Pangaea Ultima

Pangaea Ultima
A rough approximation of Pangaea Ultima

Pangaea Ultima (also called Pangaea Proxima, Neopangaea, and Pangaea II) is a possible future supercontinent configuration and an alternative to the Amasia supercontinent. Consistent with the supercontinent cycle, Pangaea Ultima could occur within the next 250 million years. This potential configuration, hypothesized by Christopher Scotese, earned its name from its similarity to the previous Pangaea supercontinent. The concept was based on examination of past cycles of formation and breakup of supercontinents, not on current understanding of the mechanisms of tectonic change, which are too imprecise to project that far in the future. "It's all pretty much fantasy to start with", Scotese has said. "But it's a fun exercise to think about what might happen. And you can only do it if you have a really clear idea of why things happen in the first place."[1]

Supercontinents describe the merger of all, or nearly all, of the Earth's landmass into a single contiguous continent. In the Pangaea Ultima scenario, subduction at the western Atlantic, east of the Americas, leads to the subduction of the Atlantic mid-ocean ridge followed by subduction destroying the Atlantic oceanic basin, causing the Atlantic Ocean to close, bringing the Americas back together with Africa and Europe. As with most supercontinents, the interior of Pangaea Proxima would probably become a semi-arid desert prone to temperature extremes.[2]

Formation

According to the Pangaea Ultima hypothesis, the Atlantic and Indian Oceans will continue to get wider until new subduction zones bring the continents back together, forming a future Pangaea. Most continents and microcontinents are predicted to collide with Eurasia, just as they did when most continents collided to Laurentia.[3]

Around 50 million years from now, North America is predicted to have shifted slightly west and Eurasia would shift to the east, and possibly even to the south, bringing Great Britain closer to the North Pole and Siberia southward towards warm, subtropical latitudes. Africa is predicted to collide with Europe and Arabia, closing the Mediterranean Sea (completely closing the Tethys Ocean (or Neotethys) and the Red Sea). A long mountain range would then extend from Iberia, across Southern Europe (the Mediterranean Mountain Range), through the Mideast and into Asia. Some are even predicted to have peaks higher than Mt. Everest. Similarly, Australia is predicted to beach itself on the doorstep of Southeast Asia and a new subduction zone is predicted to encircle Australia and extend westward across the Central Indian Ocean. Meanwhile, Southern California and Baja California are predicted to have already collided with Alaska with new mountain ranges formed between them.[4]

About 150 million years from now, the Atlantic ocean is predicted to stop widening and begin to shrink because a bit of the Atlantic Ocean mid-ridge will have been subducted. In this scenario, a mid-ocean ridge between South America and Africa will probably be subducted first, the Atlantic Ocean is predicted to have narrowed as a result of subduction beneath the Americas. The Indian Ocean is also predicted to be smaller due to northward subduction of oceanic crust into the Central Indian trench. North and South America may be pushed back southeast, and southern Africa would almost hit equator and have reached the Northern hemisphere. Australia may join back to Antarctica, meeting the South Pole.[5]

When the last bit of the Mid-Atlantic spreading ridge is subducted beneath the Americas, the Atlantic Ocean is predicted to rapidly close with a new Pangaea forming.[6]

At 250 million years in the future, the Atlantic and Indian oceans are predicted to have closed. North America is predicted to have already collided with Africa, but be in a more southerly position than where it rifted. South America is predicted to be wrapped around the southern tip of Africa, with Patagonia in contact with Indonesia, enclosing a remnant of the Indian Ocean (called the Indo-Atlantic Ocean). Antarctica would then once again be at the South Pole and the Pacific will have grown wider, encircling half the Earth.[6]

Other theories

Amasia, Novopangea, and Pangaea Ultima are discussed in the book Supercontinent by Ted Nield, and illustrated in "Pangaea, the comeback" in the New Scientist magazine issued 20 October 2007.[7]

References


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  • Pangaea — Pangaea, Pangæa or Pangea (IPAEng|pænˈdʒiːə [OED] , from παν, pan , meaning entire , and Γαῖα, Gaea , meaning Earth in Ancient Greek) was the supercontinent that existed during the Paleozoic and Mesozoic eras about 250 million years ago, before… …   Wikipedia

  • Pangea Última — Representación aproximada de Pangea Última. Se le denomina Pangea Última, Neopangea o Pangea II al hipotético supercontinente sugerido por Christopher Scotese, que se formará dentro de 250 millones de años, de acuerdo a la teoría de la deriva… …   Wikipedia Español

  • Laurentia — For the use of the surname Laurentia , see Laurentum. Laurentia, also called the North American craton. Laurentia (North American craton) is a large area of continental craton, which forms the ancient geological core of the North American… …   Wikipedia

  • Christopher Scotese — Christopher R. Scotese Born 4 May 1953 Chicago, IL Residence USA Fields …   Wikipedia

  • Erdverschiebung — Die Theorie der Kontinentaldrift, auch Kontinentalverschiebung genannt, beschreibt die langsame Bewegung, Vereinigung und Aufspaltung von Kontinenten. Das Entstehen der Theorie führte im 18. und 19.Jahrhundert zu einer allmählichen Abkehr vom… …   Deutsch Wikipedia

  • Kontinentalverschiebung — Die Theorie der Kontinentaldrift, auch Kontinentalverschiebung genannt, beschreibt die langsame Bewegung, Vereinigung und Aufspaltung von Kontinenten. Das Entstehen der Theorie führte im 18. und 19.Jahrhundert zu einer allmählichen Abkehr vom… …   Deutsch Wikipedia

  • Siberia (continent) — Siberia is the craton located in the heart of the region of Siberia. Siberia or Angaraland (or simply Angara) is today the Central Siberian Plateau. It is an extremely ancient craton that formed an independent continent before the Permian Partial …   Wikipedia

  • Kontinentaldrift — Die Theorie der Kontinentaldrift, auch Kontinentalverschiebung genannt, beschreibt die langsame Bewegung, Aufspaltung und Vereinigung von Kontinenten. Erste Hypothesen zur Kontinentaldrift führten im 18. und 19.Jahrhundert zu einer allmählichen… …   Deutsch Wikipedia

  • Euramerica — (also known as Laurussia, the Old Red Continent or the Old Red Sandstone Continent) was a minor supercontinent created in the Devonian as the result of a collision between the Laurentian, Baltica, and Avalonia cratons (Caledonian orogeny). 300… …   Wikipedia

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