Gravity flow was active in Taiwan Shoal Slope and deposited the spectacular correspondingly deposition system, and so been the perfect area of the study on process of the gravity flow. At least three geomorphologic breaks including one shelf break and two slope break exist from shelf front to abyssal Manila Trench. These breaks control the initiation and completely evolution of the gravity flow and control the distributing framework of kinds of gravity-flow-deposited system. Among them the shelf break control the initiation of the mass waste and the first and second slope break control transformation between slump, debris flow and turbidity flow respectively. After utilizing the parameters of waveform of sediment wave the correspondingly rheology of gravity flow was reconstructed and assert the existence of the actively gravity flow. The multiple breaks mark the unequilibrium of the slope system and the slope profile’s evolution to the equilibrium, so the effect of erosion-deposition of gravity flow is only the superficial expression of the adjustment of the slope system.