Deserted orange
244 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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Unfortunately the skies here in the desert are mostly hazy and full of sand and dust! There are not too many days when there are clear horizons with clouds, and to be able to catch a sunrise like this was just excellent! Located in Libya towards the Algerian border. / /
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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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Captured in Cave Creek, Arizona. Really liked the colors of the sky in this shot. / Other lightning photos: / / / /
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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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This is a dawn photo I took the other day (yes..the ‘sticks” are back!!) and having fun adding the flood filter again…
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Dawn at Jan Juc Beach, on the Great Ocean Road.
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Apophysis fractal and a bit of Photoshop for special effects. For my observant visitors … yes, this is the same fractal used in my 3d/photoshop work The Fire Joe
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A spectacular storm front approaches as I take my afternoon walk through the desert. Central Australia, 2005. [Creative Effects: Brightness adjustment and Omni Spotlight effects with Photoshop]
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i Created this art when i was 17 .. the day i went London to study art this is what i took with me , and they loved it , and got me a place in uni … one of my old work that i still keep close. —-—-—-—-—-—-—-—— Lina / came up with this story to tell , please visit her pages for more great poems . / Thank you Lina . / —-—-—-—-—-—-— / My King I was with him in the desert, / I was 12 / He was ageless / Me and my mother traveled with him / We were fighting once again, / The tribes fought for many things, / This time it was water.. / Holy Holy Water He was our King in the desert, / We went with him everywhere / And inside my soul / Out there, / Burning the tears off with / The heat of 1,000 years I fell in love I was 12 and I could not be caught / Looking at him as if I were worthy / My mother was a widow / And our kind took care of each other / In the desert / In the heat that cleansed / Our Hearts and our Minds / Praise be to Allah, / Praise be to Allah, / Al ham dulAllah.. He took each of us in with his eyes / His men fought hard and we hurt very few, / He said we would only take / What Allah would give us, And he was right, / His fighting / Clean and Pure / He was our King in the desert, / Our Prince of survival I was 12 then.. And I loved him….
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I Turned the water dragon lizard that lives outside are house into a dragon with hand drawn by pencil wings scanned in to the computer, then I added colour to the wings. Then I put my wife on it with my sons 3 dollar toy sword. As well the harness is my belt and the Sattel is my sister and laws.The back ground is the desert in Arizona. Five photos and one drawing and photoshop.
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Pastel drawing from Anatomy Eyes Series.
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The beauty of the Arabian horse, / the warmth of the setting desert sun. / This image is a play on shadows and / silhouettes. I hope you like it! More horses, dogs and pets here
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this image started life as a pencil sketch and evolved from there. The Double-mouthed sailtail generously tows his companion, Blockhead, across the Atlip desert. Blockhead shields Gorff from the watchful eye of the ever hungry Zylap. Their trusty, but aging pumpkin droid, brings up the rear.
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Pastel drawing of Salmon swimming under the desert with a dark night sky.
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Nature abstract painting. This weekend I was out in the Hajar Mountains , it is about an hour and half drive from Dubai city . here is what i call magic of nature , to me this is just God being an artist , we all can learn something from That. / these Mountains have many layers as you can see , millions of years old , and each layer only about 6 cm deep. Simply amazing what i Personally learn from Nature.it does not get better than this for me . / I kept the colors the textures the same as they are no playing around with Photoshop here.
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The original artwork is an acrylic painting on linen. Only greeting cards, matted prints and small size of laminated, mounted & framed prints are available to maintain image quality.
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A harsh environment to grow in, this tree has long ago given in to the hot and dry Australian outback.
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Captured in Cave Creek, Arizona. Thanks for looking. Other lightning photos: / / /
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Multiple storms on the Arizona desert…....one just leaving…....one just arriving…... as the sun sets. / PLEASE NOTE: The original file and prints are better quality and more detailed than the reduced sized views shown here.
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A view of Nachal Tzin in the Negev desert (the Tzin river, canyon wadi) as seen from David Ben Gurion tomb in kibbutz Sde Boker, Israel. / / Nahal Zin is 75 miles (120 km) long and drains 600 sq. miles (1550 sq. km). It is the largest wadi that begins in the Negev. The Nahal Zin was created by reverse erosion as the great height difference between the Negev Highlands and the Jordan Rift caused the underlayers to erode during the rainy season, resulting in the collapse of the harder strata of rock above. The landscape is mostly Eocene limestone, consisting of some brown-black layers of low-grade flint. The flint slows down the erosion of the limestone. / The Negev occupies 60 % of the land surface area of Israel and yet it is the least densely populated. Delineated as being south of Be’er Sheva and Dimona, it is mainly a stone and sand desert with sparse vegetation. However, following periods of heavy rain during the winter and early spring, the desert is transformed into a colourful carpet of flowers. / Sde Boker (Hebrew: שדה בוקר, lit. Cowboy’s Field, sometimes spelt Sede Boqer or some combination of the two) is an Israeli kibbutz in the Negev, in the South District of Israel, founded on May 15, 1952. It is part of the Ramat HaNegev Regional Council. / From 1963, it was the dwelling place of the first Prime Minister of Israel David Ben Gurion until his passing in 1973, when he was buried nearby at Midreshet Ben-Gurion aside his wife Paula Ben-Gurion. Ben-Gurion had a vision of cultivating the arid Negev desert and building up its surrounding towns such as Yeruham and Dimona. He believed that eventually the Negev would be home to many Jews who would move to Israel after having made aliyah, and he felt that Sde-Boker was a trailblazer and example for what should follow. / Sede Boqer is perhaps one of the most beautiful landscapes in the Negev. This oasis is situated on the loess plain overlooking the deep gorge of Nahal Zin. The area is especially good for raptors such as breeding Long-legged Buzzard, Bonelli’s Eagle, Lanner and Barbary Falcons. A feeding station at the eastern edge of the Zin Plain is maintained by the INRP A with the purpose of supplying supplementary food to the breeding Griffon and Egyptian Vultures and sometimes in winter, Black Vulture. On the ledges of towering cliffs, Sooty Falcons breed from mid-May until early October. The gorges also host breeding Desert Eagle Owl and Alpine Swifts, and in some winters, Sinai Rosefinch and Wallcreeper. / Image is an HDR process from a single RAW file *
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