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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. Alternatively, it was a ...
'Ubeidiya (Arabic: العبيدية, romanized: `Ubaydiyya; Hebrew: עובידיה), some 3 km south of the Sea of Galilee, in the Jordan Rift Valley, Israel, is an archaeological site of the early Pleistocene, [1] c. 1.5 million years ago, preserving traces of one of the earliest migrations of Homo erectus out of Africa, with (as of 2014) only ...
The Upper Jordan Valley comprises the Jordan River sources and the course of the Jordan River through the Hula Valley and the Korazim Plateau, both north of the Sea of Galilee. The lower part of the valley, known as the Ghor (from the Arabic Ghawr or Ghōr , غور ), includes the Jordan River segment south of the Sea of Galilee which ends at ...
The Israel–Jordan Peace Treaty was signed in the Arava on October 26, 1994. The governments of Jordan and Israel are promoting development of the region. There is a plan to bring sea water from the Red Sea to the Dead Sea through a canal (Red–Dead Seas Canal), which follows along the Arabah. This (long envisioned) project was once an issue ...
The main culture of the Chalcolithic period in Israel is the Ghassulian culture, named after the name of its type-site, Teleilat el-Ghassul, located in the eastern part of the Jordan Rift Valley, opposite Jericho. Afterwards, many additional settlements, located in other archaeological sites, were identified as Ghassulian settlements.
Ohalo II is the name given to the archaeological site located on the southwest shore of the Sea of Galilee in the Levant Jordan Rift Valley. [3] The site consists of the remains of six charcoal rings where brushwood dwellings had been during the Upper Paleolithic. [4] [5] The huts are oval in shape and average between 9 and 16 feet long. They ...
An earthquake struck the Jordan Rift Valley on December 5, AD 1033 and caused extreme devastation in the Levant region. It was part of a sequence of four strong earthquakes in the region between 1033 and 1035. Scholars have estimated the moment magnitude to be greater than 7.0 M w and evaluated the Modified Mercalli intensity to X (Extreme).
Lake Lisan was a prehistoric lake that existed between 70,000 and 12,000 BP in the Jordan Rift Valley in the Near East. [1] It is sometimes referred to as a Pleistocene lake. Lisan means tongue in Arabic relating to the shape of the Lisan Peninsula where studies of the sediment formations were taken.