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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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3D printed mount of “Sauropodomorph A” at the Antarctic Dinosaurs travelling exhibit (Natural History Museum of Los Angeles). Sauropodomorph A is a still unnamed Sauropodomorph (larger group that contains the Sauropods or “long necked” dinosaurs) from the Early Jurassic period of Antarctica, and is one of the few dinosaurs discovered on the continent so far. It is known from a fairly complete juvenile specimen from Mt. Kirkpatrick. Interestingly, this genus seems most closely related to Ignavusaurus (from southern Africa) rather than the other two known Antarctic Sauropodomorphs (Glacialisaurus, Sauropodomorph B). The most interesting thing about this mount, however, is that it was entirely 3D printed! With modern technology that involves scanning and digitizing fossils, paleontologists no longer have to fully remove fossils from pieces of a matrix, which minimizes the possibility of damage to the fossil. It also allows researchers to “unflatten” fossils, see inside fossils, see between two fossils that may be overlapping each other, and piece together fragmented pieces, all without manipulating and possibly destroying the original fossil. Here, you can see the original fossils of Sauropodomorph A, which may appear as a jumble of rocks to the untrained eye: A rib fragment (bottom left), the tail, most of the torso, arm, and leg (top), as well as the skull and lower jaw (bottom right).

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Submarine canyons

The waters of the Earth’s oceans hide many fascinating features. This image shows the topography offshore of the city of Los Angeles.

Like many areas of the world, the area just offshore is shallowly sloped and part of the continental crust, an area known as the continental shelf. That continent ends at a sharp break known as the continental slope, which slopes more steeply down toward the open ocean. At this boundary off Los Angeles, giant canyons have been cut. These are remnants of the recent glaciations. Sea level was lower, exposing parts of the continental shelf. Rivers including the San Gabriel River and the Santa Ana River migrated along these shelves, eroding into them and fixing their position in the form of these canyons. When the most recent glaciation ended, the oceans returned and submerged the canyons, leaving them stranded and hidden from view.

Despite being beneath the waters, these canyons still are active. Sediment carried by rivers to the ocean accumulates at the canyon heads and on occasion that sediment will tumble down, forming submarine avalanches and deposits of turbidites at the base. Similar canyons are found at the intersection between river valleys and the continental slope around the world, a remnant of the Pleistocene glaciations.

-JBB

Source: facebook.com
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Owens “Lake”

15,000 years ago, huge glaciers carved great valleys through California’s Sierra Nevada Mountain range. Moisture from the Pacific Ocean is rung out of the air as snow that falls at the range's peak, causing glaciers to flow both east and west from the crest of the range.

East of the Sierra Nevada sits Owens Valley, which receives very little rain because of the mountain range in the way. When the mountains were filled with glaciers, meltwater from those ice sheets fed huge streams and lakes that flooded the low ground from Owens Valley all the way to Death Valley.

Once the glaciers departed, Owens Valley converted into mostly a desert. It receives very little rain, but some streams are fed from snows and rains in the mountains. One of these, Owens River, flowed downhill from the tip of Owens Valley to a flat basin where it formed a lake known as Owens Lake.

That all changed in the early 20th century. The city of Los Angeles constructed an aqueduct that took the water flowing into Owens Lake, causing the lake to rapidly dry up.

Earlier we covered Iran’s lake Urmia, a brewing natural disaster that has shrunk by 88% in the last few decades (http://on.fb.me/1BvJUjE). After the city of Los Angeles took the water, Owens Lake completely dried up. As a consequence, all of the fine, salt-encrusted particles at the lake bottom were exposed to the wind and many were picked up, turning strong winds turned into dust storms.

In the 1970s, the United States passed the “Clean Air Act”, placing limits on air pollution, including particulate air pollution like that generated by an artificially dried lake bed. The Clean Air Act actually forced Los Angeles to act.

Starting in the late 1990s, small amounts of water were diverted back to Owens Lake, keeping the flat lakebed partially flooded and shutting down the dust storms. The presence of thin, salty layers of water have allowed algae to grow, turning the evaporation ponds red in many of the photos.

The environmental disaster that was Owens Lake has been partially contained, but the mountain lake that used to sit on this site will never come back. Something like Owens Lake may be the end result of many drying lakes around the world; kept just wet enough to prevent dust from blowing, but without enough water to create a vibrant ecosystem.

-JBB

Source: facebook.com
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Original caption:

Rolta Films took a trip through Southern California, hitting up Palm Springs, Joshua Tree, San Diego, Laguna Beach and of course Los Angeles. Taking with us our dear friend Ryan who talks us through his feelings about America and joined by other friends along the way... Yep It's another stupid one
Shot on: A7s II, Tamron 28-75mm Music: Recharge & Revolt - The Raveonettes
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Fossil bees!

This pair of images shows, on top, a modern-day leafcutter bee from the species Megachile rotundata and a very cool fossil find from the LaBrea Tar Pits. The bees come from a pair of full nests exhumed from a part of the tar pits; the same location has produced bones from animals 23,000 to 40,000 years old, and carbon-14 dating of the material in the nests gives the same age, so these bees are about that old. Many interesting specimens are preserved in the nests and have been found by scientists exhuming material from the tar pits, including the leafy walls of the nests themselves, adults, and pupae like this one.

The bees are from species that are widespread in the United States, but the presence of these bees at this site actually helps constrain how their distributions have changed during the big climate shifts that happened since the nests were made. The bees today have expanded ranges at higher elevations than is suggested by these fossil finds, indicating that as the climate of the area warmed, the bees moved uphill to follow similar temperature levels.

-JBB

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Source: facebook.com
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