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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 ...
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 ...
'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 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.
The Zarqa River, the second main tributary of the Jordan River, flows and empties entirely within the East Bank. A 380-kilometer-long rift valley runs from the Yarmouk River in the north to Al Aqaba in the south. The northern part, from the Yarmouk River to the Dead Sea, is commonly known as the Jordan Valley.
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).
Map of the Great Rift Valley. The Great Rift Valley (Swahili: Bonde la ufa) is a series of contiguous geographic depressions, approximately 6,000 or 7,000 kilometres (4,300 mi) in total length, the definition varying between sources, that runs from the southern Turkish Hatay Province in Asia, through the Red Sea, to Mozambique in Southeast Africa.
They extend to south to Jordan's border with Saudi Arabia. From the plateau to the east the highlands appear as a series of hills. To the west the highlands drop steeply 1,000 meters or more to the Jordan Rift Valley, which contains the Jordan River and the Dead Sea, a saline lake with a surface below sea level. [1]