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Laurasia (/ l ɔː ˈ r eɪ ʒ ə,-ʃ i ə /) [1] was the more northern of two large landmasses that formed part of the Pangaea supercontinent from around , the other being Gondwana. It separated from Gondwana 215 to 175 Mya (beginning in the late Triassic period) during the breakup of Pangaea, drifting farther north after the split and finally ...
Gondwana (/ ɡ ɒ n d ˈ w ɑː n ə /) [1] was a large landmass, sometimes referred to as a supercontinent.The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, Australia, Zealandia, Arabia, and the Indian Subcontinent.
The following other wikis use this file: Usage on af.wikipedia.org Tetisoseaan; Usage on be-tarask.wikipedia.org Гандвана; Usage on be.wikipedia.org
In the Jurassic, Pangaea split into Laurasia and Gondwana, with Avalonia as part of Laurasia. [15] In the Cretaceous, Laurasia broke up into North America and Eurasia with Avalonia split between them. [16] Iberia was later rotated away again as the African part of Gondwana strike-slipped past it.
Ontario Parks and protected areas statistics Type Number Area % land area Hectares Acres Provincial parks 341 8,278,063 20,455,540 7.69% Conservation reserves 295 1,514,147 3,741,540 1.4% Protected areas 9 1,226,016 3,029,550 1.1% Wilderness areas 28 2,590 6,400 <0.1% Total 662 11,020,284 27,231,710 10.29%
Ontario is known for the large number of lakes and rivers it contains. About one-fifth of the world's fresh water can be found in Ontario. [17] Ontario is also known for being the only province in Canada that touches the Great Lakes. Ontario touches four of the Great Lakes: Huron, Lake Ontario (the province is named after the lake), Erie and ...
First phase of the Tethys Ocean's forming: the (first) Tethys Sea starts dividing Pangaea into two supercontinents, Laurasia and Gondwana.. The Tethys Ocean (/ ˈ t iː θ ɪ s, ˈ t ɛ-/ TEETH-iss, TETH-; Greek: Τηθύς Tēthús), also called the Tethys Sea or the Neo-Tethys, was a prehistoric ocean during much of the Mesozoic Era and early-mid Cenozoic Era.
Laurentia basement rocks. Laurentia or the North American Craton is a large continental craton that forms the ancient geological core of North America.Many times in its past, Laurentia has been a separate continent, as it is now in the form of North America, although originally it also included the cratonic areas of Greenland and the Hebridean Terrane in northwest Scotland.
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