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China's Tianwen-2 has arrived at the asteroid that might be a piece of our Moon

22 June 2026 · 4 min read

Key takeaways

  • Tianwen-2 arrived at quasi-moon asteroid Kamoʻoalewa on June 7, 2026, after a 13-month transit
  • The asteroid may be a fragment of our own Moon: its spectrum matches lunar rock, though a new study disputes this
  • Three sampling methods will attempt to collect 100 grams of regolith from the fast-spinning surface
  • After returning the sample capsule in late 2027, Tianwen-2 heads for comet 311P/PanSTARRS, arriving 2035
Stars and space, representing China's Tianwen-2 mission to asteroid Kamoʻoalewa
Stars and space, representing China's Tianwen-2 mission to asteroid Kamoʻoalewa

On June 7, 2026, after 13 months in transit, China's Tianwen-2 spacecraft reached 469219 Kamoʻoalewa. The name comes from Hawaiian and means roughly "oscillating celestial fragment," which turns out to be a fair description of what this object is: a small, odd rock, somewhere between 40 and 100 metres across, that follows an orbit so close to Earth's it effectively chases our planet through space.

Astronomers call it a quasi-satellite. It's not gravitationally bound to Earth in the way the Moon is, but it loops in and around our planet's gravitational neighbourhood for decades at a time before drifting away. There are only a handful of confirmed quasi-satellites, and Kamoʻoalewa is the most accessible of them.

Is it a piece of our Moon?

The question that's driven most of the interest in Kamoʻoalewa is compositional. A 2021 study using the Large Binocular Telescope in Arizona found that its reflective spectrum more closely matched lunar rock than the typical chondrite makeup of most near-Earth asteroids, raising the possibility that it's a fragment blasted off the Moon by an ancient impact.

A new study published in Nature Communications, timed just before Tianwen-2's arrival, challenged that reading. The researchers argued that Kamoʻoalewa's surface looks more like ordinary space-weathered rock than actual lunar material. Both studies are working from Earth-based observations. The truth, presumably, is in the sample.

What happens next

Tianwen-2 is now in its mapping phase, surveying the asteroid from altitudes between roughly 300 metres and 20 kilometres above the surface. The point is to build a detailed topographic model that identifies a safe sampling site. Kamoʻoalewa spins faster than most asteroids of its size, which complicates landing, so the mission carries three different sampling methods: touch-and-go, hover collection, and anchor-and-attach. The plan is to collect about 100 grams of regolith before departing.

The sample return capsule is expected to separate from Tianwen-2 during an Earth flyby in late 2027, landing near the Jiuquan Satellite Launch Center. For context, Japan's Hayabusa2 returned just 5.4 grams from asteroid Ryugu in 2020, and those samples rewrote what we know about carbon-rich asteroids and the distribution of organic chemistry in the early solar system. 100 grams is genuinely useful.

After the handoff, Tianwen-2 won't stop. It's scheduled to continue to main-belt comet 311P/PanSTARRS, arriving in 2035, which would make it one of the most ambitious multi-target missions ever flown by any space agency.

The wider picture

This is China's first asteroid sample-return mission, and only the third in history after Japan's Hayabusa and Hayabusa2. CNSA has been characteristically tight-lipped about the mission timeline, but the autonomous deep-space navigation required to rendezvous with a small, fast-spinning object is exactly the kind of capability China is building out for its planned 2030 crewed lunar landing. Every mission like this is practice for something bigger.

Whether Kamoʻoalewa turns out to be lunar material or an ordinary space rock, the sample will tell us something new. That's not a guarantee in science, but it's a reasonable expectation. Watch for CNSA announcements on the formal sampling date over the coming months.

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