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Scientists just found the 'front door' to a massive cave on the moon

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The Moon's surface is pockmarked with more than 200 known pits where rocks and regolith collapsed into depths unknown. New research has found that one of those pits, in Mare Tranquillitatis, collapsed into a lava tube and made an underground cave conduit accessible from the lunar surface.

"We found a sort of front door to enter the subsurface," said Leonardo Carrer, a planetary scientist at the University of Trento, Italy, and first author on the research. Its access to the otherwise shielded lunar subsurface makes this pit a tantalizing site for future human and robotic exploration and could provide new insight into lunar volcanism.

Reflections from below

The Moon was once covered in seas of magma that eventually cooled into the dark basaltic maria visible today. Lunar scientists have long thought that like Earth, the Moon could host other volcanic features such as lava tubes.

Lava tubes form when a lava stream cools and forms a hardened exterior shell. Hot lava continues to flow through it like sludge in a pipe. Eventually, lava flows out of the tube and leaves a hollow conduit that could connect to emptied magma chambers or caves.

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"We had a lot of evidence on the surface of the Moon suggesting that lunar lava tubes could have existed," Carrer said. Lunar pits, elliptical craters that formed not from an impact but from the surface collapsing into an underground void, have been some of the most compelling evidence for these tubes. More than 200 of these pits have been imaged on the Moon's surface, and scientists speculate that they may be skylights into cave conduits, which happens on Earth when the top of a cave collapses and exposes it to the surface.

A black and white image of a hole on the surface of the moon.

The Lunar Reconnaissance Orbiter took this high-Sun image of the Mare Tranquillitatis pit in 2010.  (Image credit: NASA/GSFC/Arizona State University)

Carrer and his colleagues, including fellow University of Trento planetary scientist Lorenzo Bruzzone, wanted to know whether it was possible to map a hidden cave using orbital synthetic aperture radar (SAR) instruments. They first tested this method at two terrestrial cave systems in Lanzarote, Spain, and the Well of Barhout in Yemen, which are both planetary analogs. They used the SAR data to create 3D reconstructions of the two terrestrial cave systems near their entrances.

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