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Moonquakes Will Pose Risks To Long-term Lunar Base Structures

A scene from a visualization of the Lee-Lincoln scarp in Taurus-Littrow on the Moon. This scarp is evidence of moonquakes that sent rocks and landslides across the surface. Seismometers left on the Moon by Apollo astronauts recorded hundreds of events between 1969 and 1977, including 28 shallow moonquakes. The study narrowed the locations of these quakes and found that many of them occurred near scarps, implying that the forces creating the scarps also caused the quakes, and they continue to shape the lunar surface. The Lee-Lincoln scarp was only about 13 kilometers from one of the epicenters identified by the scientists. Credit: NASA's Scientific Visualization Studio

Our Moon is a seismically active world and its long history of quakes could affect the safety of permanent base structures there. That's one conclusion from a study of quakes along the Lee-Lincoln fault in the Taurus-Littrow valley where the Apollo 17 astronauts landed in 1972. “The global distribution of young thrust faults like the Lee-Lincoln fault, their potential to be still active and the potential to form new thrust faults from ongoing contraction should be considered when planning the location and assessing stability of permanent outposts on the Moon,” said Smithsonian senior scientist emeritus Thomas R. Watters, lead author of the paper.



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