Conduct a stream-table investigation modeling how flowing water erodes and deposits sediment, and relate water flow rate to erosion rate.
A stream table is a simple model: a shallow tray filled with sand or soil, tilted slightly, with water poured at the top to act like a stream. Watching where the model stream cuts into the sand, and where it drops sand back down, lets you observe erosion and deposition happening in minutes instead of years.
Changing how fast the water flows changes how much erosion happens. A slow trickle barely moves the sand, while a fast pour cuts a visible channel and carries sand a long way before dropping it. This mirrors real rivers, where a fast flood can erode far more material than the same river on a calm day.
Mastery looks like: They can run a controlled stream-table test comparing flow rates and explain that faster flow produces more erosion and longer sediment transport.
Common stumbles: Changing more than the flow rate between trials (different sand, different tilt); describing the results without connecting them back to erosion and deposition vocabulary.