Speleoseismology is the investigation of earthquake records in caves. Traces can be seen
in broken speleothems, growth anomalies in speleothems, cave sediment deformation …

The distribution and formation mechanisms of typical identified seismites are analyzed
based on various factors from plate tectonic positions, types of sedimentary basins and …

Large earthquakes (magnitude≥ 7.0) are rare, especially along slow-slipping plate
boundaries. Lack of large earthquakes in the instrumental record enlarges uncertainty of the …

We present a method to constrain the timing of fissure generation related to late Quaternary
seismic events using the uranium-series technique. Dated samples were from travertine …

There is limited understanding of temperature and atmospheric circulation changes that
accompany an Atlantic Meridional Overturning Circulation (AMOC) slowdown beyond the …

Observations of intraclast breccia layers in the Dead Sea basin, formerly termed “mixed
layers,” provide an exceptionally long and detailed record of past earthquakes and define a …

A comprehensive multisite paleoseismic archive of the late Holocene Dead Sea basin (past
2500 years) is established by constructing two age‐depth chronological models of two …

Changes in surface loads during glacial‐interglacial cycles and the associated flexure and
rebound of the lithosphere alter the stress field in actively extending regions and may lead to …

Abstract The Dead Sea rift offers a wealth of information about pre-instrumental
earthquakes. The types of potential archives include historic seismicity, archaeological sites …

Travertine deposits have long been considered as powerful tools for investigating
neotectonics and reconstructing palaeoseismic events. We document, for the first time, the …