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.
The Second Wave at Sunset, North Coyote Buttes. 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.
Light Beam in Upper Antelope Slot Canyon. Thin shafts of light briefly penetrate the convoluted narrows of Upper Antelope Slot Canyon, sending piercing beams through the sandstone maze to the sand floor below.
The Second Wave at Night. The Second Wave, a spectacular sandstone formation in the North Coyote Buttes, lies under a sky full of stars.
A hiker admiring the striated walls and dramatic light within Antelope Canyon, a deep narrow slot canyon formed by water and wind erosion.
The Second Wave at Sunset, Vermillion Cliffs. 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.
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.
Northern cardinal, male.
The Wave in the North Coyote Buttes, 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.
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.
Pyrrhuloxia, male.
Greater roadrunner.
Black-headed grosbeak, male.
Panorama of the Wave. The Wave is a sweeping, dramatic display of eroded sandstone, forged by eons of water and wind erosion, laying bare striations formed from compacted sand dunes over millenia. This panoramic picture is formed from thirteen individual photographs.
Monument Valley panorama, a composite of twelve individual photographs.
Light Beam in Upper Antelope Slot Canyon. Thin shafts of light briefly penetrate the convoluted narrows of Upper Antelope Slot Canyon, sending piercing beams through the sandstone maze to the sand floor below.
Lower Antelope Canyon, a deep, narrow and spectacular slot canyon lying on Navajo Tribal lands near Page, Arizona.
A hiker admiring the striated walls and dramatic light within Antelope Canyon, a deep narrow slot canyon formed by water and wind erosion.
Belt of Venus over Horseshoe Bend on the Colorado River. The Colorado River makes a 180-degree turn at Horseshoe Bend. Here the river has eroded the Navajo sandstone for eons, digging a canyon 1100-feet deep. The Belt of Venus, or anti-twilight arch, is the shadow of the earth cast upon the atmosphere just above the horizon, and occurs a few minutes before sunrise or after sunset.
Monument Valley panorama.
The Wave at Night, under a clear night sky full of stars. 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.
Belt of Venus over Grand Canyon at sunrise, viewed from Hopi Point on the south rim of Grand Canyon National Park. The Belt of Venus, or anti-twilight arch, is the shadow of the earth cast upon the atmosphere just above the horizon, and occurs a few minutes before sunrise or after sunset.
Lower Antelope Canyon, a deep, narrow and spectacular slot canyon lying on Navajo Tribal lands near Page, Arizona.
Lower Antelope Canyon, a deep, narrow and spectacular slot canyon lying on Navajo Tribal lands near Page, Arizona.
Monument Valley panorama, sunrise, dawn, stars in the sky.
Horseshoe Bend. The Colorado River makes a 180-degree turn at Horseshoe Bend. Here the river has eroded the Navajo sandstone for eons, digging a canyon 1100-feet deep.
The Great Wall, Navajo Tribal Lands, Arizona. Sandstone "fins", eroded striations that depict how sandstone -- ancient compressed sand -- was laid down in layers over time. Now exposed, the layer erode at different rates, forming delicate "fins" that stretch for long distances.
Agaltha Peak, also know as El Capitan Peak, rises to over 1500' in height near Kayenta, Arizona and Monument Valley. Agathla Peak is an eroded volcanic plug consisting of volcanic breccia cut by dikes of an unusual igneous rock called minette.
Light Beam in Upper Antelope Slot Canyon. Thin shafts of light briefly penetrate the convoluted narrows of Upper Antelope Slot Canyon, sending piercing beams through the sandstone maze to the sand floor below.
The Wave in the North Coyote Buttes, 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.
The Wave in the North Coyote Buttes, 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.
The Wave at Night, under a clear night sky full of stars. 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.
Grand Canyon at dusk, sunset, viewed from Grandeur Point on the south rim of Grand Canyon National Park.
Grand Canyon at sunrise viewed from Yavapai Point on the south rim of Grand Canyon National Park.
Grand Canyon at sunrise viewed from Yavapai Point on the south rim of Grand Canyon National Park.
Belt of Venus over Grand Canyon at dusk, sunset, viewed from Mather Point on the south rim of Grand Canyon National Park. The Belt of Venus, or anti-twilight arch, is the shadow of the earth cast upon the atmosphere just above the horizon, and occurs a few minutes before sunrise or after sunset.
Grand Canyon at dusk, sunset, viewed from Mather Point on the south rim of Grand Canyon National Park.
Lower Antelope Canyon, a deep, narrow and spectacular slot canyon lying on Navajo Tribal lands near Page, Arizona.
The Great Wall, Navajo Tribal Lands, Arizona. Sandstone "fins", eroded striations that depict how sandstone -- ancient compressed sand -- was laid down in layers over time. Now exposed, the layer erode at different rates, forming delicate "fins" that stretch for long distances.
Lower Antelope Canyon, a deep, narrow and spectacular slot canyon lying on Navajo Tribal lands near Page, Arizona.
Light Beam in Upper Antelope Slot Canyon. Thin shafts of light briefly penetrate the convoluted narrows of Upper Antelope Slot Canyon, sending piercing beams through the sandstone maze to the sand floor below.
Spectacular Horseshoe Bend sunrise. The Colorado River makes a 180-degree turn at Horseshoe Bend. Here the river has eroded the Navajo sandstone for eons, digging a canyon 1100-feet deep.
Grand Canyon at dusk, sunset, viewed from Grandeur Point on the south rim of Grand Canyon National Park.
Grand Canyon at sunrise viewed from Yavapai Point on the south rim of Grand Canyon National Park.
Grand Canyon at sunrise viewed from Yavapai Point on the south rim of Grand Canyon National Park.
Grand Canyon at sunrise, viewed from Hopi Point on the south rim of Grand Canyon National Park.
Sarah's Swirl, a particularly beautiful formation at White Pocket in the Vermillion Cliffs National Monument.
Hiker in Buckskin Gulch. A hiker considers the towering walls and narrow passageway of Buckskin Gulch, a dramatic slot canyon forged by centuries of erosion through sandstone. Buckskin Gulch is the worlds longest accessible slot canyon, running from the Paria River toward the Colorado River. Flash flooding is a serious danger in the narrows where there is no escape.
Lower Antelope Canyon, a deep, narrow and spectacular slot canyon lying on Navajo Tribal lands near Page, Arizona.
Brilliant red striations around the base of this pinnacle are responsible for its name: the Lollipop.
Buckskin Gulch hiker. A hiker moves through the deep narrow passages of Buckskin Gulch, a slot canyon cut deep into sandstone by years of river-induced erosion. In some places the Buckskin Gulch narrows are only about 15 feet wide but several hundred feet high, blocking sunlight. Flash floods are dangerous as there is no escape once into the Buckskin Gulch slot canyons. This is a panorama made of sixteen individual photos.
Brain rocks and clouds, sunset, White Pocket.
Pedestal rock, or hoodoo, at Stud Horse Point. These hoodoos form when erosion occurs around but not underneath a more resistant caprock that sits atop of the hoodoo spire.
Pedestal rock, or hoodoo, at Stud Horse Point. These hoodoos form when erosion occurs around but not underneath a more resistant caprock that sits atop of the hoodoo spire.
Lower Antelope Canyon, a deep, narrow and spectacular slot canyon lying on Navajo Tribal lands near Page, Arizona.
White Pocket, sandstone forms and colors are amazing.
A hiker admiring the striated walls and dramatic light within Antelope Canyon, a deep narrow slot canyon formed by water and wind erosion.
Antelope Canyon, a deep narrow slot canyon formed by water and wind erosion.
Geometric joints and cracks form in eroding sandstone.
Desert cottontail, or Audubon's cottontail rabbit.
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.