Canyon red
381 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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Click Here / Upper Antelope Canyon – USA Tour 2008 The Navajo name for Upper Antelope Canyon is Tse’ bighanilini, which means “the place where water runs through rocks.” Upper Antelope is at about 4,000 feet in elevation and the canyon walls rise 120 feet above the stream bed. Though dry most of the year, Antelope Canyon runs, and sometimes floods, with water after rains. It is the water, slowly wearing away the sandstone grain by grain, that has formed the beautiful and graceful curves in the rock. Wind has also played a role in sculpting this fantastic canyon. 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-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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A man sitting on a ledge near a canyon.
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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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Upper Antelope Canyon – USA Tour 2008 The Navajo name for Upper Antelope Canyon is Tse’ bighanilini, which means “the place where water runs through rocks.” Upper Antelope is at about 4,000 feet in elevation and the canyon walls rise 120 feet above the stream bed. Though dry most of the year, Antelope Canyon runs, and sometimes floods, with water after rains. It is the water, slowly wearing away the sandstone grain by grain, that has formed the beautiful and graceful curves in the rock. Wind has also played a role in sculpting this fantastic canyon. / Click Here 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. 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 beautiful thought / just occured to me… only to be gone / before I could / lock it in / my memory. Now it’s free / for the taker… only if you could / see it and / catch it / / / / /
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The undulating shapes of Antelope Canyon brought alive by the light. A candidate for my soon to be released dedsert calendar. Thumbs up or down?
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Antelope-Corkscrew Canyon is one of my favorite places to photograph at. You are taken there in the early morning and left there to wait on lighting that comes usually around 11 AM or so in hopes for some really strong and interesting beams of rays. This is one of three photos that I took within the twists and turns of the cavern. Antelope Canyon is so unique, it has also become known as The Corkscrew, Corkscrew Canyon, Upper Antelope, Wind Cave, or The Crack. This photograph was taken inside the upper Antelope-Corkscrew Canyon slot caverns near Page AZ. Photo exposure f8 @ 6 secs.
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Hello, The night in the Grand Canyon. Take with a Olympus SP 550
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Blossom’s_Photo_Gallery Rock Metamorphosis The colour of this rock has been changed over time due to the mineral deposits in the water flowing through this canyon. Wards Canyon, Carnarvon Gorge, Carnarvon National Park, Queensland. Featured in Textures_and_Materials and Abstracts_from_Nature – August 2008.
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Utah – USA tour 2008 Rich colours can be seen among the varied hoodoos, walls, and fins, the textures and formations were incredible. / I enjoyed the most amazing hike down to the bottom, the vista was so beautiful with remnants of snow contrasting against the vibrant colours. Bryce Canyon is not a “real” canyon. It is not carved by flowing water. Water is the active ingredient here, but in the form of “frost-wedging” and chemical weathering. For 200 days a year the temperature goes above and below freezing every day. During the day, melt water seeps into fractures only to freeze at night, expanding by 9%. Now as ice, it exerts a tremendous force (2,000-20,000 pounds per square inch). Over time this “frost-wedging” shatters and pries rock apart. In addition, rain water, which is naturally acidic, slowly dissolves the limestone, rounding off edges and washing away debris. Well worth a visit, stunningly 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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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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Scenic Byway 12 is one of the most scenic byways in the USA and has been for years. It starts at Red Canyon, just before Bryce Canyon and makes its way over Boulder Mountain and down into Capitol Reef National Park. As you head down the mountain, you will find a wonderland of trees dotting the hillsides and mountains such as colorful aspens, pines, spruce, and fir. The mid elevation provides pinyon pine and juniper. This photograph was taken near the Larb Hollow Overlook in the middle of the fall change. I have spent a great deal of time along this road and for anyone planning a trip, see some of the places to stop by and photograph below. Many of these little towns will have dirt or off roads which will lead you into canyons, slot canyons, and amazing back country scenery. For serious photographers you should plan on several days through this wilderness! Red Canyon – vermillion-colored rock formations and Ponderosa pines. / Cannonville – the gateway to Kodachrome Basin State Park. / Escalante – Devil’s Garden, Willow and Soda Gulch, and Hole-in-the-Rock. Keep a lookout for The Burr Trail, Hell’s Backbone, and Smokey Mountain roads. / Boulder – Anasazi Indian Village State Park and the Burr Trail Scenic Backway. / Larb Hollow Overlook – Waterpocket Fold in Capitol Reef National Park and the Henry Mountains. / Fish Lake National Forest – Fish Lake (don’t miss this lake!) / Capitol Reef National Park – bright colored cliffs, natural bridges, domes and stone arches, and the fruit orchards.
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Plaza de toros de Ronda a.k.a. the Bullring of Ronda. Ronda is one of the most beautiful little towns I’ve ever seen. In the south of Spain, it is built on a gorge, the old town on one side, the new town on the other. The Puente Nuevo bridge spans the gorge and stands 120m above the canyon floor. (A very impressive sight, I can tell you!) The bullring was built in 1785 and is one of the oldest operational bullfighting venues in Spain. In fact, I believe it may be one of the last bullrings still hosting fights (although very rarely). This image was featured in European Everyday Life September 25, 2008.
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I was here today on the Logan River, in the canyon not far from home. I loved the ‘just now turning’ leaves and magnificent reflections in the clear water… Little Boat and the butterfly wanted to go with me so I shot some pics of them as well… heehee..
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Tyrone, The lone defender of Canyon 9, is surprised by a Clawber. His particle weapon was calibrated to detect the movement of these biomechanical creatures, usually while still some zentrimes away. He gasped in the thin air, scrambling futilely to align the weapon, as the slashing claws decended…
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Waves in Sand Rock, Arizona, USA
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