Formation rock
429 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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Bend in the Colorado River located near the town of Page, Lake Powell and Glen Canyon in Arizona, USA. Spent sunset in this glorious spot along with millions of sand flies & mozzies LOL Shot laying on tummy hanging over the edge with wide angle :) . / . / 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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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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Once again perfecting my skills at near death experiences LOL / Different view of Horseshoe Bend :) Bend in the Colorado River located near the town of Page, Lake Powell and Glen Canyon in Arizona, USA. Spent sunset in this glorious spot along with millions of sand flies & mozzies LOL Shot laying on tummy hanging over the edge with wide angle :) . / 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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Azure Window was created by waves and rough seas breaking on the rocks over a period of thousands of years. On the top of two giant columns of rock, each with a diameter of about 40 metres, rests a huge ledge of rock measuring about 100 metres in length and 20 metres in height, forming a giant window which one can see beyond. For centuries the Gozitans have known this rare rock formation as it-Tieqa (the Window).
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One of my first photos on the Shen Hao camera, taken round at Crail harbour in Fife. / I placed myself right on the water’s edge, looking down as the tide came in and superimposed 3 exposures on the one frame to give the effect of water lapping around the rocks like mist. I think the red rock is carboniferous sandstone.
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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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“A pessimist only sees the dark side of the clouds, and mopes; a philosopher sees both sides and shrugs; an optimist doesn’t see the clouds at all …. he’s walking on them.” / - Leonard L. Levinson. / . / . / “Number Two Rocks” – South Australia. / © 2007. / . / . / /
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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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Incredibly shaped rocks in Hammersley Gorge, Karijini National Park/Western Australia Framing suggestion: / © aabz-imaging / ALL RIGHTS RESERVED
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Clicking on the image for a more detailed view is highly recomended. The last glow of the day gently renders the scene in soft hues.An incoming tide and swell has already forced me from my original composition and threatens to do so again…It’s a tedious wait for the exposure to finish without my gear and I getting wet ! / When viewed even at only 30% of the original 2 Sooty oyster catcher birds can sharply be seen on the rock outcrop in the right of frame. / Fuji G617 – Velvia 100F. / ©T.Middleton2008 —-—-—-—-—-—-—-—-—-—-—-—-—-—-—-—-—-—-—- / / see more of my TRUE panoramic photography by clicking on the image below / / -
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This pool in Karijini National Park is a bit hard to get to but well worth the effort. Framing suggestion: / © aabz-imaging / ALL RIGHTS RESERVED
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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, / /
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Horseshoe Bend is the name for a horseshoe-shaped meander of the Colorado River located near the town of Page, Arizona, in the United States. It is located slightly downstream from the Glen Canyon Dam and Lake Powell, about four miles or 6 km south of Page. Accessible via a 3⁄4-mile (1.2 km) hike from U.S. Route 89, it can be viewed from the steep cliff above, forming a spectacular vista. / This image is actually made of 4 pictures taken with my Canon 20D – 17-40mm L lens and stitched together to create this panoramic
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The Devil’s Marbles. This wonderful rock formation is near Tennant Creek, Northern Territory. This image was shot on film with a Nikon F70d and yes, I used a polariser to match the natural colours.
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Shot taken at Blairgowrie ocean beach, Victoria, Australia. /
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Image taken at the Grand Canyon Arizona-South Rim.
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This is Hound Tor at Dartmoor. It’s a great place, really interesting because the rocks are shaped like they’ve been manufactured by humans; all sort of square.
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The Compact Cassette, often referred to as audio cassette, cassette tape, cassette, or simply tape, is a magnetic tape sound recording format. Although it was originally intended as a medium for dictation, improvements in fidelity led the Compact Cassette to supplant reel-to-reel tape recording in most non-professional applications. Its uses ranged from portable audio to home recording to data storage for early microcomputers. Between the early 1960s and early 2000s, the cassette was one of the two most common formats for prerecorded music, first alongside the LP and later the Compact Disc. The word cassette is a French word meaning little box.
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