The Jordan Rift Valley, also Jordan Valley ( he|בִּקְעָת הַיַרְדֵּן Bik'at HaYarden, ar|الغور Al-Ghor or Al-Ghawr), also called the Syro-African Depression, is an elongated depression
located in modern-day Israel
, and Palestine
. This geographic region includes the entire length of the Jordan River
– from its sources, through the Hula Valley
, the Korazim block, the Sea of Galilee
, the (Lower) Jordan Valley
, all the way to the Dead Sea
, the lowest land elevation on Earth – and then continues through the Arabah
depression, the Gulf of Aqaba
whose shorelines it incorporates, until finally reaching the Red Sea
proper at the Straits of Tiran
History and physical features
The Jordan Rift Valley was formed many millions of years ago in the Miocene
epoch (23.8 – 5.3 Myr ago) when the Arabian Plate
moved northward and then eastward away from Africa. One million years later, the land between the Mediterranean
and the Jordan Rift Valley rose so that the sea water stopped flooding the area.
The geological and environmental evolution of the valley since its inception in the Oligocene
can be seen in a variety of sedimentary and magmatic rock units, preserved as continuous sequences in the deeper basins. The outcropping formations around the basins represent alternating deposition and erosion phases.
The lowest point in the Jordan Rift Valley is in the Dead Sea, the lowest spot of which is below sea level. The shore of the Dead Sea is the lowest land on earth, at below sea level. Rising sharply to almost in the west, and similarly in the east, the rift is a significant topographic feature over which a few narrow paved roads and difficult mountain tracks lead.
The valley north of the Dead Sea has long been a site of agriculture because of water available from the Jordan River and numerous springs located on the valley's flanks.
Dead Sea Transform
The plate boundary which extends through the valley is variously called the Dead Sea Transform
(DST) or Dead Sea Rift. The boundary separates the Arabian Plate from the African Plate
, connecting the divergent plate boundary in the Red Sea
(the Red Sea Rift
) to the East Anatolian Fault
.The Geophysical Institute
The DST fault system is generally considered to be a transform fault that has accommodated a northwards displacement of the Arabian Plate.
This interpretation is based on observation of offset markers, such as river terraces, gullies and archaeological features, giving horizontal slip rates of several mm per year over the last few million years. GPS data give similar rates of present-day movement of the Arabian Plate relative to the Africa Plate. It has also been proposed that the fault zone is a rift system that is an incipient oceanic spreading center, the northern extension of the Red Sea Rift.
* Geography of Israel
* Geography of Jordan
* Great Rift Valley
Category:Valleys of Asia
Category:Landforms of the Middle East
Category:Cenozoic geology of Asia
Category:Cenozoic rifts and grabens
Category:Geography of Palestine (region)
Category:Landforms of Jordan
Category:Valleys of the State of Palestine
Category:Valleys of the West Bank
Category:Landforms of Western Asia
Category:Regions of Israel
Category:Rifts and grabens
Category:Valleys of Israel
Category:Depressions of Israel
Category:Depressions of Jordan