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Second Wave — Fotopedia
Coyote Buttes North, Paria Canyon - Vermillion Cliffs Wilderness, Arizona

... my first visit to Coyote Buttes North was stunning. But already on the walk to the Wave a thunderstorm came closer. After one and a half hour we reached the Wave but with us the dark clouds too - but we decided to stay. The contrast between the dark, energy loaded clouds and the amazing colors of the low sun in front of the Second Wave were unbelievable. Suddenly a few sunbeams found their way through the clouds and covered the Second wave in fantastic light. I hope you enjoy.

28. Sep. 2005 / 5:10pm
Nikon D70 / Nikon AF-S DX 17-55mm/f2.8 G IF-ED
55mm/ 1/250sec / f16 / ISO 200 / -0.7 stop
B&W MRC Käsemann Polarizer / Tripod

Note: My images are posted here for your enjoyment only. Some rights reserved. Please contact me through flickr or at my homepage if you are interested in using this image for any reason.

Thank You.
Wikipedia Article
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The Wave, Arizona

The Wave is a sandstone rock formation located in the United States of America near the Arizona and Utah border on the slopes of the Coyote Buttes, in the Paria Canyon-Vermilion Cliffs Wilderness, on the Colorado Plateau. It is famous among hikers and photographers for its colorful, undulating forms, and the rugged, trackless hike required to reach it.


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Coconino County, Arizona

Coconino County is a county located in the north central part of the U.S. state of Arizona. It is part of the Flagstaff, Arizona Metropolitan Statistical Area. The population was 134,421 at the 2010 census. The county seat is Flagstaff. It is the second largest county by land area in the 48 contiguous United States, behind San Bernardino County, California, with its 18,661 square miles (48,300 km2) making it larger than each of the nine smallest states.

Coconino County contains Grand Canyon National Park, the Havasupai Nation, and parts of the Navajo Nation, Hualapai Nation, and Hopi Nation. It takes its name from Cosnino, a name applied to the Havasupai.

Coconino County was the setting for George Herriman's early-20th-century Krazy Kat comic strip.

Coconino County has a relatively large Native American population at nearly 30% of the county's total population, being mostly Navajo with smaller numbers of Havasupai, Hopi, and others.


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Coyote Buttes

Coyote Buttes is a section of the Paria Canyon-Vermilion Cliffs Wilderness managed by the Bureau of Land Management (BLM), spanning extreme South Central Utah and North Central Arizona, just south of US 89 halfway between Kanab, Utah and Page, Arizona. It is divided into two areas: Coyote Buttes North and Coyote Buttes South. Visiting either of the Coyote Buttes areas requires purchasing a hiking permit.

The Coyote Buttes area is an exposure of cross-bedded aeolian Jurassic Navajo Sandstone. The variable coloration of the sandstones is a result of various iron oxide pigments within the layers. A dinosaur trackway or trample surface is found in the area and provides evidence of a variety of dinosaurs. The area includes dramatic swirling erosional rock formations such as The Wave.

The Wave and Buckskin Gulch share the Wire Pass Trailhead on House Rock Valley Road.


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Paria Canyon-Vermilion Cliffs Wilderness

The Paria Canyon-Vermilion Cliffs Wilderness is a 112,500 acres (455 km2) wilderness area located in northern Arizona and southern Utah, USA, within the arid Colorado Plateau region. The wilderness is composed of broad plateaus, tall escarpments, and deep canyons.

The Paria River flows through the wilderness before joining the Colorado River at Lee's Ferry, Arizona.

The U.S. Congress designated the wilderness area in 1984 and it was largely incorporated into the new Vermilion Cliffs National Monument proclaimed in 2000 by executive order of President Bill Clinton.

Both the wilderness area and the National Monument are administered by the federal Bureau of Land Management.

The Colorado Plateau and its river basins are of immense value in the Earth sciences, specifically chronostratigraphy, as the region contains multiple terrain features exposing miles-thick contiguous rock columns geologists and paleobiologists use as reference strata of the geologic record.