Laurasiyop: Difference between revisions
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[[Image:Laurasiyop-Gondvanop.PNG|right|thumb|300px]]
'''Laurasiyop''' äbinon [[lekontinän]], kel brefabüiküno ädabinon as
==
Dö Laurasiyop sevädon as pubod mesozoigik, atimo cedoy, das kontinäns „ot“, kels äfomons Laurasiyopi, leigo idabinons as lekontinän pos slitam [[Rodiniyop]]a bü yels za 1 000-balions; ad vitön kofudi ko lekontinän Mesozoigik, panemon „[[Rulaurasiyop]]“ („''Proto-Laurasia''“). Pakredos, das Rulaurasiyop no ädönusliton bü iyumon ad kontinäns sulüdik, ko kels ifomon lekontinäni bü-Kambriumik: [[Pannotiyop]], kel äbleibon dabinön jü prim [[Kambrium]]a.
== Slitam e Dönufomam ==
Dü Kambrium, Laurasiyop äblibon cifadilo in topäds kveatorik. Pos tim at äprimon ad slitön: Nolüda-Tsyinän e [[Siberiyop]] äsveamons
nolüdio (ärivons topädis nolüdikum, ka uts, kö dü yels büik 500-balion kontinäns ädabinons). Dü [[Devon]], Nolüda-Tsyinän ätopon nilü [[Larktikän]], kö äblibon dü [[gladatimäd]] [[Karbon]]a, bü yels vü 300- e 280-balions. No dabinons ye klülabots tefü
During the Cambrian, Laurasia was largely located in equatorial latitudes and began to break up, with [[North China (continent)|North China]] and [[Siberia (continent)|Siberia]] drifting into latitudes further north than those occupied by continents during the previous 500 million years. By the [[Devonian]], North China was located near the [[Arctic Circle]] and it remained the northernmost land in the world during the [[Carboniferous]] [[Ice Age]] between 300 and 280 million years ago. There is no evidence, though, for any large scale Carbonifeous [[glaciation]] of the northern continents. This cold period saw the re-joining of Laurentia and Baltica with the formation of the [[Appalachian Mountains]] and the vast [[coal]] deposits which are today a mainstay of the economy of such regions as [[West Virginia]] and parts of the [[British Isles]] and [[Germany]].
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