Excerpt from IRIS animation showing how surface waves propagate through solid bedrock, poorly consolidated sediment, and water-saturated sand and mud. The sediment slows and amplified the waves, and the water-saturated surface is prone to liquefaction. Credit: IRIS
Latest posts by Alka Tripathy-Lang, Ph.D. (see all)
- Living through the Loma Prieta earthquake - October 21, 2021
- The Great Quake Debate: an interview with seismologist and author Susan Hough - August 27, 2020
- Salton Sea Swarm quiets down - August 12, 2020