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Lien 35: == Vönataledav silurik == Timü Silur, [[Gondwanop]] äfövon sveami nevifik sulüdio, lüodü pov sulüdik, ab dabinons klülabots, bai kels gladajüds silurik äbinons läs stääniks ka uts gladatimäda löpa-lordovigik. Smetam gladajüdas e glademas äkodon löpikami melanivoda, kelos klülädon se jenöfot, das sadots silurik seatons sus sadots lordovigik pevorüköl, gü sökaleod timavik. Kontinänadils votik äsveamons kobio nilü kveator, kö äprimons fomami lekontinäna nulik: „[[Yuramerop]]“. Kobojok ru-Yuropa e Nolüda-Meropa äplifon sedotis jolik, kela kumam iprimon ya dü [[Kambrium]], lä jol lofüdik Nolüda-Meropa e lä jol vesüdik Yuropa. Jenot at binon sevädik as [[belidavedükam di Calledonia]], kel äposbinükon belemis de tat: New York love Yurop e Gröneän jü Norgän. Finü Silur, melanivods dönu ädonikons, äposbinükölo sedotis tefik de tat: Michigan jü tat: West Virginia, e belems nulik tefädiko vifiko pävorükons fa viens. Flumed: [[Teays]], kel äflumon ini mel zänoda-kontinänik, ävorükon nevifiko sedotis lordovigik, kelos äposbinükon retodis in sadotem silurik in Ohio ed Indiana. During the Silurian, [[Gondwana]] continued a slow southward drift to high southern latitudes, but there is evidence that the Silurian icecaps were less extensive than those of the late Ordovician glaciation. The melting of icecaps and [[glacier]]s contributed to a rise in sea level, recognizable from the fact that Silurian sediments overlie eroded Ordovician sediments, forming an [[unconformity]]. Other [[craton]]s and continent fragments [[Continental Drift\|drifted]] together near the [[equator]], starting the formation of a second [[supercontinent]] known as [[Euramerica]]. When the proto-Europe collided with North America, the collision folded coastal sediments that had been accumulating since the Cambrian off the east coast of North America and the west coast of Europe. This event is the [[Caledonian orogeny]], a spate of mountain building that stretched from New York State through conjoined Europe and Greenland to Norway. At the end of the Silurian, sea levels dropped again, leaving telltale basins of [[evaporite]]s in a basin extending from Michigan to West Virginia, and the new mountain ranges were rapidly eroded. The [[Teays River]], flowing into the shallow mid-continental sea, eroded Ordovician strata, leaving traces in the Silurian strata of northern Ohio and Indiana. Sean legretik: ''[[Panthalassa]]'' ätegon cifadili lafasfera nolüdik. Seans smalikum votik binons: ''[[Proto-Tethys]]'', ''[[Paleo-Tethys]]'', ''[[Sean Rheik]], melaveg ''[[Seana di Iapetus]]'' (nu vü ''[[Avalonia]]'' e ''[[Laurentia]]''), e ''[[Sean di Ural]]'' nulik.

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