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¨
continental crust
/kËÉntÉĒnËÉntÉl kÉšËĘst/
Continental crust
01
āĻŽāĻšāĻžāĻĻā§āĻļā§āĻ¯āĻŧ āĻā§āĻ¤ā§āĻŦāĻ, āĻ¸ā§āĻĨāĻ˛āĻāĻžāĻā§āĻ° āĻā§āĻ¤ā§āĻŦāĻ
the thick, buoyant part of the Earth's crust that forms the continents, composed mainly of granitic rocks and less dense than oceanic crust
āĻ¨āĻŋāĻāĻāĻŦāĻ°ā§āĻ¤ā§ āĻļāĻŦā§āĻĻ
