dendritic drainage pattern

A dendritic drainage pattern is the most common type of stream network, resembling the branching of a tree or the veins of a leaf. This pattern develops in areas where the underlying rock or sediment is relatively uniform and lacks significant structural weaknesses like faults or joints.12

In a dendritic system, the main stream (trunk) is fed by numerous smaller tributaries, which in turn are fed by even smaller streams. This arrangement allows for efficient drainage of a large area with minimal slope. The conveyance properties of such a network are similar to those of circulatory systems or tree branching. This pattern is typically found in regions with flat-lying sedimentary rocks.12