Scientists propose using seismic waves generated by moonquakes to help locate potential water-ice deposits on and under the Moon’s surface. The approach treats moonquakes like natural “locator beacons,” allowing researchers to infer what lies beneath the regolith where ice may be present.
Both outlets note that lunar ice is difficult to identify through ordinary imaging because many deposits would not be clearly visible from the surface. Instead, the method relies on specialized subsurface mapping to detect differences in how seismic waves travel through different materials. By analyzing wave behavior from moonquake events, researchers aim to improve estimates of where ice could be buried, supporting future exploration and potential resource use.
While the articles focus on the same concept—moonquake seismic sensing as a tool for finding lunar ice—they present it primarily as a proposed technique rather than reporting new observational results. The emphasis is on the practical challenge of mapping hidden ice and on how seismic data could address it.
