Which outcome frequently occurs along transform fault boundaries in continental crust?

💡 Explanation

When transform faults occur in continental crust, lateral displacement between plates builds shear stress because friction resists motion, accumulating energy that is suddenly released as shallow focus, strike-slip earthquakes. Therefore, frequent shallow earthquakes result, rather than trenches, volcanoes, or metamorphism which require converging or diverging plate motions and different thermal conditions.

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