When streams meet the ocean, they manage to reach their base level, erode their banks, and promote the migration of meanders.
We can arrive at this answer because:
- When the stream meets the ocean, it means that it has reached its base level, with the meeting of the ocean that is at low altitudes.
- The action of low altitude allows for an elevation of the work of the stream waters, which gradually increases as the stream descends to meet the ocean.
- With that, the stream manages to erode its banks with greater intensity, due to the high work and the descending movement.
- With this, the stream can follow stones and pieces from the banks into the meander, which begins to move over time, as this system repeats itself.
In this case, when the stream meets the river, the entire path system to that meeting is affected, due to the change in altitude.
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