Sand stone
446 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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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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/ MCN: C90A3-645E0-856EB / / © Imber 2007. All photographs and artworks in this portfolio are copyrighted and owned by the artist, Imber. Any reproduction, modification, publication, transmission, transfer, or exploitation of any of the content, for personal or commercial use, whether in whole or in part, without written permission from the artist is strictly prohibited. All rights reserved. / / / / Sold as laminated print to RB member / / /
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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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Aperture priority programme / 1/400 sec / f/7.1 / ISO 100 / Spot metering RAW capture. Processed in Camera RAW and PS Elements. Water / Beach Art / Architecture / Stones / Forests / Landscapes / / /
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Location: Naher el Kaleb, Lebanon
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Some kind of dark stains left on the sand resmble fingers reaching otu from the tide as the sun sets over the beach near San Diego California
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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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A eroded piece of lava rock being pushed to and fro by the ebb and flow of the tides along a Maui beach.
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Sea Star Sculpture, Wategos Beach, Byron Bay / by Karin Taylor from the Beach Series I made this sculpture / on Wategos Beach Byron Bay / not another soul around / to give you an idea of the scale of the sculpture / most of the stones were the size of your palm / some twice that size and some smaller I had noticed large piles of beautiful stones behind me / began to create something out of them / intuitively, one stone at a time The song that really speaks for this piece is Echo Beach by Martha and the Muffins – click to see lyrics this was our signature song….along with Livin’ on an Island by Status Quo and of course 10CC’s Sunburn
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Australia Rock is located in the seaside town of Narooma in New South Wales, Australia.
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/ MCN: CCB37-A1E56-16AAA / / © Imber 2007. All photographs and artworks in this portfolio are copyrighted and owned by the artist, Imber. Any reproduction, modification, publication, transmission, transfer, or exploitation of any of the content, for personal or commercial use, whether in whole or in part, without written permission from the artist is strictly prohibited. All rights reserved. / /
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For Poppykitten’s comp – CAT=EVERYTHING ELSE This was taken on holiday in Croyde Bay, North Devon a great UK surfing beach. The wind was blowing up the beach and had blown sand away from the stones leaving them like this, lit by the afternoon sun. / . / © photogenique (dave peddie): using this image for any purpose and in any way, without prior permission, may lead to legal action. / . / Do check out Pete Langman’s great portfolio /
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Hi Guys, well finally got an internet connection so i thought i would share this one with you from corfu !!!!!
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The clff edges along the mornington peninsula’s cost line and the stunning sandstone and rock formations this shot was taken at st pauls ocean beach sorrento, © Keepsakes Photography / All the materials contained may not be reproduced, copied, edited, published, transmitted or uploaded in any way without my permission. My images do not belong to the public domain. / Using this image for any purpose and in any way, without prior permission, may lead to legal action /
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Gibson’s Beach, Port Campbell National Park, Victoria, Australia.
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Tree snag with sandstone cliffs in background. Established in 1909 Utah’s first national park will celebrate its 100th birthday next year. ~ ~ ~ ~ ~ Please don’t copy or download this image. My photos may NOT be reproduced and/or used in any form without my written permission. If you want this photograph, I would be honored for you to purchase it. ©2008 Patricia Montgomery | Bucks Mountain Galleries All rights reserved.
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The late evening sun casts a golden glow on the sandstone cliffs in Zion National Park. Established in 1909, Utah’s first national park will celebrate its 100th birthday next year. ~ ~ ~ ~ ~ Please don’t copy or download this image. My photos may NOT be reproduced and/or used in any form without my written permission. If you want this photograph, I would be honored for you to purchase it. ©2008 Patricia Montgomery | Bucks Mountain Galleries All rights reserved.
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This was the image I intended to submit with this title. Tyrifjorden, Norway.
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As usual, this time of year is filled with showers, squalls and all-day rain or snow. In showery weather the brief breaks are mostly worth a little trip outside with the camera. / This photo was shot on a stony beach on a late afternoon between the showers. Aperture priority programme / 1/40 sec / f/5.6 / ISO 100 / Spot metering RAW capture. Processed in Camera RAW and PS Elements Water / Beach Art / Architecture / Stones / Forests / Landscapes / / /
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detail from windswept beach – Northumberland
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St. Mary’s Lighthouse, Whitley Bay, Tyne and Wear, UK
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