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The awesome Cliff House Motel and Restaurant sign in Wahoo, Nebraska.
The motel itself was nowhere to be found as far as I could tell. It opened in 1961 and was still open in 1983.
Los acantilados de Dover (en inglés: White Cliffs of Dover) forman parte de la costa británica frente al estrecho de Dover y Francia. El acantilado, que alcanza hasta 106 metros de altura, debe su llamativa fachada a su composición de creta (de color blanco puro de carbonato de calcio) acentuado por vetas de pedernal negro. Los acantilados se extienden al este y oeste desde el pueblo de Dover en el condado de Kent.
Los acantilados tienen un gran valor simbólico para el Reino Unido debido a que encaran a la Europa continental a través de la parte más angosta del Canal de la Mancha, donde históricamente han amenazado invasiones y en contra de los acantilados que forman una guardia simbólica. Porque el cruce de Dover fue la principal vía para el continente antes de los viajes aéreos, la línea blanca de los acantilados también constituyó en la primera (o última) vista para los viajeros del Reino Unido.
Vaya paliza de andar...Creo que mereció la pena. Espero que os guste. Una "cuña publicitaria" entre tanta fotografía callejera.
Home again to Oregon but had lovely time in Ireland. Here are a couple shots of the cliffs. More time and I'd have walked further, though the steep parts were scary.
On the way to the Summit of Slieve League - we never actually got to the top. These cliffs are supposed to be the highest sea cliffs in Europe...
I was walking on the cliff to the right one day last month when a security guard came up to kick me off the site. People used to camp up there and now they have security guards watching the spot. He told me someone had died after falling off a cliff. "This cliff?" I asked. "One of them," He said. I had read about the death and wondered where he fell from. I guess it doesn't matter. They're all dangerous.
I drove up here last month intending to shoot north of the old pier, but stopped when I saw the trail down to this spot. I'd never been down here. Not sure why not, maybe it just looked uninviting or something. I went down and loved it so much I basically camped here for a week to shoot some differing conditions. This was a shot from a day with calm surf but some nice color.
Chalk cliffs at Birling Gap in East Sussex suffered 7 years worth of erosion in the storms this winter.
A reef surf break is in front of this cave. The homes overlooking Terra Mar Point can be seen in the distance.
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Head of the Bight
South Australia
The Bunda Cliffs are composed of limestone, which extends far inland. The cliff face ranges in height from 40-80 metres, and stretches west for 800 Km.
There are three distinct units of limestone. The light coloured base, Wilson Bluff Limestone, formed when sea levels were higher and the Southern Ocean inundated southern Australia. Skeletons of billions of marine organisms were eventually deposited on the submerged plain to form the limestone.
The next cliff layer is the Nullarbor Limestone. This began forming 25 million years ago, again due to inundation and sedimentation.
The cliffs are capped by the Bridgewater formation, formed between 1.6 million and 100, 000 years ago. It consists of a hardened layer of windblown calcareous sand.
info sign at the site
9 different types of highly detailed rock formations – various cliff covers, ramp, platform. This is 100 % mesh items with custom physics (great for combat sims), material viewer ready, 512 and 1024 pix texture versions.
The Sea Cliff Bridge is a balanced cantilever bridge located in the northern Illawarra region of New South Wales, Australia.
The Sea Cliff Bridge replaced a section of Lawrence Hargrave Drive that was permanently closed in August 2003 due to regular rock falls.
The bridge was officially opened by NSW Premier Morris Iemma at a 'ribbon cutting' ceremony on 11 December 2005, and The Sea Cliff Bridge was named by 11 Year old schoolgirl following a naming competition opened to local primary school students