asthenosphere
as
as
as
the
ˈθɛ
the
nos
nəs
nēs
phere
ˌfÉĒr
fir
/ɐsθˈɛnəsfˌiə/

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

01

āĻ…ā§āϝāĻžāĻ¸ā§āĻĨ⧇āύ⧋āĻ¸ā§āĻĢāĻŋāϝāĻŧāĻžāϰ, āĻĒ⧃āĻĨāĻŋāĻŦā§€āϰ āĻ­ā§‚āĻ¤ā§āĻŦāϕ⧇āϰ āύāĻŋāĻšā§‡ āĻ…āĻ°ā§āϧ-āϤāϰāϞ āĻļāĻŋāϞāĻžāϰ āĻ¸ā§āϤāϰ

a layer of semi-fluid rock beneath the Earth's crust that allows tectonic plates to move
āωāĻĻāĻžāĻšāϰāĻŖ
Seismic waves passing through the asthenosphere reveal its semi-fluid nature and lower resistance to deformation.
āĻ…ā§āϝāĻžāϏāĻĨ⧇āύ⧋āĻ¸ā§āĻĢāĻŋāϝāĻŧāĻžāϰ āĻāϰ āĻŽāĻ§ā§āϝ āĻĻāĻŋāϝāĻŧ⧇ āϝāĻžāĻ“āϝāĻŧāĻž āϏāĻŋāϏāĻŽāĻŋāĻ• āϤāϰāĻ™ā§āĻ—āϗ⧁āϞāĻŋ āĻāϰ āφāϧāĻž-āϤāϰāϞ āĻĒā§āϰāĻ•ā§ƒāϤāĻŋ āĻāĻŦāĻ‚ āĻŦāĻŋāĻ•ā§ƒāϤāĻŋāϰ āĻŦāĻŋāϰ⧁āĻĻā§āϧ⧇ āĻ•āĻŽ āĻĒā§āϰāϤāĻŋāϰ⧋āϧ āĻĒā§āϰāĻ•āĻžāĻļ āĻ•āϰ⧇āĨ¤
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āύāĻŋāĻ•āϟāĻŦāĻ°ā§āϤ⧀ āĻļāĻŦā§āĻĻ
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āĻ…ā§āϝāĻžāĻĒ āĻĄāĻžāωāύāϞ⧋āĻĄ āĻ•āϰ⧁āύ