Supercontinent oor Noorse Bokmål
Supercontinent
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Superkontinent
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supercontinent
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A very large continent that split into smaller ones in the Earth’s geologic past.
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superkontinent
en
very large continent in the Earth's past
In a typical reconstruction of the supposed ancient supercontinent, the southeastern coast of North America lies against the northwest coast of Africa.
I en typisk rekonstruksjon av et antatt forhistorisk superkontinent ligger sørøstkysten av Nord-Amerika mot Afrikas nordvestkyst.
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Geologic evidence points to a "megamonsoonal" circulation pattern during the time of the supercontinent Pangaea, and climate modeling suggests that the existence of the supercontinent was conducive to the establishment of monsoons.
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After breakup from Gondwana (the southern part of the supercontinent Pangea), the Antarctic plate began moving the continent of Antarctica south to its present isolated location causing the continent to develop a much colder climate.
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Around 2.1 to 1.84 Ga, when Kenorland shattered, the Arctican craton was part of the minor supercontinent Nena along with Baltica and Eastern Antarctica.
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The Old Red Sandstone Continent became a part of the supercontinent Pangaea in the Permian (299–252 Ma), during which proto-Britain continued to drift northwards.
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In a typical reconstruction of the supposed ancient supercontinent, the southeastern coast of North America lies against the northwest coast of Africa.
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A larger supercontinent will therefore have more area in which climate is strongly seasonal than will several smaller continents or islands.
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Australia and New Guinea are portions of the ancient supercontinent of Gondwana, which started to break into smaller continents in the Cretaceous era, 65–130 million years ago.
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Around 600 Ma, Laurentia was part of the major supercontinent Pannotia.
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The supercontinent Rodinia is thought to have formed about 1 billion years ago and to have embodied most or all of Earth's continents, and broken up into eight continents around 600 million years ago.
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The northern supercontinent of Laurasia began to break up, as Europe, Greenland and North America drifted apart.
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420 million years ago) the Iapetus Ocean had completely disappeared and the combined mass of the three continents formed the "new" continent of Laurasia, which would itself be the northern component of the singular supercontinent of Pangaea.
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Geologic evidence indicates that they were formed during the break-up of the supercontinent of Gondwana some 150 million years ago.
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The eight continents later re-assembled into another supercontinent called Pangaea; Pangaea broke up into Laurasia (which became North America and Eurasia) and Gondwana (which became the remaining continents).
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A larger supercontinent will therefore have more area in which climate is strongly seasonal than will several smaller continents or islands. Human influences
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The movement of plates has caused the formation and break-up of continents over time, including occasional formation of a supercontinent that contains most or all of the continents.
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The famously large island has yet to fully cleave itself tectonically from India and Africa, still crammed together with the rest of the southern supercontinent of Gondwana.
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During the first part of the middle period, from the Middle Devonian to the Eocene, all the continents were assembled into a single large landmass – the supercontinent Pangea (from the Greek word meaning “all earth”).
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Although the supercontinent was primarily experiencing compression as a result of the plate collisions during this period, eastern Greenland and Scandinavia were locally subject to crustal extension.
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An example of a supercontinent is Pangaea, formed around 300 million years ago.
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A larger supercontinent will therefore have more area in which climate is strongly seasonal than will several smaller continents or islands. Other mechanisms
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Thus emerged the original supercontinent that Wegener in his hypothesis assumed must have existed, and which he named Pangeae.
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Around 250 Ma from now, all continents may crash together, forming the major supercontinent Pangaea Ultima.
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Differences in fossil faunas on both sides of the red line (the Iapetus Suture) are evidence for the existence of an ocean between the two sides in the time before the continents were joined in the supercontinent Pangaea.
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The East Antarctic Craton is an ancient craton that forms most of Antarctica. The East Antarctic Craton was part of the supercontinent Nena 1.8 billion years ago.
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These studies show that the Earth's plates have moved around over millions of years, colliding together and breaking apart, and sometimes forming supercontinents in which most plates have joined together into a single continent.
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