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skpowell says...

The human body can be used as far more than just a vessel for our own daily activities. Given the right space and a creative mind, the human body can become a thing of art all its own. Interesting how many people you can fit in one small space, huh?

Or under a bush.

Bodies in Urban Spaces was created by an Austrian artist by the name of Willi Dorner and has placed the human body in a new light as well as the spaces that the human body can be viewed in.

What would you do if you started seeing human sculptures popping around across Ball State?

Filed under: art, body, Dorner, space, urban

Just stunning!

Filed under: photography, science, space, universe

rojblake says...

This video clearly shows the SRB parachute failing which led to the damage incurred by the booster as it hit the water.

Filed under: ares, Constellation, NASA, space, video

Michael says...

via 1x.com

The photograph is by John Colbensen and it was shot somewhere in Norway.

Filed under: astrophotography, landscape, night, Norway, ocean, panorama, photo, photograph, photography, seascape, sky, space, stars

Jlo says...

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Islands are some of the most beautiful, peaceful, violent, desolate and unique places on Earth. While experiencing a tropical island from its sandy beaches, or a volcanic island from its towering peaks is wonderful, experiencing them from above can be inspiring as well.

We’ve collected images taken by astronauts and satellites from space of some of the most interesting islands on the planet.

Atafu Atoll, Tokelau, Pacific Ocean

Around 500 people live on Atafu Atoll, mostly in a village that can be seen on the corner in the left of the image above. Atafu is just five miles wide and is the smallest of three atolls in the Tokelau Islands, a New Zealand territory.

Atafu is made up of coral reefs that surrounded the flanks of a volcano that has since become inactive and submerged. Like many tropical atolls, Atafu is very low lying and vulnerable to sea-level rise. This photograph was taken by astronauts aboard the International Space Station in January.

Image: NASA

Onekotan Island, Russia

An island within an island was created after a big eruption around 9,000 years ago caused the peak of Onekotan’s volcano to collapse, forming a caldera that subsequently filled with water. The island inside the caldera is known as Krenitzyn Peak, which is the highest point on the island at around 4,300 feet.

Onekotan is in Russia’s Kuril Islands between Japan and the tip of the Kamchatka Peninsula. The islands were formed by volcanic activity caused by the subduction of the Pacific Plate beneath the Eurasian Plate. Subduction can also generate some of the largest earthquakes on Earth, including a magnitude 9 here in 1952 which was followed a week later by Krenitzyn’s only historical eruption. This image was captured by the Advanced Land Imager (ALI) on NASA’s Earth Observing-1 (EO-1) satellite on June 10, 2009.

Image: NASA

Galapagos Islands, Pacific Ocean

The Galapagos Islands are the tops of volcanoes on the sea floor off the coast of South America along the equator. The volcanic activity that formed the islands is thought to be the result of a plume of hot mantle material rising from deep in the Earth’s interior.

The largest island, Isla Isabela, is made of the lava flows of six gently sloped shield volcanoes. The northernmost of Isabela’s volcanoes, at the top of the image above, is Wolf Volcano, which has erupted at least nine times since 1797. This image was taken by the Landsat 7 satellite in 2001.

Image: NASA/USGS

Maldives, Indian Ocean

The Maldives comprise 1,192 small coral islands adding up to just 115 square miles of territory. About 330,00 people live on the islands, the average elevation of which is a little more than 3 feet. It is probably the lowest country in the world.

This image of the North and South Malosmadulu Atolls was taken in 2002 by the ASTER instrument aboard NASA’s Terra satellite.

Image: NASA/ASTER

Henrietta Island, East Siberian Sea

This glacier-covered Russian island is just 6 miles wide. Beneath the ice, the island is made up of 500-million-year-old volcanic rocks overlain by younger sedimentary rocks. This image was taken by the Advanced Land Imager (ALI) on NASA’s Earth Observing-1 satellite on April 30, 2009.

Image: NASA

Eleuthera Island, Bahamas

The spectacular underwater formations to the west of Eleuthera Island are made of calcium carbonate sand that has been eroded off of coral reefs and deposited in dunes by ocean currents.

This 2002 image was captured by astronauts aboard the International Space Station. Located in the middle of the Bahamas, Eleuthra Island is 110 miles long, and in places just over a mile wide. Around 8,000 people live there.

Image: NASA

Augustine Volcano, Alaska

The most active volcano in Alaska’s Aleutian arc, Augustine Volcano’s biggest historical eruption occurred in 1883. It has been erupting for 40,000 years. This image, captured by The Advanced Spaceborne Thermal Emission and Reflection Radiometer on NASA ’s Terra satellite in April 2006, shows a steam or ash plume at the tail end of several months of explosive eruptions.

Image: NASA

Lesser Sunda Islands, Indonesia

The three largest islands in this image, and many smaller ones, make up Indonesia’s Komodo National Park which was established in 1980 to protect the world’s largest lizard species, Komodo dragon. The total area of the park is 230 square miles. The islands are volcanoes caused by the collision of two tectonic plates. This image was captured by the Advanced Spaceborne Thermal Emission and Reflection Radiometer on NASA’s Terra satellite in 2000.

Image: NASA/ASTER

Hawaiian Islands, Pacific Ocean

The Hawaiian Islands were formed by an upwelling plume of hot mantle material, called a hotspot. As the Pacific plate moved over the hotspot, it formed a chain of islands that first grew larger as they actively erupted, and then slowly eroded and sank below the surface of the ocean as the crust beneath them cooled.

Today, the hotspot is causing active volcanism on the Big Island of Hawaii. Kilauea Volcano has been erupting continuously since 1983. The rest of the islands, which get older from right to left, are Maui, Kahoolawe, Lanai, Molokai, Oahu, Kauai and Niihau. This image was captured by the MODIS instrument aboard NASA’s Terra satellite.

Image: NASA

Alejandro Selkirk Island, South Pacific Ocean

This small member of the Juan Fernandez Islands off the coast of Chile measure just under a mile across. But its 5,000 feet of elevation is high enough to reach the layer of stratocumulus clouds pictured above. The result is a type of flow known as a von Karmen vortex street. This striking, curly pattern of eddies can also be seen in clouds, and fluids or air moving past rounded objects such as an airplane wing. This image was taken by the Landsat 7 satellite in 1999.

Image: NASA/USGS


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Millennium Island, Republic of Kiribati, South Pacific Ocean

Also known as Caroline Island, Millennium Island is made of coral reefs that grew around a volcano, which is now underwater, leaving behind a central lagoon. The maximum elevation of the island is less than 20 feet above sea level. In the past, the island has been inhabited and mined for guano, though today there are no people and it is among the world’s most pristine tropical islands. This image was taken by astronauts aboard the International Space Station on July 1, 2009.

Image: NASA

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Filed under: beauty, earth, islands, read it, see it, space

spruiked says...

The Hubble telescope is returning incredible images of space. This close-up shows around 60 supernova remnants.

Filed under: hubble, photo, space

jonbeckett says...

You know the photo I took the other night of Jupiter and it's moons? Jupiter Today curiousity finally got the better of me, and I installed a rather wonderful application called "Stellarium" on my netbook, to figure out which moon was which. Rolling back the clock to about the right time-frame that we were in the back garden, the magic box of tricks tells us the following (click on the pic for a bigger version via Flickr); stars From left to right, they are Callisto, Europa, Io, and Ganymede. It also occurs to me that I should have pointed out that the pictures from the telescope are of course upside down and back to front - it's a reflector telescope!

Filed under: astronomy, crossposted, jupiter, moons, space, stars, tumblrize

Jlo says...

One of the greatest mysteries of astronomy is the problem of the missing mass: All of the matter scientists can see in the universe accounts for only a small percent of the observed gravity.

Astronomers often invoke the concept of dark matter to explain this discrepancy, but some researchers say the problem is really our understanding of gravity. These scientists tout an idea called MOND - Modified Theory of Newtonian Dynamics - to explain why the universe seems to behave as if there's much more matter in it than we think.

Instead of assuming that this missing mass exists in the form of dark matter, which scientists have yet to detect directly, MOND advocates say we must alter Einstein's theory of General Relativity.

Under MOND, mass is much more effective at bending space-time than under General Relativity, so it takes less stuff in the universe to account for all the gravity we measure.

Fudge factor still needed

Though no one has yet proven or disproven either dark matter or MOND, supporters of the latter are in the minority. And MOND may be becoming even more of a long shot, according to cosmologist Pedro Ferreira of Oxford University in England. Ferreira wrote a review article in the Nov. 6 issue of the journal Science assessing the current state of MOND ideas.

"My personal view at the moment is that dark matter is a far simpler theory than any of the modified theories that I've seen," Ferreira said. Nonetheless, he said MOND shouldn't be discounted out of hand just because it's the less popular idea, nor because many physicists are loathe to tamper with Einstein's General Relativity.

"Very few people have worked on MOND; a very large number of people have worked on dark matter," said Jacob Bekenstein, a physicist at Hebrew University in Jerusalem who has researched MOND. "To compare them is kind of silly because we don't really know enough of whether MOND is working well or not. Just too little effort has been going into MOND."

Bekenstein admitted that MOND was not yet a fully fleshed-out theory: It cannot make physical predictions on all scales of the universe.

When applied to just galaxies, MOND can predict very well the behavior that astronomers observe. But when MOND is applied to larger structures like clusters of galaxies, it fails. To make MOND work for clusters, it must include more complicated concepts, such as entities called dark fields, which are different from dark matter, but work in a similar way to alter the amount of gravity present.

"It seems like if you want to build a proper theory of MOND, you bring in something like dark mater through the back door," Ferreira said.

This fudge factor seems to defeat one of the primary purposes of MOND when it was first proposed, which was to avoid having to invent a mysterious unseen entity acting in the universe, such as dark matter.

Even Bekenstein admitted that involving dark fields in MOND is not ideal.

"If you work only on galaxies then MOND doesn't need any help," he told SPACE.com. "But if you go up to clusters it needs some help. This is one of the things I hold against MOND."

However ...

Bekenstein pointed out that dark matter isn't perfect either. Thirty years after it was proposed, scientists have yet to find the stuff out there in the universe, and the idea isn't yet ideal at predicting all manner of situations, either.

"In the models of galaxies with dark matter, you have to carefully adjust the distribution of dark matter," he said. "Since you don't see the dark matter you're kind of free to adjust what you want, but it's not very credible in my opinion. It's too free an idea."

Ferreira said some kind of answer may come soon with the advent of new satellites set to observe the distribution of mass in the universe more precisely.

"I think things are going to really heat up over the next 10 years," he said.

 

I just love this kind of stuff! There's such mystery out there...

Filed under: read it, science, space

skpowell says...

In 2005, a large crack was discovered in the desert of Ethiopia. At first, there were a few theories as to what this rift might be and what could possibly come of it in the future, but after further study the general consensus is that this might be the beginnings of a new ocean. Using their knowledge of similar events and the formation of rifts in the ocean floor, geologists have been able to guess what will happen with this current rift.

It is now understood that this rift, small when you take time to consider the true scale of the world, could become a new ocean in as little (on a geological time scale) as one million years. After all, they do believe the rift opened in a matter of days.

For the full article, click here.

Filed under: desert, Ethipia, geology, ocean, repurposed, space, world

Mr. Fish says...

Kit Eaton writes: "Remember how the Ansari X-Prize resulted in the nascent commercial space trip business, with Virgin Galactic in the lead? Now there's a similar push to innovate space technology, but of a different sort: Space elevators, making the ride into orbit amazingly cheap and easy." -- FastCompany

 

Filed under: Space