Caves
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Jennifer and P...
Australia
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caves
1437 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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WINNER – Gaia – The Living Planet Competition Best viewed LARGE Untouched Photograph.
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Location: Kingsgate Beach, Thanet, Kent, England Map: Google Maps Date and Time: 4 August 2007, 5.30 a.m. Camera details: ISO 200 : f/22 : 1/2 second : 18mm : Nikon D40 : Nikon 18-55mm lens Shot narrative: / Minutes after the sun had risen up over the sea, the low light was just lighting up the wall nicely and there was a nice selection of colours still in the sky. I’d only noticed the cave when the bright red caught the corner of my eye as I was walking along the beach Other shots from Thanet:
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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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Film location for the movie - The Chronicles of Narnia – Prince Caspian Cathedral Cove – New Zealand – June 2008 / 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. 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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Princess Caves was taken along the Railay Peninsula, Southern Thailand. / The whole coastline is like this, dramatic and craggy limestone. Railay also being a rock climbing mecca in these parts with climbers coming from all over the world to climb these monoliths…thanks for looking.. / rgs, Rob.
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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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This photo is a personal favourite.. The ice-cave sof Antarctica are amazingly beautiful and alluring, yet incredibly dangerous. They shimmer with frigid, crystalline magic, daring you to sail on in to admire the interior decoration, yet the ice crystals could so easily become incisors in the jaws of destruction..
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Photograph
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Full View Please ..::Stock Photo Credit::.. / Model / Background / Cave / Shell / Texture If you like this piece, please check out: / / /
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Snow cave melt, Bogong High Plains, Victoria, Australia. / © Ern Mainka A remnant patch of snow covering a small creek still left in summer. / Another view of it HERE
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I took this shot on Bell Island, if you look closely at the base of the cliff you can see a natural tunnel that has been bored through the rock by the water and out to the other side. The bravest and most daring of kayakers venture into these tunnels to explore. / / Visit my website On The Rock Photography / / /
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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 last weekend we went to a place i have not been to in years, i remember this form my chidhood, it was known as the bat cave then, it was full of bats, i didnt see any when i went back. This is in the woods at Rockley, South Yorkshire, this has not changed at all apart from the bars that prevent you from goin in! /
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Panorama shot inside a shallow cave along the Mornington Peninsula. Vic. Aus..actually taking in around 180deg. fov..The cave itself is around 20 feet high…thanks for looking and comments most welcome…rgs, Rob.
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An interesting story to this image as I ventured out into the cave to grab this image. My wife was worried because teh waves would come flowing in but I figured it was ok when a surfer went gliding by me. It seems they use that cave to get access to the better waves on the far sde of the cave.
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Taken from inside the rather large overhang cave behind Horseshoe Falls in Hazelbrook, 15 minutes walk from my house….. lucky me!!!
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When you find ice this colour it really takes your breath away! / / (Antarctic Peninsula) / / / / / / / / / / / / / / / / / / / / / / / / / / / / / / / /
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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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Antelope Canyon. This is actually flopped on its side because I like the wave feel it creates this way.
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