Stability of Moon South Pole Under Scrutiny Ahead of Artemis Human Lunar Landings
NASA-supported study Tectonics and Seismicity of the Lunar South Polar Region surveys recent LRO and historical Apollo Passive Seismic Network data to analyze 15 lobate thrust fault scarps, thought to be caused by interior cooling and Earth tidal forces, in the MSP region including in de Gerlache Rim, 1 of 13 candidate sites for Artemis 3; Modelling of associated shallow moonquakes (SMQ) indicate shaking up to 50km from epicenters, a safety concern especially for areas such as Shackleton crater which may be susceptible to regolith landslides; Further insight to be gained when Farside Seismic Suite is carried on Draper Series-2 lander to Schrödinger basin NET 2025 under CLPS