The Tethys Ocean (/ˈtiːθɪs, ˈtɛ-/ TEETH-iss, TETH-; Greek: Τηθύς Tēthús), also called the Tethys Sea or the Neo-Tethys, was a prehistoric ocean during...

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...

and surrounded by the superocean Panthalassa and the Paleo-Tethys and subsequent Tethys Oceans. Pangaea is the most recent supercontinent to have existed...

Proto-Tethys or Theic Ocean was an ancient ocean that existed from the latest Ediacaran to the Carboniferous (550–330 Ma). The name "Proto-Tethys" has...

Look up Tethys in Wiktionary, the free dictionary. Tethys or Tethis may refer to: Tethys (database), an online knowledge management system about the environmental...

when the northern region of the Tethys Ocean (Peri-Tethys) was separated from the Mediterranean region of the Tethys realm due to the formation of the...

forces in the Paleo-Tethys that detached Cimmeria from Gondwana and opened the Neo-Tethys. The mid-ocean ridge in the Paleo-Tethys subducted under Eurasia...

have been caused by fragments from the sunken floor of the much older Tethys Ocean in the narrowing gap between India and Central Asia, as the sinking fragments...

In Greek mythology, Tethys (/ˈtiːθɪs, ˈtɛ-/; Ancient Greek: Τηθύς, romanized: Tēthýs) was a Titan daughter of Uranus and Gaia, a sister and wife of the...

135–125 Ma and as the Tethys Ocean north of India began to close 118–84 Ma the Indian Ocean opened behind it. The Indian Ocean, together with the Mediterranean...

Giovanni Domenico Cassini in 1684, and is named after the titan Tethys of Greek mythology. Tethys has a low density of 0.98 g/cm3, the lowest of all the major...

Hemisphere and Gondwana in the Southern Hemisphere, separated by the Tethys Ocean. "Laurussia" was defined by Swiss geologist Peter Ziegler in 1988 as...

Tethys Trench formed when the Cimmerian Plate was subducting under eastern Laurasia, around 200 million years ago, in the Early Jurassic. The Tethys Trench...

either Peri-Gondwana or core Gondwana; the Rheic Ocean closed in front of it and the Palaeo-Tethys Ocean opened behind it. Precambrian rocks from the Iberian...

Mesoproterozoic Pontus Ocean, the western part of the early Mesozoic Panthalassa Ocean Proto-Tethys Ocean, Neoproterozoic Rheic Ocean, the Paleozoic ocean between Gondwana...

separated from the southern continent by an oceanic basin: the Paleo-Tethys. Although the western Paleo-Tethys Ocean had existed since the Cambrian, the eastern...

European shores of the former Tethys Ocean and has, if so, maintained itself by vegetative growth, floating in the ocean for millions of years. Other species...

isolated landmass as the Indian Plate drifted across the Tethys Ocean, forming the Indian Ocean. The process of India's separation from Madagascar first...

Paleo-Tethys Ocean – Ocean on the margin of Gondwana between the Middle Cambrian and Late Triassic Pan-African Ocean – Hypothesized paleo-ocean whose...

of the Tethys Ocean. Together with some other oceanic basins that existed between the continents Europe and Africa, the Piemont-Liguria Ocean is called...

world's largest lake, but it is centered on an oceanic basin (a fragment of the ancient Tethys Ocean) rather than lying entirely over continental crust...

(the "universal ocean") covered the rest of the planet. Other minor oceans were Paleo-Tethys, Proto-Tethys, Rheic Ocean and Ural Ocean (which was closed...

geographical features, the supercontinent Gondwana (proposed in 1861) and the Tethys Ocean. Eduard Suess was born on 20 August 1831 in London, England, the oldest...

The Monte Bolca formation is thought to represent a shallow sea of the Tethys Ocean with scattered coral reefs and seagrass beds. With its combination of...

older Tethys Ocean, at about 270 and up to 340 million years old. The oceanic crust displays a pattern of magnetic lines, parallel to the ocean ridges...

a region of Italy Piemont-Liguria Ocean, a former piece of oceanic crust that is seen as part of the Tethys Ocean Nicolaas Piemont(1644–1709), Dutch...

the Panthalassa–Tethys boundary is poorly known because little oceanic crust is preserved—both the Izanagi and the conjugate Pacific Ocean floor is subducted...

belt is the result of Mesozoic-to-Cenozoic-to-recent closure of the Tethys Ocean and process of collision between the northward-moving African, Arabian...

superterrane, which divided the Tethys Ocean realm into the Paleo-Tethys Ocean and the slowly expanding Neotethys Ocean. The Lopingian ended with the Permian–Triassic...

Basin to the south-west, the Paratethys Sea to the south-east, or the Tethys Ocean to the south. During the Late Cretaceous, about 85 million years ago...