Reuse terms for this investigation’s photography are still being finalised. Read image rights and use before redistributing beyond your own classroom.
What Water Leaves Behind
What can running water tell us about the land it moves through, and how should we share what is left?
A waterfall is the easy part. The harder question is where the water came from, how long it has been working on this rock, and who else is counting on it.
Choose a path
- 01
Setting the stage
Project photograph 1 with no title, no caption and no context. Say nothing about it. Ask two questions, take four or five answers, and do not confirm or correct any of them. Write the guesses on the board, and write the rainfall numbers next to them.

Water drops down a face of dark, wet rock into a still pool. Everything the water is not touching is bare: pale rock, dry branches, no soil worth the name. The green is confined to a narrow band exactly where the water runs, which is the first thing worth noticing and the last thing students notice. - 02
Engaging with the story
Show photographs 2 through 5 in order. Give students a job before you start. If Greg’s field account has been recorded, read it aloud while the images are on screen. If it has not, give students a silent minute with each frame instead.

The same process at a scale that will not fit in one glance. A large river drops over a hard step into a canyon it has cut through hundreds of meters of rock. The rainbow standing in the air below the fall is a measure of how much water is being thrown into the air, and how hard. 
A fall on a sandstone wall, with three things worth reading in one frame: the dark vertical streaks where water has run down the rock for a very long time, the green growing only in the wet zone, and the shallow pool with a sand beach at the bottom — sand that used to be part of the wall. 
The same kind of stream, in the season when it appears to be doing nothing. Snow has buried the channel except for a few dark gaps of open water. Whether the stream is working less, or working on a different schedule, is the question — and the photograph cannot settle it. 
A raft with people in it, near the far bank, against a cliff of layered rock. The raft is a few meters long. Use it to measure the cliff, then ask which of the two the river made. - 03
Working the evidence
The core of the investigation. Students work in pairs on the handout, using the Observe, Reflect, Question structure the Library of Congress developed for reading primary sources. A photograph is a primary source, and this is how it is done. Put photograph 1 back on screen and leave it there.

Water drops down a face of dark, wet rock into a still pool. Everything the water is not touching is bare: pale rock, dry branches, no soil worth the name. The green is confined to a narrow band exactly where the water runs, which is the first thing worth noticing and the last thing students notice. - 04
Delving deeper
Now name the mechanism: much of the permanent water in dry country is groundwater, recharged somewhere else and often long ago, reaching the surface where the geology forces it out. Then hand out the data.
- 05
Reflecting and projecting
The claim, evidence and reasoning assignment. Two parts. Both appear on the student handout as Part A and Part B.
The evidence

Water drops down a face of dark, wet rock into a still pool. Everything the water is not touching is bare: pale rock, dry branches, no soil worth the name. The green is confined to a narrow band exactly where the water runs, which is the first thing worth noticing and the last thing students notice.

The same process at a scale that will not fit in one glance. A large river drops over a hard step into a canyon it has cut through hundreds of meters of rock. The rainbow standing in the air below the fall is a measure of how much water is being thrown into the air, and how hard.

A fall on a sandstone wall, with three things worth reading in one frame: the dark vertical streaks where water has run down the rock for a very long time, the green growing only in the wet zone, and the shallow pool with a sand beach at the bottom — sand that used to be part of the wall.

The same kind of stream, in the season when it appears to be doing nothing. Snow has buried the channel except for a few dark gaps of open water. Whether the stream is working less, or working on a different schedule, is the question — and the photograph cannot settle it.

A raft with people in it, near the far bank, against a cliff of layered rock. The raft is a few meters long. Use it to measure the cliff, then ask which of the two the river made.
Did you teach this?
Three questions, two minutes, and it shapes the next investigation we build.