Search results
Results from the WOW.Com Content Network
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 ...
East of the Jordan River Valley, the land surface eroded to a nearly flat peneplain and many Proterozoic sediments were eroded. Before Cambrian sediments began to accumulate quartz porphyry lavas erupted to the surface. Tectonic conditions favored the preservation of Proterozoic sediments in the Wadi al'Arabah as Cambrian sandstones began to form.
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 ...
Jordan Rift Valley. East of the central highlands lies the Jordan Rift Valley, which is a small part of the 6,500 kilometers (4,039 mi)-long Syrian-East African Rift. [19] In Israel the Rift Valley is dominated by the Jordan River, the Sea of Galilee (an important freshwater source also known as Lake Tiberias and Lake Kinneret), and the Dead ...
The valley is part of the north-south Great Rift Valley, and its successive depressions are Lake Tiberias (Sea of Galilee; its bottom is about −258 metres (−846 ft)), Jordan Valley, the Dead Sea (its bottom is about −730 metres (−2,400 ft)), Arabah, and the Gulf of Aqaba at the Red Sea. Jordan's western border follows the bottom of the ...
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).
For premium support please call: 800-290-4726 more ways to reach us
Panorama of Jordan Valley. The Jordan valley segment of the DST, which is part of the Jordan Rift Valley, runs for about 100 km from the northwestern part of the Dead Sea to the southeastern part of the Sea of Galilee along the Jordan Valley. A slip rate of between 4.7 and 5.1 mm per year has been estimated over the last 47,500 years.