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The Earth Story

@earthstory / earthstory.tumblr.com

This is the blog homepage of the Facebook group "The Earth Story" (Click here to visit our Facebook group). “The Earth Story” are group of volunteers with backgrounds throughout the Earth Sciences. We cover all Earth sciences - oceanography, climatology, geology, geophysics and much, much more. Our articles combine the latest research, stunning photography, and basic knowledge of geosciences, and are written for everyone!
We hope you find us to be a unique home for learning about the Earth sciences, and we hope you enjoy!
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Slide in Bingham Canyon Mine The Bingham Canyon mine in Utah is, by volume, the largest open pit mine in the world. It has produced a huge amount of material, most notably copper, but also silver, gold, and molybdenum – in fact, it accounts for all nearly all of those materials produced in the entire state of Utah. In 2013, the mine suffered a major collapse which interrupted production for about 3 years. On May 31, a smaller portion of the walls of that mine collapsed, as seen in these press photographs.

Source: facebook.com
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This is a drone video of the landslide that occurred in Alta, Norway earlier this week. No one was hurt, and even a dog was rescued after it was able to swim back to shore.

This type of slide is thought to occur on a "Quick Clay" layer, produced as the glaciers departed at the end of the last glaciation. 15,000 years ago - Norway and Scandinavia were covered by a gigantic ice cap. The weight of this ice cap actually pressed down the Earth's crust - like using your hand to push a toy down to the bottom of the bathtub.

When the glaciers melted, the ocean returned, flooding the land you see above the water today. Those ocean waters deposited thin layers of clay and salt on the newly-submerged landscape. But, as the weight of the glaciers was also removed, the land began popping up, bringing this thin layer of ocean sediments above the surface. For the last 10,000 years, sediment from the land buried this thin clay layer, and now houses are constructed on some parts of that landscape. Today, it sometimes only takes a small event, like a rainstorm that dissolves some of the salt, to make that clay layer weak enough to trigger a slide.

-JBB

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Slides This amazing image of a formerly forested slope was captured outside of Atsuma town on Hokkaido Island, Japan, after a major earthquake followed shortly after heavy rains from Typhoon Jebi. Loose sediment making up the slopes in this area, waterlogged and heavy after the rains, liquefied and collapsed downwards during the quake, taking huge numbers of trees along with. There’s a good chance you will never see more landslides in a single photo in your lifetime. Reportedly, basically all of Hokkaido Island lost electric service during the quake. About a dozen people are known to have died, with several dozen more missing as of last press reports. -JBB Image source: AAP http://bit.ly/2MWjO8L More: https://wapo.st/2wSk9hQ

Source: facebook.com
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Cap Blanc Slide

Some of the largest debris flows on Earth happen in sediments deposited on continental shelfs, where large piles of debris from the continent accumulate on bedrock that slopes shallowly towards the ocean. This area off the coast of Mauritania in West Africa shows several large slides where 100 meter thick piles of sediment broke away and began moving downslope. The largest scarp visible in the seafloor bathymetry is called the Cap Blanc Slide.

The seafloor in this area shows two scarps, separated by tens of kilometers. Each represents a point where a slice of sedimentary layers broke away and moved downslope by at least a kilometer. The biggest of these submarine landslide deposits have the potential to trigger tsunamis on nearby coastlines, so understanding how these slides occur is important for understanding geological hazards.

Scientists collected seismic data and drill core data from ocean vessels to characterize this slide. The seismic information is collected by sending waves of energy down through the water column. When those waves hit layers in the ground they reflect back up towards the surface where they can be detected by floating seismic instruments. The cross section image shows those seismic reflections and lets scientists see what layer in the sedimentary package hosted the slide and even revealed a buried, unknown older slide at this location.

Seismic data showed that the slide moved on a couple layers buried up to 200 meters beneath the seafloor. When scientists drilled into them, they found that the layers were made of diatomaceous ooze. These layers are the remnants of blooms of certain types of plankton in the ocean. They make tiny shells out of silica and when they die, their bodies sink to the bottom. At this site, those diatom rich layers served as weak layers enabling hundreds of meters of additional sediment to slide on top of them.

-JBB

Image credits and original paper: https://bit.ly/2w0iZnA

Source: facebook.com
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natgeo Video @ladzinski & @andy_mann / The hallmark of any grueling expedition is the ability to laugh along the way with your friends as much as possible. It makes the hard times tolerable and the good times even that much better. We just returned from a 6 week expedition to Southeast Greenland, a mission led by @mikelibecki, where @ethan_pringle and Mike climbed the hardest route in the country up an unnamed mountain. A burly first ascent on un-chartered terrain. On the long boat ride back to Tasiilaq, Ethan wasn't done with "firsts" and decided to ride an inflatable slice of pizza down a 300 foot iceberg, launching into the icy waters. This trip was peppered with moments like this, the ones that make you feel like a kid again and keep you and your friends laughing. Hope you enjoy watching it as much as we did in person 😂
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