: $35 per vehicle for a 7-day pass; free with the America the Beautiful annual pass. Phone: (435) 834-5322. Website: nps.gov/brca. The park road is plowed throughout winter and remains open; some overlooks and trails may be temporarily closed after heavy snowfall.

Snow and Blue Skies

Snow-dusted red rock cliffs and hoodoos under a breaking sky at Bryce Canyon National Park, Utah

Fresh snow usually means gray skies, and we had steeled ourselves for flat, shadowless light. Instead, as the storm moved east, the clouds broke apart and sunlight began catching the formations at low angles — the kind of light that makes the reds and oranges almost luminescent against the white. The timing was lucky. We were at Bryce in the late afternoon, when the sun was already low, and the combination of fresh snow, partial clouds, and slanted winter light produced some of the most vivid images we have ever gotten at any national park.

A herd of Pronghorn Antelope crossing the road in fresh snow on the drive to Bryce Canyon National Park, Utah

The drive north from Kanab on US 89 to Highway 12 took just over an hour each way, and it was far from uneventful — a herd of Pronghorn Antelope came across the road and brought traffic to a standstill. Pronghorn are the fastest land animal in the Western Hemisphere, capable of sustaining speeds over 55 miles per hour, but on this particular morning they were in no hurry at all. Jake watched them intently from the back seat.

Red and orange rock formations dusted with snow under a clearing sky, Bryce Canyon National Park, Utah
Bryce Canyon National Park hoodoos with a light dusting of fresh snow on their upper faces, Utah
Sandy Huntley posing with a Smokey the Bear statue at the Bryce Canyon National Park ranger station, Utah

After a summer and fall of smoky western skies and poor visibility from wildfires, a world buried in clean white snow felt like a genuine relief. Sandy stopped for a moment with Smokey at the ranger station — appropriate given that fire was the last thing on anyone’s mind that day.

Bryce Canyon National Park

Sandy Huntley and Jake the dog in the snow at Bryce Canyon National Park, Utah, with snow-covered hoodoos behind them

We have been to Bryce Canyon several times — most recently in 2018 on a spring trip through Kodachrome Basin and the canyon country — and it is one of those places that never loses its impact no matter how many times you return. The formations are unlike anything else on earth, and under snow they take on an entirely different character: the orange and red of the hoodoos intensified rather than muted, the white acting as a contrast layer that makes every mineral color pop.

Despite its name, Bryce Canyon is not technically a canyon. The erosion that formed it did not come from a central river cutting downward — it came from frost wedging, rain, and snowmelt working from the rim inward and downward, carving a series of natural amphitheaters into the edge of the Paunsaugunt Plateau. The result is a horseshoe-shaped collection of basins filled with thousands of hoodoos — freestanding pillars of rock left behind as the surrounding material eroded away. It is more closely related in structure to Cedar Breaks National Monument than to the Grand Canyon.

The Bryce Canyon amphitheater partially covered in fresh snow, viewed from the rim, Bryce Canyon National Park, Utah

The park sits on the Colorado Plateau at an elevation ranging from 8,000 to 9,115 feet — high enough that snow is reliable in winter and the air stays cool even in summer. That elevation is part of what makes it so photogenic: the park straddles a climatic zone where moisture, freeze-thaw cycles, and the particular chemistry of the Claron Formation limestone work together to produce a rate of erosion that exposes new formations continuously. The hoodoos here are estimated to erode at a rate of about two to four feet per century.

Bryce Canyon National Park hoodoos and snow-covered ponderosa pines on the Colorado Plateau, Utah, at 8,000 feet elevation
Female Elk standing in the snow among ponderosa pines at Bryce Canyon National Park, Utah — winter wildlife viewing
A mule deer in the snow near the park road at Bryce Canyon National Park, Utah, in January

Wildlife was everywhere. We spotted elk and mule deer browsing in the ponderosa pines along the rim road — some Bryce elk do migrate to lower elevations for winter, but a resident population remains in the park year-round, and January is one of the better months for seeing them. Between the pronghorn on the highway and the elk and deer in the park, it was one of the better wildlife days of our entire southwest trip.

Bryce Canyon hoodoos glowing red, pink, and white against fresh snow after a winter snowfall, Utah

The colors at Bryce are produced by the mineral content of the Claron Formation — a lake sediment deposit laid down 50 to 60 million years ago during the Eocene epoch. The browns, pinks, and reds come from hematite, an iron oxide; the yellows and tans from limonite, a hydrated iron oxide; and the purples and lavenders from pyrolusite, a manganese oxide. Under snow, these colors become even more saturated against the white, and the low winter sun hits the formations at angles that create shadows the summer sun is too high to produce.

Bryce Canyon hoodoos catching the low winter sun after a snowfall — hematite reds and pink Claron limestone, Utah

We had timed it nearly right without meaning to. Arriving in the late afternoon meant the sun was already low and traveling nearly horizontally across the amphitheater, lighting the west-facing walls while leaving the east faces in deep shadow. The contrast between lit and unlit hoodoos — and between the orange rock and the white snow — was extraordinary. It is the kind of light photographers chase and rarely catch.

Wide view of snow-covered Bryce Canyon National Park hoodoos and forested rim under blue skies, Utah

Ebenezer Bryce, the Mormon settler and carpenter for whom both the park and the town of Bryce, Arizona are named, arrived in the area in the 1870s and reportedly described the canyon as “a hell of a place to lose a cow.” He wasn’t wrong — the terrain is labyrinthine — but he also ranched here and built an irrigation canal before eventually moving on to Arizona. President Harding designated the area a National Monument in 1923; it became a National Park in 1928.

Densely packed hoodoo formations in the Bryce Canyon amphitheater seen from the rim overlook, Utah
Snow-covered hoodoos and canyon walls at Bryce Canyon National Park in winter, Utah
Bryce Canyon National Park hoodoo formations dusted with fresh snow and patches of blue sky, Utah
Heavy snow blanketing the hoodoos and forested rim of Bryce Canyon National Park, Utah
Snow-laden ponderosa pines framing the coral-colored hoodoos at Bryce Canyon National Park in January, Utah
Snow-covered ponderosa pines and coral-colored hoodoos at Bryce Canyon National Park, Utah — winter visit

We have been to Bryce Canyon a number of times and it has never disappointed — but this was the best visit we have had. The snow changed everything: the scale felt larger, the colors more saturated, the experience more solitary. There were almost no other visitors. If you have the flexibility to visit Bryce Canyon in winter and can get there by car on a clear day after a storm, do not hesitate.

Practical Tips

Winter access: The main park road is plowed and open year-round, and the major rim overlooks remain accessible even after significant snowfall. Some hiking trails may be temporarily closed after heavy snow or ice — check current conditions at the visitor center or nps.gov/brca before heading out. Photography timing: Winter light at Bryce Canyon is exceptional — the sun stays low all day and travels at a nearly horizontal angle across the amphitheater, creating dramatic shadows that summer visitors never see. Arrive in the afternoon after a storm, when the clouds are breaking, for the best combination of fresh snow and dramatic light. RV and motorhome travel: Large rigs do not belong on snow-covered roads — if a storm hits while you are parked at a campground, stay put and wait it out or send the tow vehicle. Bryce Canyon Pines and Ruby’s Inn near the park entrance offer full hookup RV sites with reasonable winter access. Wildlife: January is an excellent month for wildlife viewing — elk and mule deer browse the rim forest, and pronghorn are commonly seen along US 89 on the drive from Kanab. Bring binoculars and scan the treeline from overlook pullouts. Microspikes: If you plan to hike below the rim in winter, microspikes or traction devices are strongly recommended — the trail surfaces become hard-packed ice and can be treacherous without them. The NPS sometimes rents or loans them at the visitor center. America the Beautiful pass: Covers the $35 per-vehicle entry fee and pays for itself quickly when combined with nearby parks — Zion, Capitol Reef, and Glen Canyon NRA are all within a few hours.

Frequently Asked Questions

Is Bryce Canyon open in winter? Yes, the park is open year-round, 24 hours a day. The main park road is plowed after snowfall and remains open throughout winter. The visitor center operates on reduced winter hours. Some hiking trails and backcountry routes may be temporarily closed after heavy snow, but the major rim overlooks are generally accessible.

Is Bryce Canyon worth visiting in winter and snow? In our experience, a clear day after fresh snowfall at Bryce Canyon may be the single best condition in which to visit the park. The contrast between the orange and red hoodoos and the white snow is extraordinary, the winter sun stays low and creates dramatic side-lighting all day, and the crowds are a fraction of what you find in summer. If you have the flexibility, time a winter visit to coincide with the day after a storm.

What wildlife can you see at Bryce Canyon in winter? Elk and mule deer are commonly seen browsing in the ponderosa pine forest along the rim road in winter — some elk migrate to lower elevations but a year-round population remains in the park. Pronghorn are frequently spotted along US 89 on the drive from Kanab to the park. Ravens are present throughout the year and are often seen at the overlooks. Utah prairie dogs hibernate in winter and are not active.

Can you hike below the rim at Bryce Canyon in winter? Yes, but with caution. The below-rim trails are open in winter but become packed ice after snowfall — microspikes or traction devices are strongly recommended and sometimes required. The Navajo Loop and Queens Garden trails are popular year-round; their walls shelter hikers from wind and the canyon views from below are spectacular in snow. Check current trail conditions at the visitor center before descending.

Is Bryce Canyon geologically a canyon? Technically, no. Despite its name, Bryce Canyon was not carved by a river cutting downward through rock. It is actually a series of natural amphitheaters formed by frost wedging, rainwater erosion, and snowmelt working from the rim of the Paunsaugunt Plateau inward and downward. This process — called headward erosion — produces the horseshoe-shaped basins and thousands of freestanding hoodoos that make Bryce unlike any other landscape on earth. It is structurally similar to nearby Cedar Breaks National Monument, which formed the same way.

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Filed Under: USA, Utah Tagged With: Bryce Canyon National Park, COVID-19, Hoodoos, Road Trip, Utah, Utah Bryce Canyon National Park Elk Viewing Wildlife National Parks Pronghorn Antelope, Winter Travel

About Michael Huntley

Travel photographer and blogger at Traveling Huntleys. Documenting adventures across the American Southwest and beyond since 2016.

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