First probe to explore far side of the Moon reveals secrets of lunar surface

Data could be used to reconstruct the history of our neighbour

Andrew Griffin
Wednesday 26 February 2020 20:00 GMT
Comments
Mysterious stripes on Saturn's moon Enceladus finally explained by scientists

Your support helps us to tell the story

From reproductive rights to climate change to Big Tech, The Independent is on the ground when the story is developing. Whether it's investigating the financials of Elon Musk's pro-Trump PAC or producing our latest documentary, 'The A Word', which shines a light on the American women fighting for reproductive rights, we know how important it is to parse out the facts from the messaging.

At such a critical moment in US history, we need reporters on the ground. Your donation allows us to keep sending journalists to speak to both sides of the story.

The Independent is trusted by Americans across the entire political spectrum. And unlike many other quality news outlets, we choose not to lock Americans out of our reporting and analysis with paywalls. We believe quality journalism should be available to everyone, paid for by those who can afford it.

Your support makes all the difference.

The first probe ever to explore the far side of the Moon has revealed new informaton about its surface.

The Chinese probe has revealed that the distant side – which cannot be seen from Earth since it always faces away from us – is covered with a layer of rock and dust.

It marks the first time that scientists have been able to confirm important information about the Moon's far side, which had only ever been explored from orbit until the Chinese Chang'e 4 spacecraft landed almost a year ago.

The layer of deposits was formed over billions of years as meteorites constantly smashed into the Moon's surface.

The findings, published in the journal Science Advances, reveal some of these loose deposits to be up to 39ft (12m) thick.

As most of the knowledge on lunar regolith comes from Nasa's Apollo and the Soviet Union's Luna missions to the near side of the Moon, scientists were, until now, uncertain whether these observations would hold true elsewhere on the lunar surface.

Dr Elena Pettinelli, a professor in the mathematics and physics department of Roma Tre University in Italy and one of the study authors, told the PA news agency: "These series of ejecta or deposits came from different impact craters that were created during the evolution of the Moon's surface.

"It is quite interesting because we can see quite clearly the geological sequences of these events 40 metres below the surface."

The Chang'e 4 (CE-4) spacecraft landed on the Von Karman crater on January 3 2019.

Its rover, Yutu-2, which can climb 20-degree hills and 8in (20cm) tall obstacles, was deployed 12 hours later to explore the landing site.

Previous landings have been on the near side of the Moon, which faces Earth.

The far side, which cannot be seen because it faces away from Earth, has been observed many times from lunar orbits but never explored on the surface.

Using data gathered from the first two days of Yutu-2's exploration, the researchers identified coarse granular materials up to a depth of 79ft (24m) below the lunar surface.

They were able to combine the rover's high-resolution images and ground-penetrating radar scans from 131ft (40m) below the surface to create a picture of the Moon's "internal architecture".

Although the radar signal could not be detected below 131ft (40m), the researchers speculate that these granular materials might extend deeper.

Dr Petrenelli said the information gathered from the Yutu-2 rover, along with the data from the previous near-side Moon explorations, could help shed light on the geological history of the lunar surface.

She added: "Maybe we can reconstruct historically the sequence of events in different areas on the Moon."

Additional reporting by agencies

Join our commenting forum

Join thought-provoking conversations, follow other Independent readers and see their replies

Comments

Thank you for registering

Please refresh the page or navigate to another page on the site to be automatically logged inPlease refresh your browser to be logged in