āĻ āĻ¨ā§āĻ¸āĻ¨ā§āĻ§āĻžāĻ¨ āĻāĻ°ā§āĻ¨
āĻ āĻāĻŋāĻ§āĻžāĻ¨ā§āĻ° āĻāĻžāĻˇāĻž āĻ¨āĻŋāĻ°ā§āĻŦāĻžāĻāĻ¨ āĻāĻ°ā§āĻ¨
āĻāĻĒāĻ¨āĻžāĻ° āĻāĻžāĻˇāĻž āĻ¨āĻŋāĻ°ā§āĻŦāĻžāĻāĻ¨ āĻāĻ°ā§āĻ¨
Pangea
01
āĻĒā§āĻ¯āĻžāĻ¨āĻāĻŋāĻ¯āĻŧāĻž, āĻĒā§āĻ¯āĻžāĻ¨āĻāĻŋāĻ¯āĻŧāĻž āĻŽāĻšāĻžāĻĻā§āĻļ
a supercontinent that existed during the late Paleozoic and early Mesozoic eras, comprising most of Earth's landmasses fused together before breaking apart into the continents we recognize today
āĻāĻĻāĻžāĻšāĻ°āĻŖ
The assembly of Pangaea resulted from the convergence and collision of several smaller landmasses.
āĻĒā§āĻ¯āĻžāĻ¨āĻāĻŋāĻ¯āĻŧāĻž-āĻāĻ° āĻ¸āĻŽāĻžāĻŦā§āĻļ āĻāĻ¯āĻŧā§āĻāĻāĻŋ āĻā§āĻ āĻā§āĻāĻŖā§āĻĄā§āĻ° āĻ
āĻāĻŋāĻ¸āĻ°āĻŖ āĻāĻŦāĻ āĻ¸āĻāĻāĻ°ā§āĻˇā§āĻ° āĻĢāĻ˛ā§ āĻāĻā§āĻāĻŋāĻ˛āĨ¤
āĻ¨āĻŋāĻāĻāĻŦāĻ°ā§āĻ¤ā§ āĻļāĻŦā§āĻĻ
