The Wave (Arizona)

The area is administered by the Bureau of Land Management (BLM) at the Grand Staircase–Escalante National Monument visitor center in Kanab, Utah.

[1] The formation is well-known among hikers and photographers for its colourful, undulating forms and the difficult hike required to reach it.

Due to the fragile nature of the formation and the large number of people wishing to visit it, a daily lottery system is used to dispense permits for up to 16 people and/or 4 groups (whichever comes first) two days before (visitors must apply within a geofence area encompassing the greater Kanab visitor center, Vermilion Cliffs, and Page areas).

As a result, the troughs are now almost exclusively eroded by wind, as indicated by the orientation of erosional steps and risers cut into the sandstone along their steep walls.

[4][5] The Wave exposes large-scale sets of cross-bedded eolian sandstone composed of rhythmic and cyclic alternating grainflow and windripple laminae.

The thin ridges and ribbing seen within The Wave are the result of the differential erosion of rhythmic and cyclic alternating grainflow and windripple laminae within the Navajo Sandstone.

Dinosaur tracks and the fossil burrows of desert-dwelling arthropods, such as beetles and other insects, have been found in the Navajo Sandstone within the North Coyote Buttes Wilderness Area.

[15] However, in an effort to maintain the natural integrity of the region, there are no formal trails or signage to guide hikers to The Wave from any of the trailheads.

Anyone attempting the hike in any season is wise to be prepared for harsh desert conditions, including fierce winds, blowing sand, and little shade.

[16] Hikers must choose their own route across the open desert, which requires traversing exposed sandstone, sand dunes, and sandy wash bottoms.

Each checkpoint includes a marked color photo of the terrain ahead, azimuth, latitude, longitude, UTM, northing, and easting.

[19] While not required, the Bureau of Land Management provides a list of authorized guides for those hikers who may be uncomfortable in a wilderness situation.

Thin ridges created by the erosion of differentially cemented, large-scale eolian cross bedding within Navajo sandstone
Main Wave canyon with snow, rare event during winter
Subdued colors at evening twilight