Sio Photos

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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
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.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 20605  
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, Paria Canyon-Vermilion Cliffs Wilderness
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.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 20606  
Grand Prismatic Spring (left) and Excelsior Geyser (right).  Grand Prismatic Spring displays a stunning rainbow of colors created by species of thermophilac (heat-loving) bacteria that thrive in narrow temperature ranges.  The blue water in the center is too hot to support any bacterial life, while the outer orange rings are the coolest water.  Grand Prismatic Spring is the largest spring in the United States and the third-largest in the world.  Midway Geyser Basin, Yellowstone National Park, Wyoming
Grand Prismatic Spring (left) and Excelsior Geyser (right). Grand Prismatic Spring displays a stunning rainbow of colors created by species of thermophilac (heat-loving) bacteria that thrive in narrow temperature ranges. The blue water in the center is too hot to support any bacterial life, while the outer orange rings are the coolest water. Grand Prismatic Spring is the largest spring in the United States and the third-largest in the world. Midway Geyser Basin.
Location: Midway Geyser Basin, Yellowstone National Park, Wyoming
Image ID: 13571  
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, Navajo Tribal Lands, 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.
Location: Navajo Tribal Lands, Page, Arizona
Image ID: 28570  
The Wave at Night, under a clear night sky full of stars.  Photographer is illuminating the striated rocks with a small handheld light. The Wave, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes is 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. Photographer is illuminating the striated rocks with a small handheld light. The Wave, an area of fantastic eroded sandstone featuring beautiful swirls, wild colors, countless striations, and bizarre shapes is 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.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 28620  
The Second Wave at Night.  The Second Wave, a spectacular sandstone formation in the North Coyote Buttes, lies under a sky full of stars, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
The Second Wave at Night. The Second Wave, a spectacular sandstone formation in the North Coyote Buttes, lies under a sky full of stars.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 28627  
The Tree of Eons, a spectacular dendritic formation in the Bentonite Hills of Utah. Fantastic colorful sedimentary patterns, ancient Bentonite layers are exposed through erosion in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes.  Photographed just before sunrise with soft pre-dawn illumination. Aerial panoramic photograph
The Tree of Eons, a spectacular dendritic formation in the Bentonite Hills of Utah. Fantastic colorful sedimentary patterns, ancient Bentonite layers are exposed through erosion in the Utah Badlands. The Bentonite Hills are composed of the Brushy Basin shale member of the Morrison Formation. This layer was formed during Jurassic times when mud, silt, fine sand, and volcanic ash were deposited in swamps and lakes. Photographed just before sunrise with soft pre-dawn illumination. Aerial panoramic photograph.
Location: Utah
Image ID: 37951  
Panorama dimensions: 11000 x 15000
A hiker admiring the striated walls and dramatic light within Antelope Canyon, a deep narrow slot canyon formed by water and wind erosion, Navajo Tribal Lands, 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.
Location: Navajo Tribal Lands, Page, Arizona
Image ID: 17993  
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 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.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 20607  
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, Paria Canyon-Vermilion Cliffs Wilderness
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.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 28613  
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, Paria Canyon-Vermilion Cliffs Wilderness
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.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 28614  
Broken Hill and view to La Jolla, panoramic photograph, from Torrey Pines State Reserve, sunrise, San Diego, California
Broken Hill and view to La Jolla, panoramic photograph, from Torrey Pines State Reserve, sunrise.
Location: Torrey Pines State Reserve, San Diego, California
Image ID: 28397  
Panorama dimensions: 4332 x 11344
Milky Way galaxy rises above the Fire Wave, Valley of Fire State Park
Milky Way galaxy rises above the Fire Wave, Valley of Fire State Park.
Location: Valley of Fire State Park, Nevada
Image ID: 28428  
Elephant arch and stars at night, moonlight, Valley of Fire State Park
Elephant arch and stars at night, moonlight, Valley of Fire State Park.
Location: Valley of Fire State Park, Nevada
Image ID: 28435  
Scripps Pier and Christmas Lights during holiday season, night exposure, La Jolla Coastline, Aerial view, Scripps Institution of Oceanography
Scripps Pier and Christmas Lights during holiday season, night exposure, La Jolla Coastline, Aerial view.
Location: Scripps Institution of Oceanography, La Jolla, California
Image ID: 38181  
Lunar Eclipse Sequence Over Broken Hill, Torrey Pines State Reserve. While the moon lies in the full shadow of the earth (umbra) it receives only faint, red-tinged light refracted through the Earth's atmosphere. As the moon passes into the penumbra it receives increasing amounts of direct sunlight, eventually leaving the shadow of the Earth altogether. October 8, 2014, San Diego, California
Lunar Eclipse Sequence Over Broken Hill, Torrey Pines State Reserve. While the moon lies in the full shadow of the earth (umbra) it receives only faint, red-tinged light refracted through the Earth's atmosphere. As the moon passes into the penumbra it receives increasing amounts of direct sunlight, eventually leaving the shadow of the Earth altogether. October 8, 2014.
Location: Torrey Pines State Reserve, San Diego, California
Image ID: 29412  
Clearing storm clouds over Broken Hill, overlooking La Jolla and the Pacific Ocean, Torrey Pines State Reserve, San Diego, California
Clearing storm clouds over Broken Hill, overlooking La Jolla and the Pacific Ocean, Torrey Pines State Reserve.
Location: Torrey Pines State Reserve, San Diego, California
Image ID: 29416  
Milky Way galaxy rises above the Fire Wave, Valley of Fire State Park
Milky Way galaxy rises above the Fire Wave, Valley of Fire State Park.
Location: Valley of Fire State Park, Nevada
Image ID: 28554  
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, Paria Canyon-Vermilion Cliffs Wilderness
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.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 28619  
Vancouver Island hosts a profusion of spectacular anemones, on cold water reefs rich with invertebrate life. Browning Pass, Vancouver Island, Metridium farcimen
Vancouver Island hosts a profusion of spectacular anemones, on cold water reefs rich with invertebrate life. Browning Pass, Vancouver Island.
Species: Giant plumose anemone, Metridium farcimen
Location: British Columbia, Canada
Image ID: 35250  
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, Page, Arizona
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.
Location: Horseshoe Bend, Page, Arizona
Image ID: 35939  
SIO Pier, Scripps Pier, La Jolla.  The Scripps Institution of Oceanography research pier is 1090 feet long and was built of reinforced concrete in 1988, replacing the original wooden pier built in 1915. The Scripps Pier is home to a variety of sensing equipment above and below water that collects various oceanographic data. The Scripps research diving facility is located at the foot of the pier. Fresh seawater is pumped from the pier to the many tanks and facilities of SIO, including the Birch Aquarium. The Scripps Pier is named in honor of Ellen Browning Scripps, the most significant donor and benefactor of the Institution
SIO Pier, Scripps Pier, La Jolla. The Scripps Institution of Oceanography research pier is 1090 feet long and was built of reinforced concrete in 1988, replacing the original wooden pier built in 1915. The Scripps Pier is home to a variety of sensing equipment above and below water that collects various oceanographic data. The Scripps research diving facility is located at the foot of the pier. Fresh seawater is pumped from the pier to the many tanks and facilities of SIO, including the Birch Aquarium. The Scripps Pier is named in honor of Ellen Browning Scripps, the most significant donor and benefactor of the Institution.
Location: Scripps Institution of Oceanography, La Jolla, California
Image ID: 22286  
The Fire Wave, a beautiful sandstone formation exhibiting dramatic striations, striped layers in the geologic historical record, Valley of Fire State Park
The Fire Wave, a beautiful sandstone formation exhibiting dramatic striations, striped layers in the geologic historical record.
Location: Valley of Fire State Park, Nevada
Image ID: 26473  
Sunset at Dead Horse Point Overlook, with the Colorado River flowing 2,000 feet below. 300 million years of erosion has carved the expansive canyons, cliffs and walls below and surrounding Deadhorse Point, Dead Horse Point State Park, Utah
Sunset at Dead Horse Point Overlook, with the Colorado River flowing 2,000 feet below. 300 million years of erosion has carved the expansive canyons, cliffs and walls below and surrounding Deadhorse Point.
Location: Dead Horse Point State Park, Utah
Image ID: 27823  
Panorama dimensions: 5303 x 17695
Torrey Pines Cliffs lit at night by a full moon, low tide reflections, Torrey Pines State Reserve, San Diego, California
Torrey Pines Cliffs lit at night by a full moon, low tide reflections.
Location: Torrey Pines State Reserve, San Diego, California
Image ID: 28461  
Torrey Pines Cliffs and Pacific Ocean, Razor Point view to La Jolla, San Diego, California, Torrey Pines State Reserve
Torrey Pines Cliffs and Pacific Ocean, Razor Point view to La Jolla, San Diego, California.
Location: Torrey Pines State Reserve, San Diego, California
Image ID: 28487  
Quarter Moon over Broken Hill, Torrey Pines State Reserve, San Diego, California
Quarter Moon over Broken Hill, Torrey Pines State Reserve.
Location: Torrey Pines State Reserve, San Diego, California
Image ID: 28366  
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.
Location: North Coyote Buttes, Paria Canyon-Vermilion Cliffs Wilderness, Arizona
Image ID: 28601  
Dawn over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. The Henry Mountains are in the distance
Dawn over the Skyline Rim, Factory Bench and Lower Blue Hills, Utah. The Henry Mountains are in the distance.
Location: Utah
Image ID: 38025  
Aerial Photo of Raplee Ridge near Mexican Hat, Utah. Raplee Ridge is a spectacular series of multicolored triangular flatirons near the San Juan River.  Often called "the Raplee Anticline" the geologic structure is in fact better described as a monocline, according to the Utah Geological Survey
Aerial Photo of Raplee Ridge near Mexican Hat, Utah. Raplee Ridge is a spectacular series of multicolored triangular flatirons near the San Juan River. Often called "the Raplee Anticline" the geologic structure is in fact better described as a monocline, according to the Utah Geological Survey.
Location: Mexican Hat, Utah
Image ID: 39489  
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All photographs copyright © Phillip Colla / Oceanlight.com, all rights reserved worldwide.