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Psychologists who consider the frustration-aggression hypothesis incomplete argue that the real cause of aggression is:
Foreland Basin
A basin that forms when crust (either continental or oceanic) is warped by the weight of thrust sheets, especially when formed between a mountain belt and continental interior.
Passive Margin
A tectonically inactive edge of a continent, characterized by a transition from continental to oceanic lithosphere without significant seismic activity.
Normal-Fault Basin
A low area that has been downdropped by one or more normal faults.
Passive Margin
A coastline margin that is not associated with plate boundaries and therefore experiences little to no seismic or volcanic activity.
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