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== Vönataledav lordovigik ==
Melanivods äbinons löpiks dü Lordovig; efe dü period: ''Tremadocia'', löpikam melanivoda su vol lölik äbinon gretikün, dö kel klülabots pekipedons in klifs.
Sea levels were high during the Ordovician; in fact during the Tremadocian, [[Transgression (geology)|marine transgressions]] worldwide were the greatest for which evidence is preserved in the rocks.
Dü Lordovig, kontinäns sulüdik äkobikons ad kontinän bal [[Gondwanop]] panemöl. Gondwanop äprimon periodi lä kveator e, du period äfovon, äsveamon lüodü Sulüdapov. Prim Lordoviga palecedon as vamik, pu lä trops. Soäs Nolüda-Merop e Yurop, Gondwanop ün Lordovig pätegon gretadilo fa mels nedibik. Vats nedibik kleilik ägönons glofi jäfidämemas, kels pladons kalsinkarbatis ini jals e dils düfik oksik. Sean: ''[[Panthalassia]]'' ätegon cifadili lafasfera nolüdik; seans smalikum äbinons els ''[[Proto-Tethys]]'', ''[[Paleo-Tethys]]'', ''[[Khanty]]'' (kel päfärmükon ed änepubon finü Lordovig), ''[[Iapetus]]'', e sean nulik: ''[[Rheik]]''.
Dü Lordovig, kontinäns sulüdik pakonletons ad kontinän bal [[Gondwanop]] panemöl.
During the Ordovician, the southern continents were collected into a single continent called [[Gondwana]]. Gondwana started the period in [[equator]]ial [[latitude]]s and, as the period progressed, drifted toward the [[South Pole]]. The Early Ordovician was thought to be quite warm, at least in the tropics. As with North America and [[Europe]], Gondwana was largely covered with shallow seas during the Ordovician. Shallow clear waters over continental shelves encouraged the growth of organisms that deposit calcium carbonates in their shells and hard parts. [[Panthalassic Ocean]] covered much of the northern hemisphere, and other minor oceans included [[Proto-Tethys]], [[Paleo-Tethys]], [[Khanty Ocean]] which was closed off by the Late Ordovician, [[Iapetus Ocean]], and the new [[Rheic Ocean]].
Klifs lordovigik binons ledino sädots. Sekü sürfat e löp smaliks fimäna, kels ämiedükons lerodi, sädots melik, kels fomons dili gretik sita lordovigik, binädons cifadilo me zemaston. Slet e sabaston binons läs tuvabiks.
Klifs lordovigik binons ledino sädots.
Ordovician rocks are chiefly [[sedimentary]]. Because of the restricted area and low elevation of solid land, which set limits to [[erosion]], marine [[sediment]]s that make up a large part of the Ordovician system consist chiefly of [[limestone]]. [[Shale]] and [[sandstone]] are less conspicuous.
Jenet veütik äbinon beladaveda Takonik (ma els Taconic Mountinas in Nolüda-Melop), kel iprimon ya dü [[Kambrium]].
A major mountain-building episode was the [[Taconic orogeny]] that was well under way in Cambrian times.
Finü period at, Gondwanop inilikon pov e cifadilo igladädikon.
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