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About 25million years ago, due to a combination of high sea levels in the Mediterranean Sea and seismic activity in the region, a link formed between the Mediterranean Ocean and the northern tip of the Afro-Asian Rift valley. The link was formed close to the modern city of Haifa and resulted in the inundation of what is now known as the Jordan River basin. Subsequent seismic activity resulted in the closure of the link which left behind a large lake over 200km long from north to south and around 30km wide which geologists call Lake Lisan. The level of Lake Lisan has fluctuate greatly over its lifetime but has fallen steadily in the last 25,000 years or so and the salinity has changed significantly during that time. The remaining remnants of Lake Lisan are the Sea of Galillee and the Dead Sea.

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14y ago

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