50 years later, Apollo rocks are set to solve more puzzles
HOUSTON: The first person to set foot on the moon had one last task before he came home.
Neil Armstrong needed to pick up rocks - as many as he could carry, as interesting as he could find. The material he collected would constitute humanity’s first samples taken from another world.
With less than 10 minutes to go before the end of his moonwalk, Armstrong used tongs to pile about 20 rocks into a specialised collection box. Deciding it wasn’t full enough, he scooped an additional 13 pounds of lunar soil into the container.
Today, a tablespoon of that soil sits in a sealed dish in a locked and windowless lab at Johnson Space Centre in Houston. It is a prized piece of the Apollo program’s greatest scientific legacy: nearly 850 pounds of moon rocks.
For 50 years, research on these rocks has transformed our understanding of the moon, revealing the circumstances of its birth and the reasons for its mottled face. Now, NASA has decided to release three new samples for analysis - samples that no scientist has touched.
The upcoming experiments, on vacuum-sealed cores and a longfrozen rock, can be performed only once, at the precise moment the samples are opened. That’s why the materials have been held back since they were retrieved from the moon, said Ryan Zeigler, who curates the Apollo rocks collection. NASA was waiting for the right scientists, with the right technologies, at the right time.
With Apollo 11’s 50th anniversary this year and renewed interest in the moon ahead of a proposed return mission, Zeigler said, the right time is now.
NASA’s Lunar Sample Laboratory, a maze of gleaming metal cabinets and spotless linoleum floors, was built in the 1970s to house the rocks brought back from six moon missions.
A sophisticated HVAC system, designed to keep the air 1,000 times cleaner than in the outside world, fills the facility with a faint artificial breeze. Scientists enter only after donning special white jumpsuits, caps and booties to limit contamination.
These are some of the most valuable rocks in the solar system, Zeigler said. Just look at what they have revealed so far.
Before the Apollo 11 mission, scientists couldn’t agree on where the moon came from. It’s a misfit in the solar system - much larger relative to its planet than almost any other moon. Some speculated that it was once an independent object that was “captured” by Earth’s gravity. Others proposed that the satellite formed in orbit alongside Earth when the planets were coalescing out of a primordial dust disc. Many grade-school textbooks taught that it was, in fact, a blob of Earth that had been flung away by our planet’s spin; the Pacific Ocean was thought to be a scar from this ancient loss.
All of those theories had to be discarded as soon as scientists saw the first Apollo rocks.
The moon materials were extraordinarily ancient - as old as 4.5 billion years. Although they contained many of the same chemicals as rocks from Earth, they were startlingly poor in “volatiles” - molecules like water and carbon dioxide that easily vaporise when heated. Some contained features produced only in cataclysms - showers of meteorites, blasts from volcanoes, or barrages of particles from the sun.
At a conference to discuss the initial findings six months after Apollo 11 returned to Earth, no one could agree on what all this evidence meant.
Then, toward the end of the conference, geologist John Wood explained how the clues fit together. He realised that the strange white flecks in Armstrong’s hastily gathered soil sample belonged to an unusual type of rock called anorthosite, which forms when the mineral feldspar crystallizes out of molten rock.
At some point, Wood reasoned, the moon must have been completely covered in a magma ocean, in which anorthosite rocks floated like icebergs. The molten world would have cast an eerie, blood-red glow in Earth’s night skies.
To confirm Wood’s theory, scientists needed bigger and better samples. They got what they wanted in 1971, when Apollo 15 astronauts James Irwin and David Scott uncovered a half-pound chunk of anorthosite on the rim of a crater in the moon’s northern hemisphere.
Cleaning the dirt off the rock’s exterior, Scott realised what he was holding and started to shout. “Oh, boy!”
“Guess what we just found,” he exclaimed, as Irwin laughed with delight. “Guess what we just found! I think we found what we came for . . . . What a beaut.”
That sample came to be known as “the Genesis rock” - a nod to the role it played in helping scientists unravel the story of the moon’s origins. It sits inside its own glass case, not far from the dish containing Armstrong’s soil.
“These exact samples told us how the moon formed,” Zeigler said. — Washington Post.
Guess what we just found. Guess what we just found! I think we found what we came for . . . . What a beaut. – James Irwin, astronaut