the Temple of the Sun and Moon sandstone formations in Capitol Reef National Park, Utah
a hiker in Grand Wash Canyon in Capitol Reef National Park, Utah
rock formations in Capital Reef National Park, Utah
petroglyphs in Capitol Reef National Park, Utah
a hiker under a rock arch at Coyote Gulch in Capitol Reef National Park, Utah
hikers in Cohab Canyon in Capitol Reef National Park, Utah
arch formations in Capital Reef National Park, Utah
sunset over Cathedral Valley in Capitol Reef National Park, Utah
1 of 8
Cathedral ValleySunrise lights up the Temples of the Sun and Moon sandstone formations in Cathedral Valley.
Photograph by Larry Geddis, Alamy

These Striking Rock Formations Are up to 270 Million Years Old

Capitol Reef National Park is a place of dramatic beauty and serenity so remote that the nearest traffic light is 78 miles away.

November 05, 2009
4 min read

Location: Utah
Established:
December 18, 1971
Size:
241,904 acres

The unifying geographic feature of Capitol Reef is the Waterpocket Fold. For a hundred miles its parallel ridges rise from the desert like the swell of giant waves rolling toward shore. Exposed edges of the uplift have eroded into a slickrock wilderness of massive domes, cliffs, and a maze of twisting canyons.

Geologists know the fold as one of the largest and best exposed monoclines on the North American continent. Travelers know it as a place of dramatic beauty and serenity so remote that the nearest traffic light is 78 miles away. And even though its 378 square miles are off the beaten track, the park still attracts nearly 750,000 visitors each year.

Capitol Reef is named for a particularly colorful section of the fold where rounded Navajo sandstone forms capitol-like domes and sheer cliffs form a barrier to travel, often referred to as a "reef." Although a highway now crosses the "reef," travel is still challenging for those wishing to see the park's more remote regions.

The southern end of the fold offers fine wilderness backpacking in Lower Muley Twist Canyon and Halls Creek Narrows. Along the park's northern border lies Cathedral Valley, a repository of quiet solitude where jagged monoliths rise hundreds of feet.

The middle region is best known. Here the raw beauty of the towering cliffs contrasts with the green oasis that 19th-century Mormon pioneers created along the Fremont River, establishing the village of Fruita. Their irrigation ditches still water fruit trees in fields abandoned by Fremont Indians 700 years ago. Mule deer now graze on orchard grasses and alfalfa, and park visitors harvest the apples, peaches, and apricots.

The most striking reminder of the Fremont culture is the fine rock art it produced. Figures resembling bighorn sheep crowd many petroglyph panels. The last sighting in the park of a native desert bighorn, a subspecies, occurred in 1948. Their disappearance is attributed to overhunting and various diseases caught from domestic sheep. The Park Service reintroduced desert bighorn sheep in 1984, 1996, and 1997. These herds have survived.

How to Get There

From Green River (about 85 miles away), take I-70 to Utah 24, which leads to the east entrance. For a scenic approach, start at Bryce Canyon National Park. Follow Utah 12 over Boulder Mountain to Utah 24, just outside the park's west entrance. Airport: Salt Lake City.

When to Go

Year-round. Spring and fall are mild and ideal for hiking. Winter is cold but brief. Back roads can become impassable during spring thaw, summer rains, and winter snows at higher elevations.

How to Visit

On a one-day visit, take Utah 24 along the Fremont River and then the Scenic Drive through the heart of the park. This section offers fine hiking on nearly 40 miles of developed trails. The best second-day activity is a drive along portions of the Burr Trail Loop with a walk to Strike Valley Overlook. For a longer stay, drive the Cathedral Valley Loop or hike in one of the more remote canyons of the Waterpocket Fold. Always check road, trail, and weather conditions.

FREE BONUS ISSUE

Go Further