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The Tethys Sea's remnants are Gulf of Mexico, Mediterranean Sea, Black Sea, Caspian Sea, and Aral Sea.
It is a remnant of the ancient Tethys Ocean and became landlocked about 5 million years ago due to continental drift.
Firstly, the Caspian Sea is a remnant of the former Tethys Ocean. Secondly, the Caspian Sea is still an endorheic basin, meaning that there is no outlet, allowing the salt to accumulate.
The Tethys Sea gradually disappeared during the late Mesozoic and early Cenozoic eras, primarily due to the tectonic processes associated with the collision of the African and Eurasian tectonic plates. This process led to the closure of the Tethys Ocean and the uplift of mountain ranges, such as the Alps and the Himalayas. By the late Cretaceous to early Paleogene period, the remnants of the Tethys Sea had largely been transformed into smaller bodies of water, such as the Mediterranean Sea.
The Rock of Gibraltar, primarily composed of limestone, was formed around 200 million years ago during the Jurassic period as part of the Alpine orogeny. It emerged as a result of geological processes, including sedimentation and tectonic activity. The rock is a remnant of the ancient Tethys Sea and has undergone significant geological changes over millions of years. Today, it stands as a prominent landmark at the entrance to the Mediterranean Sea.
Closure of the eastern Tethys was the result of the northward migration of Africa and the collision of Arabia and Iran with Asia Minor the later producing the Tarus and Zagros Mountains. Today the African plate continues a squeeze of the Mediterranean with subduction beneath Italy and the Greek Islands. Eventually North Africa seems destined to collide with Europe in the final elimination of the Mediterranean.
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it has come from sea Tethys
The Mediterranean Sea.
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I am Tethys, the titaness and sea goddess who was the sister and wife of Oceanus. Together, we were the parents of river gods and the Oceanids.
Mediterranean Sea