River delta slope offshore, waves will make river deltas smoother. Waves can also be responsible for carrying sediments away from the river delta, causing the delta to retreat. For deltas that form further upriver in an estuary, there are complex yet quantifiable linkages between winds, tides, river discharge, and delta water levels. Erosion is also an important control in tide-dominated deltas, such as the Ganges Delta, which may be mainly submarine, with prominent sandbars and ridges. This tends to produce a "dendritic" structure. Tidal deltas behave differently from a river- and wave-dominated deltas, which tend to have a few main distributaries. Once
Indus River Delta , 220 km, and . Because the Indus river has switched its location at various points in history, it has an "active" delta region, and total delta region (all area that was once a part of the delta). The total area is estimated at , and . The active area is estimated at , and . The length of the total delta along the axis of Indus is estimated at , whereas the current delta stretches from the Arabian Sea to just south of Thatta (~). There are currently 17 major creeks(Including Sir Creek, Bhitiaro Creek and Kori Creek) and