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Pragyan made 23 measurements as it rolled along a 338-feet (103-meter) region of the lunar surface, located within 164 feet (50 meters) of Chandrayaan-3’s landing site, for about 10 days. The rover’s data marks the first measurements of elements within lunar soil near the south polar region.

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Lunar samples are helping scientists to solve mysteries that remain about how the moon has evolved over time, including how it formed during the early chaotic days of the solar system.

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“All previous successful landings on the moon have been limited to equatorial to mid-latitude regions,” he said. “Chandrayaan-3 is the first mission to have a successful landing in the polar regions of the moon and carry out in-situ analysis. These new measurements in previously unexplored areas further enhanced the confidence in the (lunar magma ocean) hypothesis.”

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“Every time we land on the lunar surface, it anchors that understanding to a specific spot, a specific location on the surface, which is very useful for testing all the models and hypotheses we have,” he said. “That hypothesis of a magma ocean drives so much of what we think about the moon, especially early in its history. The rover results from the Chandrayaan-3 mission add another surface data point.”

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Each mission not only adds another piece to the puzzle of understanding the moon but also affords insights into how Earth and other rocky planets like Mars formed. Scientists’ understanding of how the moon came to be drives models of how all planets form and change, including planets beyond our solar system, Petro said.

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