Chang’e-4 launched on 8 December and entered a highly elongated lunar orbit 4 days later. It then manoeuvred itself into a lower orbit. Mission management reportedly selected a landing site inside the relatively flat, 186-kilometre-wide Von Kármán Crater, which sits inside the much larger South Pole–Aitken Basin.
The basin — which is more than 2,500 kilometres wide — is thought to be the oldest of the Moon’s large, deep-impact basins, and it is the only such feature on the orb’s far side. Studying the basin has long been a top priority for Solar System researchers.
The basin is thought to have formed when a large asteroid hit the Moon towards the beginning of the Late Heavy Bombardment period, around 3.8 billion years ago. An accurate dating of the basin’s formation could reveal whether this epoch of battering — which must have affected Earth as well as the Moon — stretched over hundreds of millions of years or was concentrated in a relatively brief time.
After the successful Moon landings in the 1970s, some began to take a “been there, done that” view of the Moon, says Jeffrey Taylor, a lunar scientist at the University of Hawai’i in Honolulu. But China’s venture to the far side shows otherwise, he says. “We have not done it all or gone everywhere on the Moon.” Still, solving the mysteries of lunar history will require collecting samples and returning them to Earth for analysis, he adds.
Because the Moon’s rotation around its axis is precisely synchronized with its orbit owing to ‘tidal locking’, humans had no idea what the far side of the Moon looked like until the Soviet Union’s Luna 3 probe sent back the first shots of it in 1959. Luna 3 revealed a region pockmarked by many more craters than the near side — and virtually devoid of the ‘maria’, or seas of solidified lava, which dominate the familiar near side. (Apollo 11 landed on one such mare, the Sea of Tranquility.)
In the following decades, other probes followed up with detailed topographical and gravimetric mapping of the full lunar surface, but no craft has landed on the far side until now. (A NASA probe crash-landed on the far side in 1962.) Studying the region from up close could provide clues to why it is so different.
“The Chang’e-4 mission is an historic step in the Chinese lunar exploration programme and in international scientific exploration of the Moon,” says Jim Head, a planetary scientist at Brown University in Providence, Rhode Island, and a veteran of NASA’s Apollo programme. The mission will open up the ‘Luna Incognita’ — the unknown Moon — to surface exploration for the first time, he says.
Chang’e-4 and its 6-wheeled rover carry instruments that will do a range of experiments, including radio measurements of the early Universe; a study of the radiation environment of the lunar surface, led by Wimmer-Schweingruber; deep scans with a ground-penetrating radar; and analyses of the geology of the surface with an imaging spectrometer. Chang’e 4 also carries a small, climate-controlled environment with potato and Arabidopsis seeds and silkworm cocoons.
Chang’e-4 and its rover were originally built as a back-up to the previous lunar mission, Chang’e-3, which went successfully in 2013. China’s next Moon trip, Chang’e-5, will aim to return a sample of lunar rock to Earth, and is due to launch later this year.