7Sea-floor topography can constrict, deflect, or reflect turbidity currents resulting in a range of 8 distinctive deposits. Where flows rebound off slopes and a suspension cloud collects in an enclosed 9 basin, ponded or contained turbidites are deposited. Ponded turbidites have been widely recognized 10 in slope mini-basins and on small, structurally confined basin floors in strike-slip and foreland-basin 11 settings. They can have a variable internal structure the significance of which remains poorly 12 understood in terms of flow behavior. New experiments demonstrate that the ponding process can 13 comprise up to four phases: 1) cloud establishment, 2) inflation, 3) steady-state maintenance, and 4) 14 collapse. The experiments explored the behavior of sustained turbidity currents draining into small 15 basins and show that the ponded suspensions that form are characterized by an important internal 16 interface; this divides a lower outbound-moving layer from an upper return layer. The basal layer 17 evolves to constant concentration and grain size, whereas the upper layer is graded (concentration 18 and grain size decrease upward). During the cloud inflation stage, the concentration and velocity 19 profiles of the ponded suspension evolve, and this phase can dominate the resulting deposit. 20Outbound internal waves can travel along the interface between the outbound and return layers and 21 impinge against the confining slope, and their amplitude is highest when the density contrast 22 between layers is greatest, e.g., when the input flows are thin and dense. The experiments show 23 that flow reversals can arise in several ways (initial rebound, episodic collapse of the wedge of fluid 24 above the counter slope, "grounding" of the internal velocity interface) and that despite steady 25 2 input, velocities decay and the deposit grades upwards. Internal waves emanate from the input 26 point, i.e., do not form as reflections off the counter slope. The internal grain-size interface within 27