orogeny
o
o:
o
ro
ˈrɑ:
raa
ge
ʤə
jē
ny
ni
ni
/ɔːɹˈɒd‍ʒəni/

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

01

āĻĒāĻ°ā§āĻŦāϤ āĻ—āĻ āύ, āĻ“āϰ⧋āĻœā§‡āύāĻŋ

the geological process of mountain building, usually occurring due to the collision or convergence of tectonic plates
āωāĻĻāĻžāĻšāϰāĻŖ
The Andes mountain range in South America is associated with the ongoing orogeny caused by the subduction of the Nazca Plate beneath the South American Plate.
āĻĻāĻ•ā§āώāĻŋāĻŖ āφāĻŽā§‡āϰāĻŋāĻ•āĻžāϰ āφāĻ¨ā§āĻĻ⧇āϜ āĻĒāĻ°ā§āĻŦāϤāĻŽāĻžāϞāĻž āύāĻžāϜāĻ•āĻž āĻĒā§āϞ⧇āĻŸā§‡āϰ āĻĻāĻ•ā§āώāĻŋāĻŖ āφāĻŽā§‡āϰāĻŋāĻ•āĻžāύ āĻĒā§āϞ⧇āĻŸā§‡āϰ āύāĻŋāĻšā§‡ āϏāĻžāĻŦāĻĄāĻžāĻ•āĻļāύ⧇āϰ āĻ•āĻžāϰāϪ⧇ āϚāϞāĻŽāĻžāύ āĻĒāĻ°ā§āĻŦāϤ āĻ—āĻ āύ āĻĒā§āϰāĻ•ā§āϰāĻŋāϝāĻŧāĻž āĻāϰ āϏāĻžāĻĨ⧇ āϝ⧁āĻ•ā§āϤāĨ¤
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āύāĻŋāĻ•āϟāĻŦāĻ°ā§āϤ⧀ āĻļāĻŦā§āĻĻ
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āĻ…ā§āϝāĻžāĻĒ āĻĄāĻžāωāύāϞ⧋āĻĄ āĻ•āϰ⧁āύ