Dry
1 member found
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Michelle Dry
United Kingdom
1560 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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Please check out Kye Vincent
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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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Upper Antelope Canyon Is a spectacular petrified sand dune, created by wind, water and sand, presenting a sculptured masterpiece. / My Navajo Indian guide was lovely and explained many of the legends associated with this area. Was so lucky at one point to have the canyon to myself, peaceful, serene and incredibly beautiful. / . / WARNING / ©2008 Globalphotos All rights reserved. / All photographs, text and images by Globalphotos are the exclusive property of Globalphotos – protected under Australian and international copyright laws. / These images may not be reproduced, copied or manipulated without written permission. / No use for Public Domain. / Use of any image for another photographic concept or illustration is a violation of copyright.
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n the same series: / / /
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Tangled In This Mess / / They were fightless wounds and scars that could be seen only by her / Model: Jo O’Brien
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I found these Poppy seed pods on our house hunting venture and just loved their shape, colour and texture and taking these photos definitely took my mind off the move! The name of this image came from my kids as they call them tiny honey pots. Enjoy.
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Skeleton of desert plant. Studio still life. Photo based mixed medium image. Extreme image softness, textures, and grain.
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This dry leaf was on the camping table at the beach,all frozen.The sun was trying to dry it up again…..untouched.
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Title: Woke Up From the Strangest Dream / Artist: Jessica Tremp / Model: Jo O’Brien I dreamt of a stormy, wild sea. / Starfish clung anxiously to my eager limbs as I swam through murky waters hastily, escaping vicious sharks onto a windswept dark beach, where lovers ran from rogue waves up sandy banks to reach a safe haven of warm golden sun-kissed hair. / Intertwining. / Until one of them is swept away out of the others desperate clutches by angry water under a moist sky, slipping from unwired fingers and left counting an exhausted dolphin’s last heartbeats, cradling on the anguished shore of the sad, sad silence. other image from this location
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This is my youngest daughter’s toy rabbit, “Spike”. She won’t go to sleep without him and she always sucks her thumb while stroking his silky washing instructions label with her forefinger. She wore the original label away and we had to sew another one on! Needless to say Spike gets very smelly and needs washing regularly!
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One of the many dunes located in the Sahara desert in Libya. I thought this particular shot worked well in b&w. Any feed back would be appreciated. /
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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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Take a cut lunch to cross this paddock – this was shot across the road from Drought Stricken #2 Drought Set An Australian Artist to watch Rosalie Dale
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Kept driving past this on the way back from Leeds and kept thinking, “must take a picture of that tree sometime”. Got lucky with a good day when I had my camera with me:)
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From the Japanese Gardens, Portland, Oregon
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Old bushel basket with summer daisies.
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Sand dunes – Death Valley – April 2008 Shot as sand storm was brewing, no tripod :) . . ©2008 Globalphotos All rights reserved. / All photographs, text and images by Globalphotos are the exclusive property of Globalphotos – protected under Australian and international copyright laws. / These images may not be reproduced, copied or manipulated without written permission. / No use for Public Domain. / Use of any image for another photographic concept or illustration is a violation of copyright.
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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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Stovepipe Wells, Death Valley, California USA
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Lost in the desert (well, the beach anyway!)
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A dried Opium poppy seedhead. / This was taken about two months after I bought my first digital SLR and was still getting to grips with it. The photo was taken spur of the moment in my back garden using natural light only with no reflectors, and the background is bare earth (fortunately I had just dug it over and removed anything that could have been intrusive).
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