Research news on paleoseismology

Paleoseismology is the scientific discipline that investigates prehistoric and pre-instrumental earthquakes through geological records, primarily using stratigraphic, geomorphic, and structural evidence preserved in sediments and rocks. It relies on trenching across active or suspected faults, dating displaced or deformed strata (e.g., by radiocarbon, luminescence, or dendrochronology), and analyzing offset geomorphic markers to reconstruct the timing, location, magnitude, and recurrence intervals of past seismic events. These data constrain long-term fault slip rates, characterize earthquake recurrence behavior, improve seismic hazard assessments, and test models of fault interaction and earthquake cycle processes beyond the limited span of historical and instrumental records.

CT scans help detect ancient earthquakes in Hamilton Basin

In a world-first use of medical imaging technology, scientists have revealed the earthquake-generating potential of faults in the Hamilton and Hauraki areas. The study shows that hidden geological faults in Hamilton city ...

Ancient quakes along 150-mile fault system in Nepal revealed

A common misconception about research is that it takes place in climate-controlled labs with microscopes, beakers, and Bunsen burners. While that is true for many fields, obtaining geoscience data can demand fieldwork in ...

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