Mid Wave
photo by Greg Mote

The Wave - sand dunes between Arizona & Utah

( 2 user reviews )

General

The Wave is a sandstone formation on the slopes of the Coyote Buttes in the Paria Canyon-Vermilion Cliffs Wilderness, located in northern portion of the U.S. state of Arizona, just south of the Utah-Arizona border about halfway between Kanab, Utah and Page, Arizona.

The soft sandstone of The Wave is fragile, so one needs to walk carefully, not break the small ridges. A good time for photographing The Wave is the few hours around midday when there are no shadows in the center, although early morning and late afternoon shadows can also make for dramatic photos. After a recent rain storm, numerous pools form which can contain hundreds of tadpoles and fairy shrimp. These pools can be present for several days.

The Wave is not easy to find. In an effort to maintain the natural integrity of the region, there is no formal trail to The Wave. Most hikers are guided to The Wave either by GPS or a prominent landmark known as "the Black Crack," which is widely visible within the Coyote Buttes region. The Wave lies directly below the Black Crack. Hikers must choose their own route across the open desert, which requires traversing exposed sandstone, sand dunes, and sandy wash bottoms. It is not uncommon for hikers to get lost and never find The Wave.

Contact & location

2 Reviews

hello
hello

on Mar 26,2013

I liked

most of it

I disliked

It doesn't tell you ho it's formed
twinkletoes
twinkletoes

on Mar 09,2013

I liked

Doing a research project on it. Such a beautiful lovely place.

I disliked

Nothing

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The photos displayed on this page are the property of one of the following authors:

Greg Mote, Rick McCharles, Elias, Andy Jou, brew ha ha

Some photos courtesy of: . The photos provided by Flickr are under the copyright of their owners.

This travel guide also includes text from Wikitravel articles, all available at WikitravelView full credits

This travel guide also includes text from Wikipedia articles, all available at WikipediaView full credits

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