The experiment confirms that meanders are often initiated by disturbances in the channel (e.g., obstacles or bank variations).
Based on the provided search results regarding the formation of meanders in a stream table, the (likely represented by Stream Table Meanders-How to Create a Meander , which is highly relevant to this topic), illustrates the dynamic processes of fluvial geomorphology. This video demonstrates how a relatively straight watercourse transforms into a meandering, or curvy, channel through active erosion and deposition. Meander 2019 esp.mp4
Water moves faster, creating high velocity and, consequently, high erosion, leading to the creation of a steep bank. The experiment confirms that meanders are often initiated