glaciation
gla
ˌgleÉĒ
glei
cia
ˈʃieÉĒ
shiei
tion
ʃən
shēn
/ÉĄlˌe‍ÉĒsÉĒˈe‍ÉĒʃən/

āχāĻ‚āϰ⧇āϜāĻŋāϤ⧇ "glaciation"āĻāϰ āϏāĻ‚āĻœā§āĻžāĻž āĻ“ āĻ…āĻ°ā§āĻĨ

01

āĻšāĻŋāĻŽāĻŦāĻžāĻšā§€āĻ•āϰāĻŖ, āĻšāĻŋāĻŽāϝ⧁āĻ—

the geological process involving the expansion and movement of glaciers, shaping landscapes through erosion, deposition, and the formation of distinctive glacial landforms
āωāĻĻāĻžāĻšāϰāĻŖ
Glacial striations on bedrock surfaces provide evidence of the direction of ice flow during glaciation.
āĻŦ⧇āĻĄāϰāĻ• āĻĒ⧃āĻˇā§āĻ āϤāϞ⧇ āĻšāĻŋāĻŽāĻŦāĻžāĻšā§‡āϰ āĻĻāĻžāĻ—āϗ⧁āϞāĻŋ āĻšāĻŋāĻŽāĻžāϝāĻŧāύ āϏāĻŽāϝāĻŧ⧇ āĻŦāϰāĻĢ āĻĒā§āϰāĻŦāĻžāĻšā§‡āϰ āĻĻāĻŋāϕ⧇āϰ āĻĒā§āϰāĻŽāĻžāĻŖ āĻĻ⧇āϝāĻŧāĨ¤
02

the state or condition of a region being covered by glaciers or ice as a result of glacial activity

āωāĻĻāĻžāĻšāϰāĻŖ
Glaciation left thick ice sheets across the landscape.

āĻļāĻŦā§āĻĻāϤāĻžāĻ¤ā§āĻ¤ā§āĻŦāĻŋāĻ• āĻ—āĻžāĻ›

glaciation
glaciate
glace
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āύāĻŋāĻ•āϟāĻŦāĻ°ā§āϤ⧀ āĻļāĻŦā§āĻĻ
LanGeek
āĻ…ā§āϝāĻžāĻĒ āĻĄāĻžāωāύāϞ⧋āĻĄ āĻ•āϰ⧁āύ