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¨
mesozoic
/mËÉsÉzËÉĘÉĒk/
Mesozoic
01
āĻŽā§āĻ¸ā§āĻā§āĻ¯āĻŧāĻŋāĻ, āĻĻā§āĻŦāĻŋāĻ¤ā§āĻ¯āĻŧ āĻ¯ā§āĻ
the period of time from about 252 to 66 million years ago, characterized by the dominance of dinosaurs and the gradual breakup of the supercontinent Pangaea
āĻāĻĻāĻžāĻšāĻ°āĻŖ
Geologists rely on the rock formations of the Mesozoic to understand Earth's geological history and the shifting continents.
āĻā§āĻ¤āĻ¤ā§āĻ¤ā§āĻŦāĻŦāĻŋāĻĻāĻ°āĻž āĻĒā§āĻĨāĻŋāĻŦā§āĻ° āĻā§āĻ¤āĻžāĻ¤ā§āĻ¤ā§āĻŦāĻŋāĻ āĻāĻ¤āĻŋāĻšāĻžāĻ¸ āĻāĻŦāĻ āĻŽāĻšāĻžāĻĻā§āĻļāĻā§āĻ˛āĻŋāĻ° āĻ¸ā§āĻĨāĻžāĻ¨āĻžāĻ¨ā§āĻ¤āĻ° āĻŦā§āĻāĻžāĻ° āĻāĻ¨ā§āĻ¯ āĻŽā§āĻ¸ā§āĻā§āĻāĻ āĻ¯ā§āĻā§āĻ° āĻļāĻŋāĻ˛āĻž āĻāĻ āĻ¨ā§āĻ° āĻāĻĒāĻ° āĻ¨āĻŋāĻ°ā§āĻāĻ° āĻāĻ°ā§āĻ¨āĨ¤
mesozoic
01
āĻŽā§āĻ¸ā§āĻā§āĻ¯āĻŧāĻŋāĻ, āĻŽā§āĻ¸ā§āĻā§āĻ¯āĻŧāĻŋāĻ āĻ¯ā§āĻ āĻ¸āĻŽā§āĻĒāĻ°ā§āĻāĻŋāĻ¤
relating to the geological era between 252 and 66 million years ago
āĻāĻĻāĻžāĻšāĻ°āĻŖ
Fossils from the Mesozoic period provide valuable insights into prehistoric life.
āĻŽā§āĻ¸ā§āĻā§āĻāĻ āĻ¯ā§āĻā§āĻ° āĻā§āĻŦāĻžāĻļā§āĻŽ āĻĒā§āĻ°āĻžāĻā§āĻ¤āĻŋāĻšāĻžāĻ¸āĻŋāĻ āĻā§āĻŦāĻ¨ āĻ¸āĻŽā§āĻĒāĻ°ā§āĻā§ āĻŽā§āĻ˛ā§āĻ¯āĻŦāĻžāĻ¨ āĻ¤āĻĨā§āĻ¯ āĻĒā§āĻ°āĻĻāĻžāĻ¨ āĻāĻ°ā§āĨ¤
āĻļāĻŦā§āĻĻāĻ¤āĻžāĻ¤ā§āĻ¤ā§āĻŦāĻŋāĻ āĻāĻžāĻ
mesozoic
mesozo
āĻ¨āĻŋāĻāĻāĻŦāĻ°ā§āĻ¤ā§ āĻļāĻŦā§āĻĻ
