Can We Build a River and Watch a Landscape Evolve?
Give water a gentle slope and a tray of sand. Where will it go, and will it take the same route next time?
The first change may be so small that you miss it. A few grains roll downstream, leaving a slight hollow. More water follows that hollow, moves more grains and deepens it. A little further down the tray, sand starts to collect. The growing bar deflects the water, and a place that was dry a minute ago is suddenly part of the river.
This is the sort of practical I like to set up in my home laboratory. Students can make a prediction, watch the evidence develop and change their minds while the experiment is still running. I'd ask everyone to sketch the route they expect the water to take, then keep the sketches until we can compare them with the overhead photographs.
Suitable for upper KS3 and GCSE, with A-level extensions on experimental design, sediment transport and the limits of models. Allow about an hour for a pilot and two short runs. Repeats can fill a second session.
A river changes the ground that guides it
Erosion removes material from the bed or banks. Transport carries it downstream. Deposition occurs when some of that material settles or comes to rest. All three can happen at once in different parts of the tray. You might see a bank retreat while a sandbar grows a few centimetres away.
The interesting part is what happens next. A shallow hollow can concentrate flow, which may deepen the hollow further. A growing sandbar may split the flow and send water against a bank that had previously been sheltered. This is feedback. The water changes the landscape, and the changed landscape redirects the water. Keep the inlet steady and the channel can still evolve.
Set up a river you can rebuild
Use a shallow, waterproof tray around 60 cm long, damp washed play sand, a few small pebbles, a ruler, stable blocks or shims, a measured water supply and a catch container. A gravity-fed water container with a tap and a short tube makes the flow easier to control. Put the tray on a level workbench, raise the inlet end securely and keep the tray level from side to side. Use a tray with a low outlet or drain into a catch bucket. Test the drainage before adding sand.
- Make the bed. Spread about 2–3 cm of damp sand across the tray and smooth it evenly. Photograph it before starting. For an exploratory run, let the water find its own route. For controlled comparisons, use the same shallow starter groove each time, about 1 cm wide and a few millimetres deep. A simple cardboard template helps reproduce a gentle bend if you want to study one.
- Set the slope. Try raising one end by about 2 cm over a 60 cm horizontal run. Measure the actual rise and run rather than relying on the nominal height of the block.
- Set the discharge. Collect water from the inlet tube for 30 seconds and measure the volume. As a trial setting, aim for about 60 mL in 30 seconds. Recheck the flow during or immediately after the run, especially if the water level in the supply container drops. Direct the water over a small flat stone at the inlet so a falling jet does not dig a crater.
- Start the clock. Run the water for five minutes as a pilot. Take a photograph at the start, then every minute. If the bed barely changes, adjust the discharge or slope for the next pilot. If most of the bed washes away, dial back one of those settings.
- Reset before comparing. Rebuild the bed using the same amount and type of sand, starting moisture, thickness and groove shape. Put the inlet in the same place. Keep sediment out of the sink by letting it settle in the catch bucket and collecting the solids separately.
Two measurements are enough to describe the starting conditions in Blogger-friendly text:
- Discharge (mL/s) = volume collected (mL) / collection time (s)
- Gradient (%) = 100 x vertical rise / horizontal run
So 60 mL in 30 s gives 2 mL/s, and a rise of 2 cm over 60 cm gives a gradient of about 3.3%. Discharge tells you the volume passing per second. Water speed can still vary from place to place as the channel changes width and depth.
Further reading and classroom setup from Carleton College’s Science Education Resource Center
Five investigations from one tray
| Change | How to make the comparison | What to look for |
|---|---|---|
| Water discharge | Try 2 mL/s and 4 mL/s for five minutes each at the same gradient. Use a fresh bed for each run. | When do grains first move? How much does the channel widen at a marked point? Equal times give different total water volumes. To investigate the effect of delivering the same volume more quickly, run 2 mL/s for 5 minutes and 4 mL/s for 2.5 minutes. |
| Slope | Compare a 2 cm rise with a 4 cm rise over the same 60 cm run. Keep the measured inlet discharge the same. | Does a steeper slope change where erosion first appears or how far sediment travels? Check whether erosion deepens the channel, widens it, or does both. |
| Particle size | Lay equal-width strips of finer and coarser sand across the same starter channel. Use the same sediment type where possible and swap the order in a repeat. | Which grains move first? Where do they settle? Swapping the order helps separate the effect of grain size from the effect of position. |
| An obstacle | Compare an open channel with the same channel containing one small, firmly placed pebble. | Look for a scour hollow near the pebble, a sheltered deposit or a jet diverted into the bank. Mark the exact locations on a photograph. |
| Vegetation analogues | Add a row of upright bristles fixed in a base buried flush with the sand. Compare with an otherwise identical buried base without bristles. | Does sediment accumulate among the stems? Does flow concentrate around the ends of the row? The bristles model the effect of stems on flow. Real roots can also strengthen a bank, which this setup does not test. |
For a first lesson I would choose the obstacle. It gives students a specific spot to watch, and their predictions are often quite revealing. Some will look only for a deposit behind the pebble. Others will follow the water squeezing round the sides and notice what happens to the neighbouring bank. Both observations help explain how one small feature can affect a larger stretch of channel.
Make a bend migrate, then give the river somewhere to end
A gentle starter bend gives you a better chance of seeing bend development in a short session. Put two marks on the rim of the tray opposite the bend and use them to locate the same cross-section in every photograph. Look for erosion on the outside and deposition on the inside. If both persist and the bend shifts sideways, you have evidence of bend migration. Loose sand may slump, the flow may split, or the bend may straighten. A single curved groove shows a bend. A sequence of photographs can show whether it behaves like a migrating meander.
To investigate a delta, arrange the downstream end so the channel enters a shallow pool of standing water. A separate clear container below the tray outlet works if the channel enters gently at the water surface. An overflow lip draining to the catch bucket can keep the pool level approximately steady. Use sand carried by the stream and watch where it accumulates as the inflow spreads into the pool. Photograph the leading edge from above. If it advances into the water, you are watching a small delta grow. Sediment spreading onto a dry, flatter surface forms a fan-shaped deposit, which makes a useful comparison with the pool run.
Look closely at the deposits. Coarser sand may settle near the entrance while finer grains travel further. Some of the finest material may leave the pool in the overflow. Follow the grains you can actually see, and use a close-up before assigning each patch to a size class.
Laboratory research on bend development and meander cut-off
Let the camera do some of the measuring
For filming this in my lab, I would use a fixed camera directly overhead and a second camera low at the downstream end. The overhead view shows where the channel goes. The lower view helps reveal grains in motion and makes it easier to see the difference between a submerged deposit and a bar emerging above the water.
Keep a ruler and two fixed reference marks in the overhead frame. If you are measuring from the photos, position the ruler close to the level of the sand surface and keep it out of the water. Use the same crop and lighting throughout. Label the stills with elapsed time and run conditions. Trace the channel edges from successive frames on separate layers, or mark them on printed photographs with different colours.
| Elapsed time | Channel width at marked section | What changed? |
|---|---|---|
| 0 min | 1.0 cm | Starter groove visible |
| 1 min | 1.3 cm | A few grains roll past the bend |
| 3 min | 2.1 cm | Outer bank retreats and an inner bar appears |
| 5 min | 2.4 cm | Bar extends downstream |
Illustrative data to show how to record a run. The widths are examples.
At the end of the example run the channel is 1.4 cm wider, but the notes tell you more than the subtraction. The outer bank moved and a bar grew inside the bend. Next time, record the position of each bank as well as the width. A channel can migrate sideways while staying nearly the same width. Repeat each condition, if time allows, and show the spread of the results before deciding how much weight to give a difference.
From the tray to the Thames
Spending time on the Thames makes me particularly interested in where the current is strongest and where material collects. From a boat you can notice the flow slipping around an obstruction or a quiet patch opening up behind it. In the tray, you can pause over that same sort of pattern and ask what it might do to the bed if it continued.
A tray brings some river processes into view on a laboratory timescale. It cannot tell us how quickly a particular reach of the Thames will change. Real rivers have a history of floods, changing sediment supplies, different bank materials, living roots and human engineering. Even dedicated laboratory research treats the translation of experimental time to river time cautiously. For a student, that makes a good final question. Which feature of the model would you change first to represent the stretch of river you know? Laboratory study of meander cut-off
Look at the first minute again
When the experiment finishes, go back to the first photograph. Find the first tiny hollow, displaced grain or patch of sand that started to grow. Can you trace a line from that small change to the final channel? Then rebuild the tray and see which parts of that story happen again.
The channel on the last photograph may look as though it was always going to end up there. The pleasure of watching the whole sequence is seeing how much depended on what happened just before. Next time you look down from a bridge at a sandbar or a sharply cut bank, ask yourself where the water will go because that feature is there, and what it might change next.




