Results 61 to 70 of about 250 (169)
Dating a Medieval Tsunami With Uranium‐Series Techniques on Caribbean Corals
Abstract Uranium‐series dates from coral boulders constrain the timing of a medieval tsunami from the Puerto Rico Trench. Previously reported evidence for this tsunami includes hundreds of coral boulders that came to rest hundreds of meters inland on Anegada, British Virgin Islands.
K. Halimeda Kilbourne +8 more
wiley +1 more source
Differentiating Frictionally Locked Asperities From Kinematically Coupled Zones
Abstract Seismogenic areas on plate‐boundary faults resist slipping until earthquakes begin. The delay in slip relative to plate motion, termed slip deficit, represents plate coupling as an interseismic proxy of seismic potential. However, when a part of a frictional interface sticks together (locked), the unlocked sliding surroundings are braked and ...
Dye SK Sato +2 more
wiley +1 more source
Influence of Subduction Interface Geometry on Surface Displacements and Slip Processes in Cascadia
Abstract The subduction interface geometry is particularly important for estimating interplate coupling and surface geodetic motion, which has significant implications for seismic hazard mapping. Several published Cascadia subduction interface geometries derived from different seismic data sets vary significantly from one another. However, results from
H. M. Elston +2 more
wiley +1 more source
Australian paleoseismology: towards a better basis for seismic hazard estimation
Probabilistic seismic hazard analyses in Australia rely fundamentally on the assumption that earthquakes recorded in the past are indicative of where earthquakes will occur in the future.
K. McCue, D. Clark
doaj +1 more source
New stratigraphic evidence from the Cascadia margin demonstrates that 13 earthquakes ruptured the margin from Vancouver Island to at least the California border following the catastrophic eruption of Mount Mazama.
J. E. Johnson +2 more
doaj +1 more source
A reexamination of the observations and analysis recently reported to conclude that an 800 km section of the Himalayan Frontal Thrust ruptured in 1255 A.D. shows that the conclusion is flawed and without merit because of misinterpretations of trench logs
Ian Pierce, Steven G. Wesnousky
doaj +1 more source
Paleoseismological analyses were performed along the Campo Imperatore Fault (part of the Gran Sasso Range Fault System) in order to define the seismogenic behaviour (recurrence interval for surface faulting events, elapsed time since the last ...
M. Moro, P. Galli, F. Galadini
doaj +1 more source
Validation of seismic hazard curves using a calibrated 14 ka lacustrine record in the Eastern Alps, Austria. [PDF]
Daxer C +5 more
europepmc +1 more source
Earthquake-enhanced dissolved carbon cycles in ultra-deep ocean sediments. [PDF]
Chu M +39 more
europepmc +1 more source
Luminescence sediment tracing reveals the complex dynamics of colluvial wedge formation. [PDF]
Gray H, DuRoss C, Nicovich S, Gold R.
europepmc +1 more source

