Open AccessActive tectonics along the Wadi Araba‐Jordan Valley transform fault
Author(s) -
Galli Paolo
Publication year - 1999
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/1998jb900013
Subject(s) - geology , wadi , fault (geology) , graben , seismology , transform fault , sinistral and dextral , tectonics , transtension , fault scarp , slip (aerodynamics) , active fault , geography , archaeology , physics , thermodynamics
A geological study has been carried out along the 200 km long Wadi Araba following the transform fault that separates the Arabian and Sinai‐African Plates. Recent movements along this structure affect upper Pleistocene‐Holocene deposits and archaeological sites. Kinematic indicators show sinistral strike‐slip and oblique movements, in agreement with the relative motion between the two plates. Other evidence of recent horizontal displacement exists along the Jordan Valley Fault, both on the Dead Sea‐Lake Tiberias segment and on the segment north of Lake Tiberias. A minimum horizontal slip rate of 1 cm yr −1 has been estimated for both the southern segment of the Wadi Araba Fault and for the southern Jordan River Fault. The two faults can be roughly subdivided into at least four segments: two in the Wadi Araba (80 km long each), one from the Dead Sea to Lake Tiberias (130 km), and one from Lake Tiberias to the Hula graben (>30 km). Faulting may also occur along shorter subsegments, as shown by bends in the Wadi Araba‐Jordan River Fault and by the growth of local compression and extension features. Instrument‐recorded seismicity appears to be mainly concentrated along some of these subsegments. A comparison between the observed seismic and field‐determined slip rates across the fault indicates possible strain accumulation during the last 2000 years.