Paleoearthquake features as indicators of potential earthquake activities in the Karameh dam site

摘要

Prehistorical earthquake induced features, such as faults, folds, fissures, and slumps have been discovered during the Karameh dam construction. The dam is located close to the plate tectonics boundary formed by the active Jordan Valley Fault. Of most importance are those known as the foldtype deformations "decollement type of structure" which are well preserved in the laminated Lisan formations. These features show that historical moderate to strongly sized earthquake activities are likely to have been originated in the vicinity of the dam site. Such features may well provide valuable information for identification of areas of highly strong earthquake regions.