Cave rock
284 creative works found
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Canon 20D – 17-40mm L – 17mm – 1s – f/11 Antelope Canyon is the most-visited and most-photographed slot canyon in the American Southwest. It is located on Navajo land near Page, Arizona. Antelope Canyon formed over the course of millions of years by erosion of the Navajo Sandstone, primarily due to flash flooding and secondarily due to wind erosion. Rainwater (especially during monsoon season) runs into the wash that Antelope Canyon is part of, picking up speed and sand as it rushes through the narrow passageways. Over time the passageways are eroded away, making the corridors wider and smoothing hard edges in such a way as to form characteristic ‘flowing’ shapes in the rock. Upper Antelope Canyon, called Tse bighanilini, “the place where water runs through rocks” by the Navajo, is the most frequently visited by tourists, due to two considerations. First, its entrance and entire length are at ground level, requiring no climbing. Second, beams (shafts of direct sunlight radiating down from openings in the top of the canyon) are much more common in Upper than in Lower. Beams occur most often in the summer months, as they require the sun to be high in the sky. / In the same series: / / /
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Antelope Canyon is the most-visited and most-photographed slot canyon in the American Southwest. It is located on Navajo land near Page, Arizona. Antelope Canyon formed over the course of millions of years by erosion of the Navajo Sandstone, primarily due to flash flooding and secondarily due to wind erosion. Rainwater (especially during monsoon season) runs into the wash that Antelope Canyon is part of, picking up speed and sand as it rushes through the narrow passageways. Over time the passageways are eroded away, making the corridors wider and smoothing hard edges in such a way as to form characteristic ‘flowing’ shapes in the rock. Lower Antelope Canyon, called Hasdeztwazi, or “spiral rock arches” by the Navajo, is located a few kilometers away from the upper Antelope Canyon and is a more difficult hike. In the same series: / / /
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WINNER – Gaia – The Living Planet Competition Best viewed LARGE Untouched Photograph.
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Antelope-Corkscrew Canyon, shows a powerful ray of light coming through the cavern top and illuminating the cave walls in brilliant orange-reddish colors. Antelope Canyon is so unique, it has also become known as The Corkscrew, Corkscrew Canyon, Upper Antelope, Wind Cave, or The Crack. This image was taken inside the cave with a 45 second time exposure to account for reciprocity failure. I use a Canon Elan with a 20mm lens and negative film. I still love the color depth in negative film vs. digital cameras :) Upper Corkscrew Canyon is located around the Navajo Reservations and usually requires a jeep to get you there. This location is just outside Page, Arizona.
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Antelope Canyon is the most-visited and most-photographed slot canyon in the American Southwest. It is located on Navajo land near Page, Arizona. Antelope Canyon formed over the course of millions of years by erosion of the Navajo Sandstone, primarily due to flash flooding and secondarily due to wind erosion. Rainwater (especially during monsoon season) runs into the wash that Antelope Canyon is part of, picking up speed and sand as it rushes through the narrow passageways. Over time the passageways are eroded away, making the corridors wider and smoothing hard edges in such a way as to form characteristic ‘flowing’ shapes in the rock. Upper Antelope Canyon, called Tse bighanilini, “the place where water runs through rocks” by the Navajo, is the most frequently visited by tourists, due to two considerations. First, its entrance and entire length are at ground level, requiring no climbing. Second, beams (shafts of direct sunlight radiating down from openings in the top of the canyon) are much more common in Upper than in Lower. Beams occur most often in the summer months, as they require the sun to be high in the sky. In the same series: / / /
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n the same series: / / /
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Sun Beam entering Upper Antelope Canyon, Arizona, USA. Antelope Canyon is the most-visited and most-photographed slot canyon in the American Southwest. It is located on Navajo land near Page, Arizona. Antelope Canyon formed over the course of millions of years by erosion of the Navajo Sandstone, primarily due to flash flooding and secondarily due to wind erosion. Rainwater (especially during monsoon season) runs into the wash that Antelope Canyon is part of, picking up speed and sand as it rushes through the narrow passageways. Over time the passageways are eroded away, making the corridors wider and smoothing hard edges in such a way as to form characteristic ‘flowing’ shapes in the rock. Upper Antelope Canyon, called Tse bighanilini, “the place where water runs through rocks” by the Navajo, is the most frequently visited by tourists, due to two considerations. First, its entrance and entire length are at ground level, requiring no climbing. Second, beams (shafts of direct sunlight radiating down from openings in the top of the canyon) are much more common in Upper than in Lower. Beams occur most often in the summer months, as they require the sun to be high in the sky. / In the same series: / / /
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Photograph
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Full View Please ..::Stock Photo Credit::.. / Model / Background / Cave / Shell / Texture If you like this piece, please check out: / / /
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I took this shot on Bell Island, if you look closely at the base of the cliff you can see a natural tunnel that has been bored through the rock by the water and out to the other side. The bravest and most daring of kayakers venture into these tunnels to explore. / / Visit my website On The Rock Photography / / /
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Antelope Canyon is the most-visited and most-photographed slot canyon in the American Southwest. It is located on Navajo land near Page, Arizona. Antelope Canyon formed over the course of millions of years by erosion of the Navajo Sandstone, primarily due to flash flooding and secondarily due to wind erosion. Rainwater (especially during monsoon season) runs into the wash that Antelope Canyon is part of, picking up speed and sand as it rushes through the narrow passageways. Over time the passageways are eroded away, making the corridors wider and smoothing hard edges in such a way as to form characteristic ‘flowing’ shapes in the rock. Lower Antelope Canyon, called Hasdeztwazi, or “spiral rock arches” by the Navajo, is located a few kilometers away from the upper Antelope Canyon and is a more difficult hike. In the same series: / / /
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Antelope Canyon. This is actually flopped on its side because I like the wave feel it creates this way.
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Natural Bridge, Numminbah Valley, / Gold Coast Hinterland, Queensland, / Australia
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This is the famous Seal cave in Oregon. They have a view point where the view is obscured by a cage. There is a small ledge of cement where you can sit a camera down and take a time exposure or at least try to hold your camera still. The view is though a small window in the cage for the camera. Those are seals on the rocks. The light was nice and my luck was good.
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This is one of many mine shafts that go deep into the heart of Bell Island and then these shafts run for several miles out and under the Atlantic Ocean. The mine is now closed as most of it has flooded and remains under water. / / Visit my website On The Rock Photography / /
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Antelope Canyon is the most-visited and most-photographed slot canyon in the American Southwest. It is located on Navajo land near Page, Arizona. Antelope Canyon includes two separate, photogenic slot canyon sections, referred to individually as Upper Antelope Canyon or The Crack; and Lower Antelope Canyon or The Corkscrew. The Navajo name for Upper Antelope Canyon is Tse’ bighanilini, which means “the place where water runs through rocks.” Lower Antelope Canyon is Hasdestwazi, or “spiral rock arches.” Both are located within the LeChee Chapter of the Navajo Nation. source: wikipedia Taken with a Nikon D70s with a 18-200mm Sigma lens
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Acrylic & Mixed Media / Painted by Ciska 03/08 ORIGINAL FOR SALE / 70cm x 90cm / $860.00AU Ciska’s Original works also available at … / Top Frames Castletown Shopping Centre Townsville Queensland
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A view from inside the cavern at Natural Arch. / Not many people will be able to get inside the cavern now without getting a $225 fine from the EPA as they have put a closure on Natural Arch due to fear of it caving in, plus a frog species in or around the cave is now under threat.
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There is a wonderful headland at the south end of Caves Beach, on the Central Coast of New South Wales. Great for exploring but make sure you check the tides!
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Waves in Sand Rock, Arizona, USA
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Taken on the RB outing to the Blue Mountains (Australia) on Saturday 15 March. The caves and rocks were just amazing. / Landscapes Trees Cards EOD Rusty Flowers Architecture Macro CatchAll DM
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Crystal Cave, Bermuda – Aug 2006
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I stood there watching, wondering about what may have happend in that space over thousands of years. / And the little boy running around with his father pulls on my jeans, points and says “Look, the rock has teeth” / I smile. / After all. / He is right. / And I wonder how many children over thousands of years looked at that rock and saw teeth.
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