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¨
lithosphere
/lËÉĒθÉsfËiÉ/
Lithosphere
āĻāĻĻāĻžāĻšāĻ°āĻŖ
Oceanic lithosphere is denser than continental lithosphere, leading to differences in elevation.
āĻ¸āĻžāĻŽā§āĻĻā§āĻ°āĻŋāĻ āĻ˛āĻŋāĻĨā§āĻ¸ā§āĻĢāĻŋāĻ¯āĻŧāĻžāĻ° āĻŽāĻšāĻžāĻĻā§āĻļā§āĻ¯āĻŧ āĻ˛āĻŋāĻĨā§āĻ¸ā§āĻĢāĻŋāĻ¯āĻŧāĻžāĻ° āĻāĻ° āĻā§āĻ¯āĻŧā§ āĻāĻ¨, āĻ¯āĻž āĻāĻā§āĻāĻ¤āĻžāĻ° āĻĒāĻžāĻ°ā§āĻĨāĻā§āĻ¯ā§āĻ° āĻĻāĻŋāĻā§ āĻ¨āĻŋāĻ¯āĻŧā§ āĻ¯āĻžāĻ¯āĻŧāĨ¤
āĻ¨āĻŋāĻāĻāĻŦāĻ°ā§āĻ¤ā§ āĻļāĻŦā§āĻĻ
