Silur: Difference between revisions
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== 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.
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]].
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