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Through much of the Big Sur region (and elsewhere, for that matter) the Pacific Coast Highway (Highway 1) is built on steep slopes that are naturally eroding into the Pacific Ocean. Often this erosion is slow and unnoticed, but occasionally it is more dramatic, when landslides take out large sections of highway in a r...
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- 1315
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The small hamlet of Seatown lies just to the east of Golden Cap, the highest point on the south coast of England. The National Trust own some 2000 acres of herb rich grassland and spectacular landslipped cliffs.
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The Charmouth landslide in April 2010. There is a gigapan image taken from this location in April 2009, things have changed considerably. During the Easter break numerous people became stuck in the quicksand flowing onto the beach; their footprints are clear to see, including the ones that stop!
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This landslide, located just east of the River Char at Charmouth, has been active for a number of years and getting a lot larger each year. There is a second gigapan image taken in April 2010 for comparison. For more information about the coast visit: www.charmouth.org
or www.jurassiccoast.com -
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A different angle from my former image of the Hope Slide
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The Kozushima Island located in the 180km south of Tokyo, and it is a volcanic island of 18 square km. This island is covered to the thick rhyolite lava and pyroclastic flow deposits that a lot of small volcanoes erupted. A representative volcano of Kozushima Island is the Tenjyousan volcano, and it is about 570m above...
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- 2034
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The last sunlight of the day illuminates the upper slopes of the Madison Landslide scar. Quake Lake is in the foreground, it's skeletal trees a testament to the deadly night fifty years ago.
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On August 17, 1959 the M7.5 Hebgen Lake Earthquake triggered a massive landslide that blocked the drainage of the Madison River and formed the modern day Quake Lake. This 360 degree panorama is shot from atop the landslide deposit. To the south one can see the landslide scar on the facing ridge. All around the camer...
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- 7011
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A relatively large landslide complex in SE Oregon. It is comprised of two major landslide features that originate from a single, broad source area. In map view it looks very much like a molar tooth with two roots extending to the Owyhee River. Each of the two slides have prominent rotational slump block components ne...
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- 3500
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On or about June 23, 1925 about 38 million cubic meters of rocks and debris slid northward off of Sheep Mountain and into the valley of the Gros Ventre River, forming an impoundment that now holds back Lower Slide Lake. Almost two years later a portion of this landslide dam failed and the resulting flood wiped out the...
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