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NSF-BSF: Earthquake temporal occurrence variability (clustering) observed in the longest d — NSF Award to Florida International Un

The Dead Sea Fault (DSF) in Israel provides a unique opportunity to study the long-term history of earthquakes along a major fault: in some places it passes under the Dead Sea, and evidence of past earthquakes is recorded in layers of seafloor sediments. When a large earthquake occurs, the violent shaking deforms the s

Award titleNSF-BSF: Earthquake temporal occurrence variability (clustering) observed in the longest d
Award ID2344420
AwardeeFlorida International University
CityMIAMI
StateFL
Amount obligated$375,718
Principal investigatorShimon Wdowinski
ProgramTectonics, Geophysics, SPSE-Study of Physics of Earth, XC-Crosscutting Activities Pro
Start date09/01/2024
AbstractThe Dead Sea Fault (DSF) in Israel provides a unique opportunity to study the long-term history of earthquakes along a major fault: in some places it passes under the Dead Sea, and evidence of past earthquakes is recorded in layers of seafloor sediments. When a large earthquake occurs, the violent shaking deforms the softest shallow sediments, forming “seismites”. Over 200,000 years worth of seismites have been documented in rocks and in core samples taken from a deep drill hole in the Dead Sea.
SourceNSF Awards

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