Activity
MEL Science
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Water at −15 °C is a solid (ice).
40 particles
| State | Shape | Volume | Particles | Motion | Examples |
|---|---|---|---|---|---|
| Solid | Keeps its own shape | Fixed | Packed tightly in a pattern | Vibrate in place | Ice, a rock, a pencil |
| Liquid | Takes the shape of its container | Fixed | Close together, not in a pattern | Slide past each other | Water, milk, juice |
| Gas | Fills its whole container | Fills its whole container | Far apart | Move fast in all directions | Steam, air, helium in a balloon |
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Drag the temperature slider. Watch ice melt at 0 °C and boil at 100 °C, or switch to dry ice and watch it sublimate at −78.5 °C.
Start the quiz. The readouts hide and the box jumps to a mystery temperature; name the state from how the particles move.
Tap the numbered pins on the phase-change diagram to read about melting, freezing, evaporation, condensation, sublimation and deposition.
Drag the names onto the diagram, then heat an ice cube one step at a time in Order it.
Turn a glass box of particles with your finger, change the temperature, and take the guided tour of every phase change.
Everything around you is matter: anything that has mass and takes up space. Your desk, the water in your glass and the air you breathe are all matter. Matter is made of tiny particles (atoms and molecules) far too small to see, and how those particles are arranged and how they move decides the matter's state.
The three states you meet every day are:
NASA's Glenn Research Center sums it up: a solid holds its shape and its volume is fixed; a liquid takes the shape of its container but has a fixed volume; a gas fills its container, taking both the shape and the volume of the container.
The simulation above shows 40 particles of water. Drag the temperature slider and watch them go from a vibrating crystal (ice) to a sloshing puddle (liquid water) to a buzzing swarm (water vapor).
| Solid | Liquid | Gas | |
|---|---|---|---|
| Shape | Keeps its own shape | Takes the shape of its container | Fills its container |
| Volume | Fixed | Fixed | Fills its container |
| Particles | Packed tightly in a pattern | Close together, not in a pattern | Far apart |
| Motion | Vibrate in place | Slide past each other | Move fast in all directions |
| Can it flow? | No | Yes | Yes |
| Can you squeeze it smaller? | Hardly at all | Hardly at all | Yes, easily |
| Examples | Ice, a rock, a pencil | Water, milk, juice | Steam, air, helium |
Liquids and gases are both called fluids because they can flow. Gases are the only state you can easily squeeze into a smaller space, because their particles have so much room between them. That's how a bike pump packs air into a tire.
Particles are always moving, even in a solid. The hotter something is, the faster its particles move. That one idea explains every state:
Changing from one state to another is called a phase change (or change of state). Three of them happen when matter gains heat, and three when it loses heat:
| Phase change | From → to | Heat | Everyday example |
|---|---|---|---|
| Melting | Solid → liquid | Added | An ice cube melting in a drink |
| Freezing | Liquid → solid | Removed | Water turning to ice in the freezer |
| Evaporation (boiling) | Liquid → gas | Added | A puddle drying up; a pot boiling |
| Condensation | Gas → liquid | Removed | Drops on a cold glass; dew on grass |
| Sublimation | Solid → gas | Added | Dry ice "smoking"; snow vanishing on a dry, windy day |
| Deposition | Gas → solid | Removed | Frost on a window; snowflakes |
In the phase-change diagram, heating arrows are solid and cooling arrows are dashed. Each pair are opposites: melting and freezing, evaporation and condensation, sublimation and deposition.
When a solid warms up, its particles vibrate harder and harder. At the melting point, they shake loose from their pattern and the solid becomes a liquid. Ice melts at 0 °C (32 °F). Cool the liquid back down and it freezes at the same temperature, the freezing point.
Something surprising happens at the melting point: while ice is melting, its temperature stays at 0 °C until it has all melted. The heat is busy pulling particles out of their pattern instead of making them faster. The USGS gives the numbers for water: it takes 80 calories to melt one gram of ice, but only 100 more to heat that water all the way to boiling.
Water also has a famous quirk. Most substances shrink when they freeze, but water expands, so ice is less dense than liquid water and floats. If ice sank, lakes would freeze from the bottom up.
Evaporation happens when the fastest particles at the surface of a liquid escape into the air as a gas. It happens at any temperature, which is why a puddle dries on a cool day, just more slowly. Boiling is evaporation turned all the way up: at the boiling point, 100 °C (212 °F) for water at sea level, bubbles of vapor form all through the liquid. Water boils at a lower temperature on a high mountain, where the air pressure is lower.
Turning liquid water into vapor takes a lot of energy. The USGS gives 540 calories per gram, more than six times what it takes to melt ice. That's why sweating cools you down: as sweat evaporates, it carries heat away from your skin.
Condensation is the reverse. When a gas cools, its particles slow down and clump into drops of liquid. NOAA explains that condensation happens when there is more water vapor than the air can hold at its current temperature. It makes clouds, fog, dew and the drops on the outside of a glass of ice water, and it's a key step in the water cycle.
Some solids skip the liquid state entirely. Sublimation is a solid turning straight into a gas. The USGS describes it as the conversion between the solid and the gaseous phases of matter, with no intermediate liquid stage. Dry ice, frozen carbon dioxide, sublimates at −78.5 °C (−109.3 °F), which is why it makes a cold, smoky fog instead of a puddle. Choose Dry ice in the simulation and warm it past −78.5 °C to watch the particles fly straight out of the solid.
Snow and ice can sublimate too. The USGS notes it happens most with low humidity, dry winds, strong sunlight and low air pressure, such as high on Mount Everest, and that warm, dry chinook winds can make snow disappear in the American West.
Deposition is the reverse: a gas turning straight into a solid. The USGS gives snowflakes and frost as examples. On a cold, clear night, water vapor in the air can deposit as feathery frost on a car window without ever becoming liquid.
For everyday life, three: solid, liquid and gas. But scientists recognize more.
Pressure matters too, not just temperature. Earth's inner core is hotter than its outer core, yet National Geographic explains that the inner core stays solid because the pressure is so immense. See it in our layers of the Earth explorer.
A phase change is a physical change. The particles themselves don't change; only how they are arranged and how fast they move. Ice, liquid water and steam are all the same substance, H₂O, and you can turn one into another and back again. A chemical change, like burning wood or baking a cake, makes new substances that can't simply be turned back.
After the activities, try the Guess the state quiz in the simulation, then print the states of matter chart for a science notebook or the states of matter worksheet for review.
Select Open in 3D to see 64 particles in a glass box over a heater, with a thermometer beside it. Drag the Temperature slider and watch the crystal shake apart into a liquid, then boil into a gas that fills the box. Switch to dry ice to see sublimation, or take the guided tour, which stops at each state and each phase change and runs the change for you. The 3D model uses the same particle rules as the 2D simulation. If your device can't show 3D graphics, the page shows the 2D simulation instead.
States of matter connect to almost every other science topic, from the water cycle to cooking and weather. If you want a full course that builds on them, compare the options in our best homeschool science curriculum guide or browse science programs, many of which families can pay for with a state scholarship or education savings account.
Three are common in everyday life: solid, liquid and gas. Plasma is a fourth state, found in stars, lightning and neon signs, and scientists have made others in labs, such as Bose-Einstein condensates at temperatures near absolute zero.
Plasma. Britannica notes that nearly all the visible matter in the universe is plasma, because stars like the Sun are made of it. On Earth, solids, liquids and gases are far more common.
No. Melting, freezing, boiling and the others are physical changes. NASA's states of matter page makes the same point: water is still water whether it is ice, liquid or vapor, and you can change it back.
Water is unusual: it expands when it freezes, so ice is less dense than liquid water. That's why ice cubes float and ponds freeze from the top down, which protects fish in the water below.
100 °C (212 °F) at sea level. Higher up, where the air pressure is lower, water boils at a lower temperature, which is why cooking times on high mountains are longer.
Yes, in any browser that supports WebGL, which includes current Chromebooks, iPads and most phones. If 3D graphics are turned off, the page shows the 2D simulation and diagram instead.