Which consequence results when magma's slow cooling rate within dikes creates a high viscosity lava that obstructs its own pathway?

A)Increased country rock assimilation rates

B)Formation of densely packed lava domes✓

C)Widespread pyroclastic density currents

D)Reduced phenocryst formation in magma

💡 Explanation

The formation of lava domes occurs because high viscosity lava solidifies near the vent, obstructing the pathway; viscous lava cannot flow far causing a buildup. Therefore, lava domes form rather than effusive flows because the magma's high silica content increases viscosity.

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Which consequence results when magma's slow cooling rate within dikes creates a high viscosity lava that obstructs its own pathway?

💡 Explanation

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