Wear on Earth
View Sequence overviewStudents will:
- conduct a fair test to explore changes to water volume as it changes state from a liquid to a solid.
- apply their understanding of increasing water volume (during freezing) to explain how freeze-thaw weathering can split rocks in nature.
Students will represent their understanding as they:
- make a claim about the effect of freezing on water, based on their findings.
- draw a labelled diagram to explain freeze-thaw weathering.
- consider and discuss the conditions in nature required to facilitate freeze-thaw weathering.
In this lesson, assessment is formative.
Feedback might focus on:
- students’ line graphs. Have students clearly represented their observations with an increase in water volume (when frozen) on the line graph?
- students’ claims about water volume as a liquid and a solid. Have students identified and provided evidence to support the claim that water expands when it freezes?
- students’ freeze-thaw weathering diagram. Have students identified the repeated freezing and thawing cycle that gradually cracks and breaks rocks?
Whole class
Class science journal (digital or hard-copy)
Demonstration copy of the What broke the bottle? Resource sheet
Demonstration copy of the Variables grid Resource sheet
Optional: Demonstration copy of the Freeze-thaw investigation planner Resource sheet
1 x syringe (10ml or 20ml, catheter tip or similar, no needle) with coloured water inside and sealed with blu-tac on end, or another container that can hold water and will be easy for students to see the visible change in the volume. This will be used for demonstration purposes only.
Video: Freeze-Thaw Weathering Explained (2:48)
Each group
1 x syringe (10ml or 20ml, catheter tip or similar, no needle), or another container that can hold water and will be easy for students to see the visible change in the volume
Small amount of blu tac to seal the end (if using syringes)
Coloured water
Optional: a second identical syringe with the same amount of coloured water, pre-frozen—the water will expand (see note below on lesson timing)
Each student
Individual science journal (digital or hard-copy)
Freeze-thaw investigation planner Resource sheet
Note on lesson timing
The investigation in this lesson involves freezing water for observation. The water must be frozen before the final steps of the investigation can be completed.
To manage the timing and allow for freezing, it is recommended that the lesson is completed in two stages. See the end of the Investigate step for recommendation on how to split the lesson.
Alternatively, you might pre-freeze the exact amounts of water students are going to use, in the same containers, prior to beginning the lesson. These can them be presented as “some I prepared earlier” before the lesson continues.
Lesson
Re-orient
Review the definition of physical weathering introduced in the previous lesson: when physical forces break down rock into smaller pieces.
Discuss the physical forces that break down rocks that students explored in their investigations—abrasion (which occurs when rocks rub and tumble against each other), breaking of particles and smoothing edges of rocks.
- What is physical weathering?
- What type of force did we use to weather our rocks in the last investigation?
- Why did our rocks change shape when we shook them?
- What process in nature were we replicating when we shook the ‘rocks’ in the jar?
- In nature, would all rock types weather and change shape at the same rate? Why/why not?
- Harder rocks made of harder minerals take longer to weather.
- Other than the hardness of rocks, what else might affect how fast they weather?
The Inquire phase allows students to cycle progressively and with increasing complexity through the key science ideas related to the core concepts. Each Inquire cycle is divided into three teaching and learning routines that allow students to systematically build their knowledge and skills in science and incorporate this into their current understanding of the world.
When designing a teaching sequence, it is important to consider the knowledge and skills that students will need in the final Act phase. Consider what the students already know and identify the steps that need to be taken to reach the level required. How could you facilitate students’ understanding at each step? What investigations could be designed to build the skills at each step?
Read more about using the LIA FrameworkIdentifying and constructing questions is the creative driver of the inquiry process. It allows students to explore what they know and how they know it. During the Inquire phase of the LIA Framework, the Question routine allows for past activities to be reviewed and to set the scene for the investigation that students will undertake. The use of effective questioning techniques can influence students’ view and interpretation of upcoming content, open them to exploration and link to their current interests and science capital.
When designing a teaching sequence, it is important to spend some time considering the mindset of students at the start of each Inquire phase. What do you want students to be thinking about, what do they already know and what is the best way for them to approach the task? What might tap into their curiosity?
Read more about using the LIA FrameworkHow can water cause weathering?
Ask students to identify how water appears in the environment, prompting them to think about it in all its states.For example:
- Liquid: creek, river, lake, puddle, ocean.
- Solid: ice, snow (loosely held ice crystals).
- Gas: water vapour caused through evaporation.
Note: In Year 3 students would have learned about how adding and removing heat from liquids changes its state. They also will have learned about the water cycle in Year 4, and may have already learned about the three states of matter—solid, liquid and gas—earlier in Year 5. Their level of understanding of these phenomena will impact their responses. The key focus relevant here is water moving between a solid and liquid state through the adding and removal of heat energy.
Pose the question: Can freezing and thawing water cause weathering to rocks?
Discuss the definition of the term ‘thawing’ if required.
The Inquire phase allows students to cycle progressively and with increasing complexity through the key science ideas related to the core concepts. Each Inquire cycle is divided into three teaching and learning routines that allow students to systematically build their knowledge and skills in science and incorporate this into their current understanding of the world.
When designing a teaching sequence, it is important to consider the knowledge and skills that students will need in the final Act phase. Consider what the students already know and identify the steps that need to be taken to reach the level required. How could you facilitate students’ understanding at each step? What investigations could be designed to build the skills at each step?
Read more about using the LIA FrameworkThe Investigate routine provides students with an opportunity to explore the key ideas of science, to plan and conduct an investigation, and to gather and record data. The investigations are designed to systematically develop content knowledge and skills through increasingly complex processes of structured inquiry, guided inquiry and open inquiry approaches. Students are encouraged to process data to identify trends and patterns and link them to the real-world context of the teaching sequence.
When designing a teaching sequence, consider the diagnostic assessment (Launch phase) that identified the alternative conceptions that students held. Are there activities that challenge these ideas and provide openings for discussion? What content knowledge and skills do students need to be able to complete the final (Act phase) task? How could you systematically build these through the investigation routines? Are there opportunities to build students’ understanding and skills in the science inquiry processes through the successive investigations?
Read more about using the LIA FrameworkWhat happens to water when it freezes?
Ask students if they have ever seen what happens when a full bottle of water is left in the freezer. View the image on the What broke the bottle? Resource sheet telling students that the bottle had been left in the freezer overnight. Students compare this to previous experiences and suggest reasons why the bottle broke.
If not already offered by the students, share your own thinking: As the water froze, it expanded and broke the bottle.
Ask students how they might devise a fair test to investigate if water does indeed expand as it freezes.
If required, prompt students by showing them the equipment available for the investigation. For example, show them a syringe of coloured water (with a small amount of Blu-Tac used to seal the end) and ask them how we might use it to see if water expands when it is frozen.

Pose the broad question: What things might affect the volume of water?
Using a demonstration copy of the Variables grid Resource sheet, identify and record the thing to be measured during the investigation—that is, the volume of water in the syringe—and place that in the centre of the grid, marked with (M). Brainstorm other variables in the surrounding columns/rows. Add or remove additional columns/rows as required. For example,
Note: In some investigations it is appropriate to allow teams to select the variable they wish to change, and teams might select different variables. However, in this case, the goal of the investigation is to show that water expands as it freezes. This is achieved by changing the water from a liquid state to a solid state through freezing, so all teams should investigate this same variable.
Model how to use the question stem to write a question for the investigation: What happens to the volume of water when we change the state of the water from liquid to solid?
Discuss how the investigation will be conducted and data collected and recorded.
- How could we measure the volume of water?
- How will we record the before and after freezing measurements?
- How long will it need to be in the freezer for the water to freeze?
Optional: Discuss fair testing principles, including why it is essential to only change one variable and leave everything else the same: to ensure that we find out the impact changing a specific variable has on the outcome. If multiple variables are changed there is no way of knowing which one made the impact and to what degree.
In collaborative teams, students plan their investigation and record their results using the Freeze-thaw Investigation Planner Resource Sheet.
Ideally this investigation should take place over two lessons to allow the water time to freeze. You might organise this by:
- Completing page 1 of the investigation planner and the liquid water observations and measurements on page 2 in one lesson.
- Placing the water-filled syringes into the freezer.
- In a follow-up lesson the next day or week, complete the solid water observations, results and claims (remainder of page 2 and page 3).
- Leave the freeze-thaw weathering diagram to be complete AFTER the integrate step is complete.
Using a variables grid to plan a fair test investigation
How might you support students to conduct an accurate fair test investigation, with a clear investigable question?
All scientific fair tests involve variables. Variables are things that can be changed (independent), measured/observed (dependent) or kept the same (controlled) in an investigation.
When planning a fair-test investigation, to make it a fair, we need to identify the variables. A variables grid can be used to record the identified variables. We then use these variables to turn a broad question, such as "What affects plant growth?" into an investigable one, such as "What happens to the growth of a plant when I change how much water it gets?".
Investigable questions are characterised by their clear identification of what is being changed and what outcome is being measured in a fair test, supporting students to investigate a specific physical phenomenon.
Investigable questions enable students to plan a fair test investigation. The question they have devised can be answered empirically, and data can be collected to support and justify claims made.
By planning for and conducting a fair test, students can make claims about how the variable they have changed in their investigation may have affected what is being measured and/or observed.
To support students to identify variables, and to use those variables to inform their planning of a fair test, we suggest this handy mnemonic ‘Cows Moo Softly’. This helps students remember the letters C, M and S, representing the three types of variables in a fair test:
- Cows: Change one thing (independent variable)
- Moo: Measure/Observe the outcome (dependent variable) and
- Softly: Keep the other things (controlled variables) the Same
Why does water expand when frozen?
Most liquids take up less volume as they become solids. Liquid water is unique.
Most liquids take up less volume as they become solids. When a liquid loses heat, the particles in the liquid slow their movement. This means they can get closer to each other and take up less volume.
Water (liquid H₂O) is unique. Each water molecule is like a tiny magnet arranged in a V-shape with O (oxygen) at the bottom of the V, and the two H (hydrogen) at the top of each arm of the V.
Like magnets, the H atoms on the arms of one water molecule are attracted to the O atom on the point of a neighbouring water molecule. This is what makes water molecules stick close to each other. In liquid water, the molecules are constantly moving, briefly sticking together before breaking apart again.
When the liquid water starts to freeze, the molecules in liquid water slow down and start arranging themselves so that each H is pointing to an O on another molecule. This creates special solid shapes with the molecules arranged in a permanent lattice shape that takes up more volume.
Most liquids take up less volume as they become solids. When a liquid loses heat, the particles in the liquid slow their movement. This means they can get closer to each other and take up less volume.
Water (liquid H₂O) is unique. Each water molecule is like a tiny magnet arranged in a V-shape with O (oxygen) at the bottom of the V, and the two H (hydrogen) at the top of each arm of the V.
Like magnets, the H atoms on the arms of one water molecule are attracted to the O atom on the point of a neighbouring water molecule. This is what makes water molecules stick close to each other. In liquid water, the molecules are constantly moving, briefly sticking together before breaking apart again.
When the liquid water starts to freeze, the molecules in liquid water slow down and start arranging themselves so that each H is pointing to an O on another molecule. This creates special solid shapes with the molecules arranged in a permanent lattice shape that takes up more volume.
The Inquire phase allows students to cycle progressively and with increasing complexity through the key science ideas related to the core concepts. Each Inquire cycle is divided into three teaching and learning routines that allow students to systematically build their knowledge and skills in science and incorporate this into their current understanding of the world.
When designing a teaching sequence, it is important to consider the knowledge and skills that students will need in the final Act phase. Consider what the students already know and identify the steps that need to be taken to reach the level required. How could you facilitate students’ understanding at each step? What investigations could be designed to build the skills at each step?
Read more about using the LIA FrameworkFollowing an investigation, the Integrate routine provides time and space for data to be evaluated and insights to be synthesized. It reveals new insights, consolidates and refines representations, generalises context and broadens students’ perspectives. It allows student thinking to become visible and opens formative feedback opportunities. It may also lead to further questions being asked, allowing the Inquire phase to start again.
When designing a teaching sequence, consider the diagnostic assessment that was undertaken during the Launch phase. Consider if alternative conceptions could be used as a jumping off point to discussions. How could students represent their learning in a way that would support formative feedback opportunities? Could small summative assessment occur at different stages in the teaching sequence?
Read more about using the LIA FrameworkComparing water volume
In this integrate step, guide students to link their experiences in the investigation to the processes of freeze-thaw weathering in real life.
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Teams share the result of their investigations.
Using the QCER framework as a guide, each team makes a claim to answer the question they were investigating: What happens to the volume of water when we change the state of the water from liquid to solid? For example, Water expands and takes up more volume when it changes from a liquid to a solid. Teams support their claim with evidence from their investigation, for example The water in our syringe increased from 5ml as a liquid to 6ml when it froze solid.
Compare to see if each team got the same results and made the same/similar claims. Discuss why this happened, any results that differed, and why they might have differed. Ask students if they would now consider the prediction "water expands when it is frozen" to be shown as true, and what they think broke the glass bottle from the What broke the bottle? Resource sheet.
Using the Think-Pair-Share strategy, ask students to consider how the force created by water physically expanding when it freezes would contribute to weathering.
Show the video Freeze-Thaw Weathering Explained (2:48) so students can generalise what they have learned about water expansion and freeze-thaw weathering of rocks.
Students complete their freeze-thaw weathering diagram on the Freeze-thaw investigation planner Resource sheet.
Discuss the conditions required for freeze-thaw weathering to occur: rain or snow and temperature change that repeatedly goes above and below 0°C. Determine if it is likely for freeze-thaw weathering to occur in your location and why/why not.
Optional: Explore summer images of Blue Lake at Mt Kosciuszko, NSW. Zoom in to see signs of freeze-thaw weathering on the large rock faces and rocky debris on the ground.
Reflect on the lesson
You might:
- add new words and images to the word wall or glossary.
- add to the W and H sections of the TWLH chart.
- ask students to articulate the forces involved when the water volume expands when it freezes.
- discuss how the learning from this lesson relates to freeze-thaw weathering of rocks.
- discuss how students were thinking and acting like scientists during this lesson. Focus on recording, explaining, evaluating data and using scientific diagrams.
Freeze-thaw weathering
What is freeze-thaw weathering and where/when does it occur in Australia?
Freeze-thaw weathering, also known as frost-wedging, is one type of physical weathering. Liquid water seeps into cracks and crevices in rocks, then if the temperature drops low enough, the water freezes and increases in volume, working as a wedge to slowly widen the crack. An increase in temperature causes the water to melt and run deeper into the cracks. The cycle of freezing and melting eventually causes the rock to split.
Some rock debris found high on the slopes of mountains such as Mount Kosciuszko in the Australian Alps and Mount Wellington in Tasmania is the result of freeze-thaw weathering.
In this lesson, students investigate freeze-thaw weathering by measuring and graphing changes in water volume when water changes state from a liquid to a solid in the freezer.
Freeze-thaw weathering, also known as frost-wedging, is one type of physical weathering. Liquid water seeps into cracks and crevices in rocks, then if the temperature drops low enough, the water freezes and increases in volume, working as a wedge to slowly widen the crack. An increase in temperature causes the water to melt and run deeper into the cracks. The cycle of freezing and melting eventually causes the rock to split.
Some rock debris found high on the slopes of mountains such as Mount Kosciuszko in the Australian Alps and Mount Wellington in Tasmania is the result of freeze-thaw weathering.
In this lesson, students investigate freeze-thaw weathering by measuring and graphing changes in water volume when water changes state from a liquid to a solid in the freezer.