Astronomie - This Yellow Egyptian Glass Was Forged by a Meteorite Impact 29 Million Years Ago



King Tut's tomb included an artifact called a pectoral, which incorporated a piece of Libyan Desert Glass as the scarab beetle at its center.

Visit the right patch of desert along the border of Libya and Egypt, and you could stumble on pieces of pale yellow glass, the traces of a meteorite impact that took place 29 million years ago.

That glass, one notable piece of which was used in jewelry found in King Tut's tomb, has long been argued to have celestial roots. It's also the subject of a new study, which finds that so-called Libyan Desert Glass was likely created by a meteorite impact, not by an airburst of a space rock. If the research holds up, it suggests that scientists studying the threat of asteroids colliding with Earth may not need to worry so much about the consequences on the ground of large space rocks exploding in the atmosphere.

"Both meteorite impacts and airbursts can cause melting," lead author Aaron Cavosie, a geologist at Curtin University in Australia, said in a statement. "However, only meteorite impacts create shock waves that form high-pressure minerals, so finding evidence of former reidite confirms it was created as the result of a meteorite impact."

They knew that whether the glassmaking space rock hit the ground or not, it was large. But Cavosie and his co-author wanted to pin down whether the culprit was an impact or an airburst. So they worked with seven pieces of the pale yellow glass, looking at them under a high-powered scanning microscope. That let the pair get a close-up look at zircon crystals within the glass, which develop slightly different structures depending on what happens to them over the millennia.

That analysis suggested some of the zircon crystals had once been reidite, a mineral that only forms under very specific high-pressure circumstances that match what occurs when a meteorite slams into Earth, but not when such a space rock explodes in the air. (In an email to, Cavosie added that although scientists haven't spotted a crater to match the impact, there's a lot of sand in the area that could be hiding such a structure below the dunes.)

Cavosie and his co-author hope that's comforting news for planetary defense experts, who focus on the threat of asteroids colliding with Earth and what humans can do to protect ourselves. That's because after the airburst over Chelyabinsk, Russia, in 2013, people had worried that Libyan Desert Glass was formed during a much, much larger airblast.

Now, the geologists say that with the reidite identified in Libyan Desert Glass, that scenario is off the table. Combine that with the fact that geologists haven't tracked down any evidence of relatively recent reidite-free glass samples, and the findings suggest that even massive airblasts don't have as serious of consequences on the ground as some people had feared.


Quelle: SC


Overestimation of threat from 100 Mt–class airbursts? High-pressure evidence from zircon in Libyan Desert Glass

tmospheric airbursts over Russia at Chelyabinsk in 2013 and Tunguska in 1908 provide dramatic examples of hazards posed by near-Earth objects (NEOs). These two events produced 0.5 and 5 Mt of energy, respectively, which dramatically affected surface environments and, in the case of Chelyabinsk, injured humans. Enigmatic natural glasses have been cited as geologic evidence of the threat posed by large airbursts. Libyan Desert Glass (LDG) is a natural glass found in western Egypt that formed ~29 m.y. ago, however its origin is disputed; the two main formation hypotheses include melting by meteorite impact or melting by a large, 100 Mt–class airburst. High-temperature fusion occurs during both processes, however airbursts do not produce shocked minerals; airbursts generate overpressures at the level of thousands of pascals in the atmosphere, whereas crater-forming impacts generate shockwaves at the level of billions of pascals on the ground. Here we report the presence in LDG of granular zircon grains that are comprised of neoblasts that preserve systematic crystallographic orientation relations that uniquely form during reversion from reidite, a 30 GPa high-pressure ZrSiO4 polymorph, back to zircon. Evidence of former reidite provides the first unequivocal substantiation that LDG was generated during an event that produced high-pressure shock waves; these results thus preclude an origin of LDG by airburst alone. Other glasses of disputed origin that contain zircon with evidence of former reidite, such as Australasian tektites, similarly were also likely made during crater-forming events. Public-policy discussions and planning to mitigate hazards from airbursts caused by NEOs are clearly warranted, but should be cautious about considering LDG or other glasses with evidence of high-pressure shock deformation as products of an airburst. At present, there are no confirmed examples of products from a 100 Mt–class airburst in the geologic record.

Quelle: GeoScienceWorld



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