Meteorites Found from Asteroid 2008 TC3
This week I'm in Houston for the 40th annual Lunar & Planetary Science Conference, where 1,500 researchers have gathered to talk shop about the solar system. And indeed the big space news this week involves high-stakes interplanetary events — but the story should be datelined "Almahata Sitta, Sudan" instead of "Houston, Texas."
Our saga begins a few months ago, when Planet Earth got an unprecedented visit from a small asteroid designated 2008 TC3. A telescopic observer atop Mount Lemmon, Arizona, discovered this incoming chunk of rock on October 6th, and it slammed into the atmosphere over northern Sudan just 19 hours later. Since the 1970s astronomers have tracked down thousands of asteroids that might someday strike Earth — this is the first discovery that actually did.
"We thought that was the end of the story," recalls Steve Chesley, the orbital specialist at NASA's Jet Propulsion Laboratory who pinpointed where and when 2008 TC3 would end its 4½-billion-year existence.
But a couple of weeks later Chesley got a call from Peter Jenniskens, who wanted details about the final flight path. A meteor specialist at NASA's SETI Institute in Mountain View, California, Jenniskens had recently returned from a highly successful effort to study the atmospheric reentry of a European spacecraft, and the blazing piecemeal breakup he'd witnessed gave him hope that pieces of the shattered asteroid might have survived and fallen from the sky as meteorites. All too aware of the stones' scientific potential, Jenniskens was determined to look for them — though he admits, "It was a long shot."
Six weeks later Jenniskens found himself standing in the Nubian Desert of northern Sudan with Mauwia Shaddad and a busload of 45 students and staff from the University of Khartoum, where Shaddad teaches physics. All the available information about the asteroid's track — gleaned from civilian and military satellite photos, detection networks on the ground, and eyewitness accounts — suggested that any meteorites from 2008 TC3 should lie along a roughly east-west track about 20 miles southwest of a remote Sudanese railway station called Station 6.
A Scientific Coup
Jenniskens's long shot had paid off. Now he had everything he needed to piece together the entire story of 2008 TC3. Chesley had computed the space rock's exact orbit before it collided with Earth, and an observing team had managed to record a spectrum of the asteroid just 2 hours before its demise using the 4.2-meter William Herschel Telescope in the Canary Islands. And, remarkably, pieces of that same asteroid were in hand.
That in itself was unprecedented. Geologists have spent decades trying to match the spectra of various meteorite types with their most likely asteroidal sources, but the match is never exact and so the associations remain unproven. "We have more than 40,000 samples of asteroids as meteorites," explains Michael Zolensky of NASA's Johnson Space Center, "but we don't know where a single one of them came from."
Once back in the U.S., Jenniskens rushed samples of the newly recovered meteorite — now officially named Almahata Sitta, the Arabic phrase for "Station 6" — to labs around the country. Those analyses revealed that the fallen stones belong to a rare meteorite class known as ureilites, dark carbon-enriched rocks that were once at least partly molten.
But even as ureilites go, the Sudanese stones are unique. Scattered here and there are blotches of carbon that have undergone extreme heating. "Of all the meteorites we've ever studied," comments analyst Andrew Steele (Carnegie Institution of Washington), "the carbon in this one has been cooked to the greatest extent." Moreover, the stones' interiors are full of holes (technically, vugs) lined with coating crystals of the magnesium-rich silicates olivine and pyroxene. Their overall porosity ranges from 10% to 25%, and they crumble easily — making it all the more remarkable that any survived.
Meanwhile, the flat, featureless spectrum of the meteorites is a dead ringer for that of the asteroid itself. As it turns out, 2008 TC3 was also a rare and little-understood asteroidal breed known as an F type. At some point it was chipped off a larger object; conceivably that's the unnamed F asteroid designated 1998 KU2 and numbered 152679, an Earth-crosser estimated to be about 1.6 miles (2.6 km) across. Its rapid spin assures that the surface lacks a dusty coating, which means the observed spectrum reflects its true surface character.
A careful researcher, Jenniskens has kept all this very hush-hush for the past few months. But he and his extensive team of collaborators have now published their findings in today's issue of Nature (it's the cover story).
You can learn more about the flurry of activity surrounding the impact of 2008 TC3 and the recovery effort by checking out press releases issued by the SETI Institute, Carnegie Institution, and the UK's Science and Technology Facilities Council. NASA has posted many illustrations about these remarkable events here.