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← GeographyWhich outcome results when pyroclastic density currents encounter topographic obstacles?
A)Localized surge pockets form rapidly✓
B)Pressure gradients stabilize flow layers
C)Entrainment of ash deposits ceases
D)Magmatic outgassing spontaneously elevates
💡 Explanation
Localized surge pockets form because the flow compresses due to the topographic barrier which initiates a process of Boundary Layer Separation; therefore, these create turbulent, ash-rich regions rather than ceasing entrainment.
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