Duck Creek Guide
Navajo Lake disappears into a sinkhole, runs a mile through the rock, and comes back out of a cliff face — 1.1 easy miles from a trailhead 20 minutes from the inn
At a glance
Cascade Falls is the strangest waterfall on the Markagunt Plateau: the water does not come down a creek, it comes out of the side of a cliff. Navajo Lake, a mile away and 180 feet higher, has no surface outlet — it drains into sinkholes at its east end, runs through a cave dissolved in the Claron limestone, and reappears here as the head of the North Fork of the Virgin River, the same water that goes on to carve Zion Canyon. Forest Trail #32055 gets you to it in 1.1 miles round trip along the rim, with benches, stairs and two railed viewing platforms. It has been a National Recreation Trail since 1979.
This is the part people get wrong, and it is worth two minutes before you leave. The trailhead is 7.6 miles from the inn and the last 2.7 of them are forest road, with two forks that decide whether you end up at a waterfall or at a lake. The five numbered pins on the map are the five steps below.
The interactive map needs JavaScript. In short: Highway 14 west 4.5 miles, left on Navajo Lake Road, left again at the Cascade Falls sign after 0.3 miles, then 2.7 miles of forest road — bearing right at the Y — to the trailhead.
Leave the inn heading west. You climb steadily — the highway tops out around 9,160 ft at the turnoff, some 700 feet above the village.
Paved the whole way.
A signed junction on the south side of the highway near milepost 26, just past the Navajo Lake scenic pullout. Still paved.
The road splits. Right carries on paved to the lake, the campgrounds and the lodge. You want the left fork onto Forest Road 054, and this is where the pavement ends.
Miss this and you end up at Navajo Lake — which is a fine mistake, but it is not the falls.
Graded gravel through the pines. At the Y, right stays on FR-054; left drops toward Duck Creek. The Forest Service signs it, but the sign is small and easy to pass at speed.
Narrower and rougher than the first stretch, and the last few hundred yards run out along the rim. The road ends in the parking loop at 8,926 ft.
Trailhead coordinates: N 37° 29.837′ W 112° 45.096′.
Reasonable in a passenger car, most of the time. The first 1.1 miles of FR-054 are graded gravel that a rental sedan handles at 20 mph without drama. The final 1.6 miles are narrower, more rutted, and washboarded in places, and they run out along the rim near the end — slow, not technical.
The caveats are weather and season. After a summer thunderstorm the clay in the tread turns slick and the ruts fill, which is when high clearance stops being optional. Through winter and early spring the road is snowed in and nobody plows it. If the forest is wet, or if you are driving something low with a full car, give yourself the extra ten minutes and take it slowly.
There is no gas, no water and no cell coverage past the highway. The last services are in Duck Creek Village, five minutes from your room.
Easy is the right word, but it hides something: the trail runs downhill to the falls. You climb 22 feet in the first tenth of a mile, and from there it is level or descending the whole way out, finishing 47 feet below where you parked. All the effort is on the return, and the numerous stairs are what you feel, not the grade.
Large dirt loop at 8,926 ft with a pit toilet and no water. The Virgin River Rim Trail leaves from the same lot.
The only climb on the way out, and it is 22 feet. From here the trail is level or downhill all the way to the falls.
The first of the two viewing platforms, with benches. The canyon opens up south toward Zion.
End of the trail at 8,879 ft: a railed platform under the rim rock, facing the cave mouth the water pours from.
Honest answer: usually, but not always, and nobody measures it. There is no gauge on Cascade Falls. What the flow tracks is how full Navajo Lake is, because the lake is the falls — and the Utah Geological Survey puts the range bluntly, from “a small trickle to a raging torrent.”
In a dry year an engineered earthen dam at the east end of the lake holds the water back from the sinkhole, and the overflow drains through a small opening in the bottom of the sink. In a wet year the lake tops the dike, fills the valley, and the sink runs like a bathtub drain.
What that means for a visit: late May through early July is the window, when snowmelt has the lake at its highest. August and September are a gamble that gets worse in a dry summer. If you want a read before you drive out, the winter's snowpack is the best predictor there is — our snow report tracks the two SNOTEL stations that bracket the village, and a big year up there is a loud year down here.
And if the falls are thin, the walk is still worth the morning. The cave mouth, the Pink Cliffs and the canyon running south toward Zion do not depend on the water.
A lava flow dammed a narrow valley on the Markagunt Plateau and made Navajo Lake. Underneath the lava sits the Claron Formation — the soft, vividly coloured freshwater limestone and marl, roughly 50 million years old, that erodes into the hoodoos at Bryce Canyon and the amphitheatre at Cedar Breaks. Limestone dissolves. Water percolating down through the basalt ate a cave into it, and the lake found the drain.
So Navajo Lake has no surface outlet. It empties through sinkholes at its east end, runs a little over a mile through the rock, and comes back out of the Pink Cliffs escarpment here, about 180 feet lower, as the head of the North Fork of the Virgin River. That is the same river that carves Zion Canyon downstream — and you can see the country it heads for from the second platform.
The part that is genuinely strange is what the U.S. Geological Survey found when it put dye in the sinkholes. The water splits. Some of it surfaced at Cascade Spring after about 8.5 hours, bound for the Virgin River and eventually the Colorado. The rest surfaced at Duck Creek Spring after about 53 hours, bound for the Sevier River and the Great Basin, which has no outlet to the sea at all. One lake, feeding two river systems on opposite sides of the divide — and the second one comes back up beside the village you are staying in.
A note on wording, since the signs disagree: the Forest Service calls the passage a lava tube, and the Utah Geological Survey describes a dissolution cave in the Claron limestone beneath the lava flow. Both descriptions are in print; the geology reads as limestone.
The Forest Service closes the lava tube and cave system to travel because of low oxygen levels and high water flows — a combination that gives no warning and no second chance. The trail ends at a railed platform facing the cave mouth, and that is as close as anyone is meant to get. Nothing on this page describes a route off the tread.
The Forest Service gives roughly Memorial Day to Labor Day as the open season, weather permitting, and the trail is walkable into fall until snow closes the forest road. Flow is the thing that changes: it tracks how full Navajo Lake is, and the Utah Geological Survey describes it ranging from a small trickle to a raging torrent. Late May through early July, on snowmelt, is the reliable window. Later in a dry year the falls thin out, though the cave mouth, the Pink Cliffs and the canyon view are still there.
An hour of driving and 45 minutes of walking is not a day. Here is what pairs with the falls, roughly in the order they make sense on the way back.
Stand at the dike on the east end and you are looking at the sinkhole that swallows the water you just watched come out of a cliff. It is the other half of the same story, and the lake has the boat ramp, the campgrounds and the lodge.
Navajo Lake guideCascade Falls is an intermediate trailhead on the 32-mile rim trail: 9 miles north to Te-Ah Campground, 11 miles south to Strawberry Point. Walk 20 minutes out and back for the rim view without the commitment.
Trails near Duck CreekThe south end of that same rim trail, reached by road instead: a fin of rock sticking out over the pink cliffs with one of the biggest views on the plateau. Forty minutes from the falls trailhead.
Strawberry PointIf the closed lava tube at the falls left you curious about what is under this plateau, the caves east of the village are the ones you can actually walk into.
Caves and lava tubesReviewed September 2026
Trail number, length, season, facilities and the cave closure come from the Forest Service’s own trail page and its Cedar City brochure. The geology and the dye-trace travel times come from the Utah Geological Survey and a USGS study of the Markagunt Plateau. Every distance and elevation on this page was measured — the drive routed over OpenStreetMap road geometry, the trail traced from the mapped tread, and elevations sampled from the USGS 3DEP dataset — then checked against the Forest Service’s published mileages, which they match. Road and snow conditions change; check the forest alerts before an early or late-season drive.
The questions trip planners usually ask next.
The Forest Service signs it at 1.1 miles round trip, about 0.6 miles each way, and most people spend 45 minutes to an hour including time on the platforms. It is rated easy, but there are numerous stairs and the trail loses about 50 feet on the way out, which you climb on the way back.
Head west on Highway 14 for about 4.5 miles and turn left onto Navajo Lake Road (Forest Road 053). After 0.3 miles take the left fork at the Cascade Falls sign onto Forest Road 054; the pavement ends there. Follow FR-054 for 1.1 miles, bear right at the Y to stay on it, and go another 1.6 miles to the trailhead. That is 7.6 miles total, about 20 minutes.
Usually yes. The 2.7 miles of forest road are graded dirt and gravel and are fine for a careful passenger car when dry. They get rutted and slick after storms and are snowed in through winter and early spring, so a high-clearance vehicle helps in bad conditions but is not required in good ones.
Late May through early July, when snowmelt has Navajo Lake high enough to push water through the sinkhole. The Utah Geological Survey describes the falls ranging from a small trickle to a raging torrent depending on lake level. Morning is the better half of the day: the trail has almost no shade and faces the afternoon sun.
Navajo Lake, about a mile away and 180 feet higher. The lake has no surface outlet — it drains through sinkholes at its east end into a cave dissolved in the Claron Formation limestone. USGS dye tracing showed that water reaching Cascade Spring in about 8.5 hours, and some of the same water reaching Duck Creek Spring after about 53 hours, which sends one lake into two different river basins.
No. The Forest Service closes the lava tube and cave system to travel because of low oxygen levels and high water flows. The trail ends at a railed viewing platform facing the cave mouth, and there is a second platform with benches about halfway along.
Yes, on leash. The trail is foot traffic only — closed to motorized vehicles, horses and bicycles — and there is no water along it, so bring some for your dog. Keep them close; parts of the trail run along steep drop-offs.
Start from the broader guide hub if you want the bigger set of destinations, activities, and planning pages first.
Sideways links to the nearby destinations and guide pages guests usually compare.
Every hiking trail and trailhead near Duck Creek Village: Cascade Falls, the Navajo Lake Loop, the Virgin River Rim Trail, and the Cedar Breaks rim
View guide
Fishing, kayaking, and lakeside relaxation
See lake
Alpine amphitheater, sunset overlooks, and an International Dark Sky Park, 20 minutes from the inn
View guideUse these pages to move from a guide idea into a concrete itinerary or comparison.
Choose the stay type that matches the trip you are building.
Rooms with breakfast or cabins with a kitchen at Duck Creek Village Inn — twenty minutes from the trailhead, and five from the springs where the other half of that water comes back up.
