The drainage pattern of the Gindi river basin is likely to be dendritic. A dendritic drainage pattern is characterized by a network of streams that resemble the branches of a tree, with tributaries joining together to form larger streams, which eventually converge into a main stem. This type of pattern is commonly found in areas with relatively flat terrain and uniform rock types, where streams are able to develop a maze-like network of channels as they meander across the landscape. In a dendritic drainage pattern, the streams follow a random, branching pattern and there is no dominant direction of flow.
