EPS Highlights

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Slow earthquakes are characterized by slower fault slips than ordinary earthquakes but faster than stable sliding, with various characteristic timescales ranging from seconds to years. 
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Delta fronts are often characterized by high rates of sediment supply that result in unstable slopes and a wide variety of soft‐sediment deformation, including the formation of overpressured and...
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Almost all seismic stations around the world are based on land, leaving many oceanic earthquakes undetected. Harnessing the million-plus kilometers of underwater fiber-optic cables to monitor...