What effect does a uniform bedrock have on streamflow patterns in dendritic systems?

Uniform bedrock influences streamflow patterns in dendritic systems by providing a consistent underlying geological structure. When the bedrock is uniform, the topography tends to erode in predictable ways, allowing streams to develop more systematic and organized drainage patterns. This uniformity means that variations in streamflow are less influenced by changes in the underlying materials, leading to a more consistent and steady flow of water through the system.

In contrast, irregular bedrock could lead to chaotic flow patterns due to variations in resistance to erosion, while a series of waterfalls might develop if there are significant differences in rock types or elevations, neither of which would be the case with uniform bedrock. Hence, it can be concluded that a uniform bedrock indeed does not control or significantly alter the pattern of streamflow beyond what is expected in a regular dendritic drainage system.