The Wave, North Coyote Buttes, Vermilion Cliffs / Paria Canyon Wilderness, Arizona
The Wave is such a wonderful place, I still get excited looking at the images I photographed there a few weeks ago. I was fortunate to have near-perfect conditions to make my hike and take photos. I spent the entire day out among the North Coyote Buttes and would have stayed longer if overnight camping was permitted there.
OK, this is last time I post a photo of the Wave! Well, at least until next month, when I return for a second time to try some different techniques. I was lucky to get permits two months in a row in the lottery, for the two most sought-after months (April and May), so in late May I will go back, knowing what mistakes I made the first time around and hoping to correct them while they are still fresh in my mind.
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| The Wave, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes set amidst the dramatic surrounding North Coyote Buttes of Arizona and Utah. The sandstone formations of the North Coyote Buttes, including the Wave, date from the Jurassic period. Managed by the Bureau of Land Management, the Wave is located in the Paria Canyon-Vermilion Cliffs Wilderness and is accessible on foot by permit only. North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA. Image: 20608 Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA View this Image in Google Earth! |
The website has lots more photos of the Wave, North Coyote Buttes
Photo of the Second Wave
The Second Wave is found a few hundred yards from the Wave itself. While the Second Wave is characterized by striated sandstone in the same way that the Wave is, beyond that it is quite different in appearance, having a half-hourglass shape and being somewhat lighter in color. For photography the best light on the Second Wave occurs just before the sun sets behind the hills to the west, setting the ridges and striations in strong relief:
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| The Second Wave at sunset. The Second Wave, a curiously-shaped sandstone swirl, takes on rich warm tones and dramatic shadowed textures at sunset. Set in the North Coyote Buttes of Arizona and Utah, the Second Wave is characterized by striations revealing layers of sedimentary deposits, a visible historical record depicting eons of submarine geology. North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA. Image: 20606 Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA View this Image in Google Earth! |
Photo of Brain Rocks
Brain Rocks are found in the vicinity around the Wave. Here are some sporting a view across the Navaho sandstone of the North Coyote Buttes:
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| Brain rocks, curious sandstone formations in the North Coyote Buttes. North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA. Image: 20611 Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA View this Image in Google Earth! |
Photo of the “Heart of the Wave”, North Coyote Buttes
Sitting on the rim of the main bowl of the Wave — right where the photograph below was taken — I watched a couple of hikers arriving. There reaction was natural: no sooner did they step foot through the entry passage than they looked around at the strange surroundings in awe. As one of them walked toward me, she turned around and suddenly said “Oh, its the Heart of the Wave!” She must have recognized the view (below) that is oft-repeated in photographs, and her name for this view must have been coined by someone before her. It seemed quite fitting to me. So thus it is, the Heart of the Wave:
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| The Wave, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes set amidst the dramatic surrounding North Coyote Buttes of Arizona and Utah. The sandstone formations of the North Coyote Buttes, including the Wave, date from the Jurassic period. Managed by the Bureau of Land Management, the Wave is located in the Paria Canyon-Vermilion Cliffs Wilderness and is accessible on foot by permit only. North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA. Image: 20625 Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA View this Image in Google Earth! |
What process produced this geologic oddity? Diagenic coloration arising from stratigraphic relationships among the sandstone layers. Navaho sandstone, almost 200 million years old, was formed from what were formerly sand dunes, compressed and hardened into their current stony form. The colorations stems from iron oxides (think rust!) such as goethite and hematite, with colors ranging from oranges and yellows to salmon, reds and purples.
The Wave in the North Coyote Buttes: The Perfect Skatepark?
Before X-Games and Tony Hawk, nay even before Bahne skateboards, Chicago trucks and Cadillac wheels, there was the Wave. Formed in the days before mankind walked erect, indeed before there was a mankind, God created the ultimate skatepark, one that has yet to be improved upon. The Wave has waited through the eons as man developed lungs, legs, self-awareness, bipedal balance and, finally, sufficient disregard for his own survival to Ride the Board. Hidden in the parched desert of northwestern Arizona, the Perfect Skatepark has been gently, slowly, delicately carved by the winds and sands of time, eroded into unsurpassed contours of verticality that beckon those Most Evolved Humans, the ones who heed the call to bend gravity through a 720° mobius. On Any Given Sunday only a fortunate 20 are chosen to visit by The Man. I have finally lain eyes upon the Perfect Skatepark and my Skate Perspective will never be the same. Ride on bro.
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| The Wave, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes set amidst the dramatic surrounding North Coyote Buttes of Arizona and Utah. The sandstone formations of the North Coyote Buttes, including the Wave, date from the Jurassic period. Managed by the Bureau of Land Management, the Wave is located in the Paria Canyon-Vermilion Cliffs Wilderness and is accessible on foot by permit only. North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA. Image: 20614 Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA View this Image in Google Earth! |
Photo of Diagenetic Coloration in Sandstone, North Coyote Buttes
Not far from the Second Wave is a broad swatch of sandstone displaying exellent examples of diagenetic coloration, various iron oxides producing different colors in the Navaho sandstone strata, dating from the Jurassic era:
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| Striations in sandstone tell of eons of sedimentary deposits, a visible geologic record of the time when this region was under the sea. North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA. Image: 20612 Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA View this Image in Google Earth! |
Hiking the Wave in Arizona’s North Coyote Buttes
Walking around the area surrounding the Wave in Arizona’s Paria Canyon / Vermilion Cliffs Wilderness, one is certain to find this interesting alcove. During the time of day that it lies in shade, it receives only deep red light reflected from neighboring walls. That, combined with its own coloration, results in some parts of the wall taking on nearly purple shades.
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| The Wave, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes set amidst the dramatic surrounding North Coyote Buttes of Arizona and Utah. The sandstone formations of the North Coyote Buttes, including the Wave, date from the Jurassic period. Managed by the Bureau of Land Management, the Wave is located in the Paria Canyon-Vermilion Cliffs Wilderness and is accessible on foot by permit only. North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA. Image: 20609 Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona, USA View this Image in Google Earth! |
Route 66
One our recent desert road trip, we found ourselves on Route 66 for a while. We passed some seriously forlorn-looking old eateries, defunct and barely surviving service stations, and some funky little communities that look like they are ever-so-slowly fading away. It was strange to think that before the interstate system was developed, Route 66 was one of the major travel arteries of our country. Now it is little more than a footnote and curiosity for old-timers and history buffs.
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| Route 66 (also known as U.S. Route 66, The Main Street of America, The Mother Road and the Will Rogers Highway) was a highway in the U.S. Highway system. One of the original federal routes, US 66 was established in 1926 and originally ran from Chicago through Missouri, Kansas, Oklahoma, Texas, New Mexico, Arizona, and California, before ending at Los Angeles for a total of 2,448 miles. US 66 was officially decommissioned (i.e., removed from the offical U.S. Highway system) in 1985 after it was decided the route was no longer relevant and had been replaced by the Interstate Highway System. California, USA. Image: 20567 Location: California, USA |
Late Night Run to the Ice Machine
As soon as we check into a hotel room, any hotel room, one of my kids always has to make a run to the ice machine. What’s up with that?
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| Girl walks down hotel corridor at night, carrying ice bucket, abstract blur time exposure. Image: 20571 |
Photo of the Devil’s Golf Course, Death Valley National Park
The Devil’s Golf Course is a curious assemblage of crystalline salt shapes spread over a large swath of the Death Valley salt pan. This saltpan, which is the lowest point in Death Valley National Park, and indeed the western hemisphere, holds a small amount of subsurface moisture. This water is extremely salty and briny, a result of the accumulation of minerals that were left behind when the 30-foot-deep Holocene-era lake disappeared (the accumulation continues with each year’s winter rains). Capillary action draws the subsurface moisture upward. As the water evaporates, it leaves behind salt crystals that form myriad fantastic shapes. The growth is quite slow, perhaps as little as one inch every 35 years. Wind friction and seasonal flooding of the area during winter storms erodes or reshapes the salt crystal forms, and the process continues.
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| Devils Golf Course, California. Evaporated salt has formed into gnarled, complex crystalline shapes in on the salt pan of Death Valley National Park, one of the largest salt pans in the world. The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt. Devils Golf Course, Death Valley National Park, California, USA. Image: 15582 Location: Devils Golf Course, Death Valley National Park, California, USA View this Image in Google Earth! |
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| Devils Golf Course. Evaporated salt has formed into gnarled, complex crystalline shapes on the salt pan of Death Valley National Park, one of the largest salt pans in the world. The shapes are constantly evolving as occasional floods submerge the salt concretions before receding and depositing more salt. Devils Golf Course, Death Valley National Park, California, USA. Image: 20552 Location: Devils Golf Course, Death Valley National Park, California, USA View this Image in Google Earth! |
Photo of Badwater, Death Valley National Park
Badwater is the lowest point in Death Valley National Park, at 282 feet below sea level. Indeed, it is the lowest point in the entire western hemisphere. The Badwater Basin is the catch point for 9000 square miles of drainage, however, there is typically little water here except following winter rains, since the water evaporates quickly. When it does, it leaves behind a saline, crusty, flat white playa made up of almost pure table salt and stretching for miles — a bizarre place. Evaporation is most extreme in Death Valley: a 1.9 inch annual rainfall is exceeded by evaporation potential of 150 inches per year, enough to scorch a 12 foot deep lake to dust in just 12 months. The water that does manage to persist here is the motivation for the place’s name, for it is a salty, warm, nasty swill which you are advised not to drink. A small, specialized species of snail, the Badwater snail, somehow manages to eke out an existence in these waters. Rising above the parking area are some of the oldest rocks in Death Valley, 1.7 billion (with a b) year old Precambrian volcanic and sedimentary rock layers that have metamorphosed into gneiss. Perched 282 feet up the cliff face is a sign marking sea level. If you visit, be sure to walk out onto the playa, not just a hundred yards or so but far enough that the other visitors and their cars become specks. Admire the sheer white horizon stretching in all directions, the Panamint Mountain and Black Mountain ranges that form the walls of the valley, and the blue sky. Hear the silence as your feet crackle and crunch the salt upon which you walk. Feel the parched air wick the sweat off your skin. Feel your throat become dry. Squint. So nice. Now back to the car and air conditioning, to sip your Diet Coke.
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| Badwater, Death Valley. A spring feeds this small pool year round. The water is four times more saline than ocean water. The small Badwater snail (Assiminea infima) is found only in Death Valley, in spring-fed pools such as these, and is threatened by habitat destruction. At 282 feet below sea level, Badwater is the lowest point in North America. Badwater, Death Valley National Park, California, USA. Image: 20554 Location: Badwater, Death Valley National Park, California, USA View this Image in Google Earth! |
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| Badwater, California. Badwater, at 282 feet below sea level, is the lowest point in North America. 9000 square miles of watershed drain into the Badwater basin, to dry and form huge white salt flats. Badwater, Death Valley National Park, California, USA. Image: 15579 |
Badwater, California. Badwater, at 282 feet below sea level, is the lowest point in North America. 9000 square miles of watershed drain into the Badwater basin, to dry and form huge white salt flats. Badwater, Death Valley National Park, California, USA. Image: 15580 |
Photo of Pink Sunrise on Telescope Peak over Badwater
I’ve been on a few deep scuba dives in my life but relative to sea level this is as deep as I have ever been, and I didn’t even need to strap on a scuba tank to get there. Seen here is delicate pre-dawn pink light on a snow covered Telescope Peak, viewed from Badwater. Telescope Peak, at 11,049 feet, is the highest point in Death Valley National Park as well as the Panamint Range. Badwater is the lowest point in Death Valley National Park, at 282 feet below sea level.
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| Sunrise lights Telescope Peak as it rises over the salt flats of Badwater, Death Valley. At 11,049 feet, Telescope Peak is the highest peak in the Panamint Range as well as the highest point in Death Valley National Park. At 282 feet below sea level, Badwater is the lowest point in North America. Badwater, Death Valley National Park, California, USA. Image: 20549 Location: Badwater, Death Valley National Park, California, USA View this Image in Google Earth! |
Photo of the Paris Hotel Fountain
The Paris Hotel in Las Vegas is most noted for its tall, half-scale replica of the Eiffel Tower. However, it also has a replica of the Arc de Triomphe, a neon-light balloon and a cool fountain at street level as well. Here is the fountain with the balloon in the background, and a bright billboard of two Abercrombie-beautiful models kissing.
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| Fountain at night, Paris Hotel. Las Vegas, Nevada, USA. Image: 20563 Location: Las Vegas, Nevada, USA View this Image in Google Earth! |
Photo of Caesar’s Palace and Jasmine Restaurant
Caesar’s Palace, a Las Vegas landmark, seems so surrounded by other buildings that it was hard to get a decent photo of just the hotel itself. I liked the blue lights in the Bellagio reflection pool illuminating the Jasmine Restaurant with Caesar’s rising in the background.
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| Jasmine Restaurant and Caesar’s Palace Hotel are reflected in the Bellagio Hotel fountain pool at night. Las Vegas, Nevada, USA. Image: 20561 Location: Las Vegas, Nevada, USA View this Image in Google Earth! |
Photo of the Venetian Hotel and “Phantom”
Well, we were with the kids while in Las Vegas so we did not go to any of the shows we might otherwise hit (Ka, Phantom, O) if we had been there on our own, instead opting for sunny days by the pool and dinner out each night. It was fun walking around Vegas in the evenings and seeing it through kids’ eye, they enjoyed the lights and the sounds and the high energy. We thought the Venetian Hotel looked cool, with its tall banner for Phantom of the Opera hanging over the Strip:
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| The Venetian Hotel rises above the Strip, Las Vegas Boulevard, at night. Las Vegas, Nevada, USA. Image: 20562 Location: Las Vegas, Nevada, USA View this Image in Google Earth! |
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Updated: May 22, 2013





































