Zion Park in Utah feels like spring
ZION NATIONAL PARK, Utah — Late each winter, when the snow gets sloppy and the streams get muddy, the same thought begins creeping ever more insistently into my mind: I need green. I need warm. I need spring.
That feeling often demands beaches. But when it hit last winter, a different vision commanded: desert, slickrock cliffs and sheer monoliths. That meant southern Utah. And in southern Utah, there is no place better for a spring getaway than Zion National Park.
Nick Driggs/Utah Office of Tourism
From April through October, the heart of the Zion Canyon is closed to private vehicles. Visitors board free propane-powered shuttle buses near the entrance station to complete their journey into the park.
Zion is in Utah's southwest corner, the part of the state that Utahans call Dixie, where the early leaders of the Mormon church kept their winter homes. It is here that spring arrives first.
The grass was still brown when we left our home in Montana in early April, headed south on Interstate 15. But as we descended the last stretch toward Zion, dropping from mountains into valleys, canyon walls soaring beside us until we reached the Virgin River, we could feel spring engulfing us.
Cottonwoods lined the river bank, flaunting fresh green leaves that swayed over acres of brilliant green grass. Wildflowers were in riotous bloom under the warm desert sun. Kids on spring break splashed in the still-frigid river. Desert this may be, but after a long winter it was a welcoming oasis.
Established in 1919, Zion was Utah's first national park. The state hosts some of the nation's most spectacular parks — Arches, Canyonlands, Capitol Reef, Bryce Canyon — but Zion bows to none of them in its magnificence.
The park is part of the Grand Staircase, a huge geological formation on the Colorado Plateau. Layers of sedimentary rock have been lifted, tilted and eroded. Its colorful cliffs stretch from Bryce Canyon to the Grand Canyon.
The scale of the staircase is enormous: The sedimentary rock layers were 10,000 feet thick before erosion began carving. The bottom layer of rock at Bryce Canyon is the top layer at Zion, and the bottom layer at Zion is the top layer at the Grand Canyon. (The Grand Staircase-Escalante National Monument, a separate park in Utah, is part of the formation.)
If you go
GETTING THERE: Zion National Park is in the southwest corner of Utah, about 2 1/2 hours by car from Las Vegas or 4 1/2 hours from Salt Lake City. From Las Vegas, take Interstate 15 north. North of St. George, Utah, take Exit 16 and travel east on State Route 9 for 31 miles to Springdale, the park's main entrance. The entrance fee is $25 per vehicle for seven days.
ACCOMMODATIONS: The Zion Lodge, midway in Zion Canyon, is the only hotel in the park and offers cabins, motel rooms and suites beginning at about $150 per night; reservations at zionlodge.com or 888-297-2757. The Watchman and South campgrounds are just inside the park entrance; Watchman campsites can be reserved by calling 877-444-6777 or on the Web at recreation.gov; South campsites are first-come, first-served. Motel and bed-and-breakfast accommodations, as well as full-hookup campsites for RVs, are available in Springdale and other nearby towns.
FOR MORE INFORMATION: Visit nps.gov/zion/ or 435-772-3256 or zionpark.com/.
As the thousands of feet of sedimentary rock were lifted over the millennia, swift streams cut downward, forming the region's famous canyons. The main canyon in Zion, center of park activity and the focus of our visit, was cut by the North Fork of the Virgin River. It is narrow, less than a quarter-mile wide. But it is deep, flanked by towering sandstone palisades 2,000 to 3,000 feet high that draw rock climbers who savor big walls.
The six-mile canyon drive ends at a formation known as Temple of Sinawava, where the canyon begins narrowing to a slot only 30 to 40 feet wide. The canyon used to be overwhelmed by traffic in spring and summer, bringing noise, pollution and frustration for visitors who could find nowhere to park. The National Park Service now has a mandatory shuttle bus system.
In summer, April through October, the heart of the Zion Canyon is closed to private vehicles. Visitors board free propane-powered shuttle buses near the entrance station to journey into the park.
The buses run every six minutes in the day, stopping at all popular trailheads in the canyon, so people spend far less time waiting for buses than they did in the search for a parking space. The buses also are quiet. A shuttle bus route runs through the town of Springdale, at the park's main gate.
Two campgrounds are just inside the park entrance, and a grocery store is on the city side of the foot bridge.
Our stay was limited to a few days, so we could not hit all Zion's trails. But we could not resist the classic Angels Landing.
Angels Landing is only a five-mile hike, but guides recommend allowing at least five hours because of the terrain the trail covers: a 1,500-foot climb through a slot canyon and out to a 5,785-foot peak perched at the end of a narrow rock fin.
This is not a hike for those afraid of heights. It also is not a hike recommended for young children.
A different adventure awaits at the Temple of Sinawava. At road's end, a paved, mile-long trail leads up the river. There begins a classic slot canyon, the Zion Narrows, where visitors can embark on a four- to 10-mile hike. This is a wet hike and not one to be taken lightly. The river is frigid until mid-summer, requiring dry suits to avoid hypothermia. Good wading boots are essential.
All the specialized gear is available for rent from outfitters in Springdale, who also brief first-time hikers on the peculiar hazards of hiking slot canyons. The reward is a unique hike through canyons of unforgettable beauty.
And for early season refugees from winter like us, it also is a unique welcome to spring.


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