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Paratethys and Tethys Ocean

Shortcuts: Differences, Similarities, Jaccard Similarity Coefficient, References.

Difference between Paratethys and Tethys Ocean

Paratethys vs. Tethys Ocean

The Paratethys sea, Paratethys ocean, Paratethys realm or just Paratethys was a large shallow inland sea that stretched from the region north of the Alps over Central Europe to the Aral Sea in Central Asia. The Tethys Ocean (Τηθύς), also called the Tethys Sea or the Neo-Tethys, was a prehistoric ocean during much of the Mesozoic Era and early-mid Cenozoic Era.

Similarities between Paratethys and Tethys Ocean

Paratethys and Tethys Ocean have 25 things in common (in Unionpedia): Alborz, Alpine orogeny, Aral Sea, Atlantic Ocean, Black Sea, Carpathian Mountains, Caspian Sea, Cimmeria (continent), Cretaceous, Dinaric Alps, Gondwana, Indian Ocean, Inland sea, Jurassic, Laurasia, Mediterranean Sea, Miocene, Molasse basin, Oligocene, Paleo-Tethys Ocean, Pangaea, Pliocene, Taurus Mountains, Triassic, University of Lausanne.

Alborz

The Alborz (البرز) range, also spelled as Alburz, Elburz or Elborz, is a mountain range in northern Iran that stretches from the border of Azerbaijan along the western and entire southern coast of the Caspian Sea and finally runs northeast and merges into the smaller Aladagh Mountains and borders in the northeast on the parallel mountain ridge Kopet Dag in the northern parts of Khorasan.

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Alpine orogeny

The Alpine orogeny or Alpide orogeny is an orogenic phase in the Late Mesozoic (Eoalpine) and the current Cenozoic that has formed the mountain ranges of the Alpide belt.

Alpine orogeny and Paratethys · Alpine orogeny and Tethys Ocean · See more »

Aral Sea

The Aral Sea was an endorheic lake (that is, without an outlet) lying between Kazakhstan to its north and Uzbekistan to its south, which began shrinking in the 1960s and largely dried up by the 2010s.

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Atlantic Ocean

The Atlantic Ocean is the second-largest of the world's five oceanic divisions, with an area of about.

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Black Sea

The Black Sea is a marginal mediterranean sea lying between Europe and Asia, east of the Balkans, south of the East European Plain, west of the Caucasus, and north of Anatolia.

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Carpathian Mountains

The Carpathian Mountains or Carpathians are a range of mountains forming an arc across Central Europe and Southeast Europe.

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Caspian Sea

The Caspian Sea is the world's largest inland body of water, often described as the world's largest lake and sometimes referred to as a full-fledged sea.

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Cimmeria (continent)

Cimmeria was an ancient continent, or, rather, a string of microcontinents or terranes, that rifted from Gondwana in the Southern Hemisphere and was accreted to Eurasia in the Northern Hemisphere.

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Cretaceous

The Cretaceous is a geological period that lasted from about 145 to 66 million years ago (Mya).

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Dinaric Alps

The Dinaric Alps, also Dinarides, are a mountain range in Southern and Southcentral Europe, separating the continental Balkan Peninsula from the Adriatic Sea.

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Gondwana

Gondwana was a large landmass, sometimes referred to as a supercontinent.

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Indian Ocean

The Indian Ocean is the third-largest of the world's five oceanic divisions, covering or approx.

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Inland sea

An inland sea (also known as an epeiric sea or an epicontinental sea) is a continental body of water which is very large in area and is either completely surrounded by dry land or connected to an ocean by a river, strait or "arm of the sea".

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Jurassic

The Jurassic is a geologic period and stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya.

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Laurasia

Laurasia was the more northern of two large landmasses that formed part of the Pangaea supercontinent from around (Mya), the other being Gondwana.

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Mediterranean Sea

The Mediterranean Sea is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean Basin and almost completely enclosed by land: on the north by Southern Europe and Anatolia, on the south by North Africa, on the east by the Levant in West Asia, and on the west almost by the Morocco–Spain border.

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Miocene

The Miocene is the first geological epoch of the Neogene Period and extends from about (Ma).

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Molasse basin

The Molasse basin (or North Alpine foreland basin) is a foreland basin north of the Alps which formed during the Oligocene and Miocene epochs.

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Oligocene

The Oligocene is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present (to). As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain.

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Paleo-Tethys Ocean

The Paleo-Tethys or Palaeo-Tethys Ocean was an ocean located along the northern margin of the paleocontinent Gondwana that started to open during the Middle Cambrian, grew throughout the Paleozoic, and finally closed during the Late Triassic; existing for about 400 million years.

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Pangaea

Pangaea or Pangea was a supercontinent that existed during the late Paleozoic and early Mesozoic eras.

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Pliocene

The Pliocene (also Pleiocene) is the epoch in the geologic time scale that extends from 5.333 million to 2.58 million years ago.

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Taurus Mountains

The Taurus Mountains (Turkish: Toros Dağları or Toroslar, Greek: Ταύρος) are a mountain complex in southern Turkey, separating the Mediterranean coastal region from the central Anatolian Plateau.

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Triassic

The Triassic (sometimes symbolized 🝈) is a geologic period and system which spans 50.5 million years from the end of the Permian Period 251.902 million years ago (Mya), to the beginning of the Jurassic Period 201.4 Mya.

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University of Lausanne

The University of Lausanne (UNIL; Université de Lausanne) in Lausanne, Switzerland was founded in 1537 as a school of Protestant theology, before being made a university in 1890.

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The list above answers the following questions

Paratethys and Tethys Ocean Comparison

Paratethys has 89 relations, while Tethys Ocean has 94. As they have in common 25, the Jaccard index is 13.66% = 25 / (89 + 94).

References

This article shows the relationship between Paratethys and Tethys Ocean. To access each article from which the information was extracted, please visit: