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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 ...
Nowadays the Jordan Valley still is an essential part of one of the main migration routes for birds in the world; within the region, it constitutes the Eastern Route which, together with the parallel Western Route and the Southern-Eilat Mountains Route, allow an estimated 500 million birds belonging 200 species to fly across Israel twice a year ...
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).
The old meaning, which was in use up to around the early 20th century, covered almost the entire length of what today is called the Jordan Rift Valley, running in a north–south orientation between the southern end of the Sea of Galilee and the northern tip of the Gulf of Aqaba of the Red Sea at Aqaba–Eilat.
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.
Its type-site, Teleilat Ghassul (Teleilat el-Ghassul, Tulaylat al-Ghassul), is located in the eastern Jordan Valley near the northern edge of the Dead Sea, in modern Jordan. It was excavated in 1929-1938 and in 1959–1960, by the Jesuits. [2] [3] [4] Basil Hennessy dug at the site in 1967 and in 1975–1977, and Stephen Bourke in 1994–1999 ...
Wadi as-Sir (approximate phonetic transcription Wâdī es-Sîr) is a valley descending along the eastern slopes of the Jordan Rift Valley westwards towards the Jordan River. Qasr al-Abd, a Hellenistic palace at Iraq el-Amir. The valley offers access to the impressive Hellenistic-period ruins of Iraq el-Amir. [4]