Mantaua superioară se mai numește și
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Magmatic currents in the asthenosphere rupture the crust, forming pieces known as the upper mantle. These currents circulate, moving upwards or downwards, shaping Earth's solid crust.
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Mantaua superioară se mai numește și
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Scoarța este ruptă de curenții magmatici din astenosferă. Bucățile formate poartă denumirea de
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Curenții magmatici au sens circular, astfel, când se unesc, pot să se deplaseze în sus sau în jos. a. Când curenții au sens ascendent
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