Archaeological structures that exhibit seismogenic damage expand our knowledge of
temporal and spatial distribution of earthquakes, afford independent examination of …

The Dead Sea Fault is an active transform fault linking opening in the Red Sea with collision
in the Taurus/Zagros Mountains. Motion is left-lateral and estimated at approximately 5–7 …

The Dead Sea basin is located along the left-lateral transform boundary between the
Arabian and Sinai plates. Its structure and history are known from surface geology, drilling …

The temporal distribution of earthquakes in the Dead Sea Graben is studied through a
50,000‐year paleoseismic record recovered in laminated sediments of the Late Pleistocene …

The specialist contributors to Geomorphological Techniques have thoroughly augmented
and updated their original, authoritative coverage with critical evaluations of major recent …

A Catalogue of macroseismic observations of earthquakes in and near Israel and their
effects has been revised and updated to 1994. Data on some events have been extended …

A high-resolution Holocene seismic history of the Dead Sea Transform (DST) is established
from laminated sedimentary cores recovered at the shores of the Dead Sea. Radiocarbon …

We have measured the orientations of small faults, slickensides, tectonic stylolites, vein with
secondary mineralization, small folds and dikes in Israel and Sinai. These structures are …

We define the Sinai subplate, from a seismotectonic perspective, as a distinct component in
the plate tectonics of the eastern Mediterranean region. This is based on the tectonic …

Earthquake-induced fluidizations and suspensions of lake sediments, associated with
syndepositional faults, form a paleoseismic record in the Dead Sea graben. The association …