Two reports describe how sedimentary basins can amplify shaking from distant earthquakes. Sedimentary basins are depressions in Earth’s crust, often relatively flat, and they are frequently chosen for building cities because the terrain is convenient and extensive. The research explains that during earthquakes, seismic energy can become trapped within these basin-shaped structures. Rather than dissipating, the trapped waves can build up and increase ground motion as they reverberate, effectively turning the basin into a natural “resonance chamber.” As a result, cities located above the basin can experience stronger shaking than locations outside the basin when an earthquake occurs at a distance. The combined accounts emphasize the basin’s geometry and the way seismic waves interact with sediment-filled structures. While earthquakes and their direct sources vary, the key shared point is that basin resonance can make distant shaking more destructive for communities built on these geological features.