What occurs after a river adjusts its base level regarding floodplains?

When a river adjusts its base level, it can lead to complex geomorphological changes, particularly influencing the characteristics of its floodplain. If the base level of the river decreases—for instance, due to a lowering of sea level or uplift of land—the river will begin to erode its banks further, cutting downwards into its bed. This process often results in the formation of a new floodplain at a lower elevation than the previous one.

As the riverbed lowers, sediment can be deposited along this newly formed channel, creating a floodplain that is positioned at a level below the old one. This is crucial for understanding how rivers respond to changes in their hydrological and geological context, as the ecological dynamics and flood risk associated with these floodplains will evolve as a result of these adjustments.

This understanding illustrates the interconnectedness of hydrology and landscape evolution, highlighting how rivers can reshape their environments over time in response to changes in base level.