
The Wave
Interesting facts
- The Navajo Sandstone of the Wave was laid down as desert dunes about 200 to 195 million years ago, in the Early Jurassic.
- The ancient sand sea that left the Navajo Sandstone may originally have been about two and a half times larger than its surviving outcrop of roughly 102,000 square miles.
- The two main troughs measure about 19 by 36 metres and 2 by 16 metres, so the famous formation is far smaller than photos suggest.
- Only 64 people a day may visit: 48 permits go by online lottery four months ahead and 16 by a geofenced lottery two days before.
- From March to November the odds of winning a permit in either lottery are well below fifty per cent.
- Its fame spread in Europe after the 1996 German documentary Faszination Natur featured the formation.
- In the nearby North Coyote Buttes the same sandstone preserves dinosaur tracks and fossil arthropod burrows, and some layers look trampled and churned by dinosaurs.
- The tiny creatures that hatch in rain pools are tadpole shrimps of the species Lepidurus apus, sometimes appearing by the hundreds.
Why it is worth it
In the Coyote Buttes of northern Arizona, on the border with Utah, the Navajo Sandstone has been eroded into a pair of intersecting troughs whose walls are banded in red, orange, pink and cream. The stripes curve and swirl around the walls like frozen surf, and walking through them feels like stepping into a sculpture. The Wave is one of the most photographed rock formations in the American Southwest, and one of the hardest to reach.
The stripes record ancient history. The Navajo Sandstone formed from sand dunes of the Jurassic period, and its fine alternating layers are traces of how the dunes grew, grain by grain, under the wind. Wind and occasional water then carved U-shaped channels through the rock, cutting across the layers and exposing them in sweeping lines. After rain, pools form in the hollows and can briefly fill with tiny tadpole shrimp. Nearby is the Second Wave, with fainter colouring.
The Wave lies within the Paria Canyon–Vermilion Cliffs Wilderness, managed by the Bureau of Land Management, and to protect the fragile sandstone the number of daily visitors is strictly limited. Most permits are allocated by an online lottery months in advance, with a smaller number through a daily lottery close to the site. There is no marked trail: hikers cross about three miles of open desert, slickrock and sand from the trailhead, making a round trip of around six miles.
Getting there
The usual start is the Wire Pass Trailhead on the unpaved House Rock Valley Road, about 8 miles south of U.S. Route 89 between Kanab, Utah, and Page, Arizona. The nearest airport is Page Municipal Airport (PGA), about 50 km away; the nearest larger city in the directory is Cedar City, Utah, about 120 km away.
Plan your visit
We have no confirmed visit data yet. Once it is confirmed, this block also carries the date it was checked.
Nearby places
- Buckskin Gulch 12.5 km · gorge
On these lists
From the encyclopaedia
The Wave is a sandstone rock formation located in Arizona, US, near its northern border with Utah. The formation is situated on the slopes of the Coyote Buttes in the Paria Canyon-Vermilion Cliffs Wilderness of the Colorado Plateau. The area is administered by the Bureau of Land Management (BLM) at the Grand Staircase–Escalante National Monument visitor center in Kanab, Utah.
Wikipedia · CC BY-SA 4.0
36.99610, -112.00600per Wikidata