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== 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 gladädam kontinänas nolüdik dü Karbon. Ün period koldik at, Laurentiyop e Baltikop äkobikons, kelos äfomon belemi: [[Appalachians]] ed i kolataleseatöps legretik, kels binons adelo stab konömavik topädas soäs tat Lamerikänik: [[West Virginia]], äsi dils [[Regän Pebalöl|Regäna Pebalöl]] e [[Deutän]]a.
Siberiyop ämufon sulüdio, ed äyümon oki ad Kazakstaniyop: topäd kontinänik smalik, dö kel tikoy atimo, das pijafon dü volkanam vemöfik [[Silur]]a. Ven kontinäns tel at äkobikons, Laurasiyop tio pädönufomon; primü [[Triat]], el ''craton'' Lofüda-Tsyinänik ya iyümon oki ad Laurasiyop pädönufomöl dü äkobojokon ko [[Gondvanop]] ad fomön [[Pangeyop]]i. Nolüda-Tsyinän äbinon, dü äsveamon sulüdio de topäds Larktik, kontinän lätik ad yümön oki ad Pangeyop.
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]].
Siberia moved southwards and joined with [[Kazakhstania]], a small continental region believed today to have been created during the Silurian by extensive volcanism. When these two continents joined together, Laurasia was nearly reformed, and by the beginning of the [[Triassic]], the East China craton had rejoined the redeveloping Laurasia as it collided with [[Gondwana]] to form [[Pangaea]]. North China became, as it drifted southwards from near-Arctic latitudes, the last continent to join with Pangaea.
== Slitam lätik ==
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