Temple of Sinawava and the Riverside Walk: The Gateway to The Narrows

Zion Travel Team··5 min read

The shuttle doors fold open at Stop 9 and the canyon does something unusual: it stops moving. The walls on either side rise to 2,000 feet, close enough that you can trace individual seams of Navajo sandstone with your eyes, and the Virgin River hisses past just below the trail edge. You are standing inside the Temple of Sinawava — a natural rock amphitheater at the northern terminus of Zion Canyon — and there is nowhere left to drive. The road ends here. The hike begins here.

The name comes from the Paiute tradition, where Sinawava is the Coyote deity. The Paiute people lived in this canyon for centuries before the park existed, and their name for this place captures something accurate about the atmosphere: it feels set apart, deliberately enclosed, like a space that was meant for something.

Trail Snapshot

Distance: 2.2 miles round trip

Elevation gain: Negligible — essentially flat

Surface: Paved throughout

Accessibility: Wheelchair accessible

Trailhead: Shuttle Stop 9 (Temple of Sinawava) — last stop on the Zion Canyon route

Permit required: None for the Riverside Walk or for entering The Narrows from the bottom

Park entrance fee: $35/vehicle, valid 7 days; America the Beautiful pass accepted

What the Riverside Walk Actually Is

The Riverside Walk is a 1.1-mile paved path (2.2 miles out and back) that follows the left bank of the Virgin River from the shuttle stop northward into the canyon. The walls continue to converge the entire way. By the time you reach the end of the pavement — where the trail dissolves into the river itself — the canyon is roughly 20 feet wide in places and the sun only reaches the floor for a narrow window each day.

This is one of the most visited trails in any national park in the country, and the reason is simple arithmetic: zero elevation gain plus canyon drama that would normally cost you a strenuous all-day hike to see. Most trails that put you inside walls this tall and this close require serious effort. The Riverside Walk asks for a comfortable 45-minute walk on a flat paved surface. Children, elderly visitors, and people using wheelchairs can reach the canyon's most dramatic interior on this trail.

The Hanging Gardens and Ancient Water

About halfway along the walk you will notice water seeping directly from the canyon walls — thin green smears of moss and maidenhair fern appearing on rock faces where no soil exists. These are the hanging gardens, and they mark one of the more interesting geological boundaries in the park.

Zion Canyon is carved primarily through Navajo sandstone, a porous formation that absorbs water readily. Beneath the Navajo layer sits the Kayenta formation, which is far less permeable. Rain and snowmelt that falls on the plateau above — the high country at 7,000 to 8,000 feet — percolates downward through the Navajo sandstone over hundreds to thousands of years. When that water reaches the Kayenta layer, it has nowhere to go vertically, so it migrates horizontally until it finds a wall face: the canyon. The seeps and springs you see emerging here may contain water that fell as precipitation more than 1,000 years ago. It is genuinely ancient water, and it supports a narrow band of life — columbine, monkeyflower, and scarlet penstemon alongside the fern — that exists nowhere else in the immediate landscape.

The same geology feeds Weeping Rock, about 2 miles back toward the canyon entrance. Same process, different wall face. If you want a shorter introduction to the concept before committing to the full walk, the Weeping Rock trail (0.5 miles round trip from Stop 7) gives you the seeps in miniature.

Timing: Beat the Crowd or Wait It Out

The Temple of Sinawava is the last shuttle stop. Every visitor who boards anywhere in the canyon and rides to the end arrives here. That means by 9:00 AM on a summer morning, the trailhead is already busy. By 11:00 AM it is genuinely crowded — the parking areas and shuttle stop are packed, the trail has steady foot traffic both directions, and the return shuttle queue stretches back from the stop.

Two windows consistently produce a different experience. The first is before 8:00 AM: board the shuttle from Springdale early, arrive at Stop 9 when the light is still low and the canyon air is cool, and you will have long stretches of the trail nearly to yourself. The second is after 4:00 PM: crowds thin as day-trippers head back to their cars, the afternoon light shifts into the canyon, and the lower angle catches the red walls differently than midday. The shuttle runs until 8:15 PM during peak season (mid-May through mid-September), so a late-afternoon walk followed by a last-shuttle return is a practical option.

The Narrows: What Happens If You Keep Walking

At the end of the pavement, the trail ends and the river begins. If you step into the Virgin River and continue north, you have entered The Narrows — the slot canyon section that the Riverside Walk was always pointing toward. The walls tighten to as little as 20 feet apart and rise 1,000 feet above the river. The hike becomes a wade, sometimes thigh-deep, over slippery river cobbles.

No permit is required to enter The Narrows from the bottom (this direction). You can walk as far as you are comfortable and turn around whenever you want. The most popular turnaround point is Orderville Canyon, about 1.5 miles upstream from where the pavement ends, reached after roughly 1.5 to 2 hours of river hiking depending on water levels and pace.

Gear matters here. The river bottom is uneven and cold even in summer; water shoes with ankle support or canyoneering-specific footwear are worth renting. Several outfitters in Springdale rent dry pants, neoprene socks, and walking sticks specifically for this hike — our Getting Around section covers the Springdale outfitter options in detail.

Flash Flood Risk: Read This Before You Wade In

Flash floods in the Virgin River can originate from storms miles upstream — storms you cannot see from inside the canyon. The park closes The Narrows when the National Weather Service issues a Flash Flood Warning for the area, and the river is also closed to all hiking when flow exceeds 150 cubic feet per second. Check the real-time flow rate data before you go; the NPS posts current conditions at the Narrows information board at the trailhead and online.

The Riverside Walk itself — the paved section — is not exposed to the same flood risk as the river hiking section. The warning applies specifically to once you leave the pavement and enter the water. During July, August, and September, afternoon monsoon weather builds quickly over the plateau. An entirely clear sky at Stop 9 means nothing about conditions 15 miles north. If there is any storm in the forecast for the region, stay on the pavement.

Getting There: Shuttle Logistics

During shuttle season — March 7 through November 28 in 2026 — private vehicles are not permitted on Zion Canyon Scenic Drive. You must take the free shuttle. Board at the Zion Canyon Visitor Center or at any stop along the canyon route (Stops 1–8); all routes terminate at Stop 9. The shuttle is first-come, first-served with no reservation required. On peak summer days, the visitor center queue can back up; arriving before 7:00 AM or after 3:00 PM shortens the wait significantly.

Outside shuttle season, you can drive your own vehicle to the Temple of Sinawava parking area. The lot is small — roughly 20 spaces — and fills fast on any clear-weather day, even in winter. The lot at the visitor center with a walk to the shuttle boarding area, or the paid parking in Springdale with a free town shuttle connection, are the two reliable alternatives when the lot is full.

The Riverside Walk is open year-round. In winter, sections of the trail can ice over and the park may post traction device requirements. The Narrows river hiking is possible year-round but the water temperature drops near freezing in winter, making full dry suits — not just rental gear — appropriate for anyone planning more than a short wade.

There is no single trail in Zion that delivers this ratio of access to reward. The Riverside Walk is 1.1 miles of flat pavement that ends at one of the most dramatic slot canyon entries in the American Southwest. Go early, check the flow rate, and bring shoes you are willing to get wet.

Frequently Asked Questions

How long does it take to hike the Riverside Walk at Temple of Sinawava?

The Riverside Walk is 2.2 miles round trip on a flat, paved surface, and most visitors complete it in about 45 minutes at a comfortable pace. If you plan to continue into The Narrows past the end of the pavement, add roughly 1.5 to 2 hours of river hiking to reach the popular Orderville Canyon turnaround.

Do you need a permit to hike the Riverside Walk or enter The Narrows from the bottom?

No permit is required for the Riverside Walk or for entering The Narrows from the bottom (the Temple of Sinawava end). You pay the standard park entrance fee of $35 per vehicle, valid for 7 days, and America the Beautiful passes are accepted.

What is the best time of day to visit Temple of Sinawava to avoid crowds?

Arriving before 8:00 AM gives you the coolest canyon air and nearly empty stretches of trail. After 4:00 PM is the other reliable window — day-trippers thin out, the light drops lower into the canyon walls, and the free shuttle runs until 8:15 PM during peak season so a late return is easy.

Is it safe to hike into The Narrows on a clear day, and how do I check conditions?

A clear sky at Stop 9 does not rule out flash flood danger, because storms miles upstream on the plateau can send a flood through the canyon with no warning. The park closes The Narrows when a Flash Flood Warning is issued or when river flow exceeds 150 cubic feet per second. Check the NPS conditions board at the trailhead or current flow data online before stepping off the pavement.

What are the hanging gardens along the Riverside Walk?

About halfway along the trail, water seeps directly from the canyon walls, feeding narrow strips of maidenhair fern, columbine, monkeyflower, and scarlet penstemon growing on bare rock. The seeps form where ancient water — rain that soaked into the plateau above potentially more than 1,000 years ago — reaches an impermeable rock layer and migrates sideways until it finds the canyon wall face.