Drop the cube
An ice cube in lemonade
Plop!
Drop the ice cube, or drag it under and let go. Where does it end up?
Drop the cube or push it under: it settles with about about 90% submerged.
Drop the ice. Does it sink or float?
Your turn
Each lab is one step from the video. Change things and see what happens.
Each lab isolates one part of the story. Molecule counts are small, the lattice is drawn flat (real ice is 3D), and the lake temperatures are a simplified model.
Tap the buttons and slide the sliders.
Drop the ice cube, or drag it under and let go. Where does it end up?
Drop the cube or push it under: it settles with about about 90% submerged.
Drop the ice. Does it sink or float?
Pick a liquid. How deep does the ice block sit, and when does it sink?
Compare the submerged fraction ρ(ice)/ρ(liquid) in four liquids.
Turn the heat up or down and watch the hydrogen bonds snap and re-form.
Change the temperature: faster motion, faster hydrogen-bond turnover.
Make the water hot or cold. Watch the tiny bits wiggle!
Drag the temperature below zero, then warm it up. Watch the box grow and shrink.
Freeze and melt the lattice; the frame shows the ~9% volume change.
Make it freezing. The bits hold hands in rings!
Slide through the winter, then flip the rule so ice sinks.
Step through autumn turnover and winter stratification, then try a world where ice sinks.
Slide to winter. Where does the ice go?
Push the iceberg under and let go, or freeze the pipe.
Displace the iceberg and watch it return to ~90% submerged; freeze the pipe (9% expansion).
Drop an ice cube in a drink. It pops back up and floats! Most things sink when they freeze, but ice floats.
Water is made of tiny bits, much too small to see. Each bit has a big ball and two small balls, in a V shape.
In runny water, the tiny bits wiggle and bump. They are all squashed up close.
When water freezes, the bits hold hands in rings. Every ring has a hole in the middle. So ice needs more room, and it is lighter than water. That is why it floats!
In winter, ice floats on top of a pond like a lid. Under the lid, the water stays runny, and the fish swim all winter.
How does salt melt ice? · How is snow made? · Why is the sea salty? · ← More explainers
Ice floats because it is less dense than liquid water.1 A cubic centimetre of ice weighs about 0.92 grams, while the same cube of water weighs about 1.00 gram.61 Anything that is less dense than the liquid around it floats.7
The surprising part is why ice is lighter. When water freezes, hydrogen bonds lock its V-shaped molecules into an open hexagonal lattice, a honeycomb with empty space in every ring.34 The molecules end up farther apart than in the liquid, so the density drops by about 9 percent.12
For most substances, the solid is denser than the liquid. As a liquid cools, its molecules slow down and pack more tightly, so the solid sinks in its own liquid.2
Water does the opposite. It expands when it freezes. The same water takes up about 9% more space as ice, which is why a full ice tray bulges and why frozen pipes can burst.112
Density is how much mass is packed into each bit of space: density = mass ÷ volume. Here is how ice compares with some common liquids:681
| Substance | Density (g/cm³) | Does ice float in it? |
|---|---|---|
| Ice (at 0 °C) | 0.917 | — |
| Olive oil | 0.92 | Only just: almost fully under |
| Alcohol (ethanol) | 0.79 | No, ice sinks |
| Fresh water (at 4 °C) | 1.000 | Yes, about 92% under |
| Fresh water (at 0 °C) | 0.99987 | Yes |
| Sea water | 1.025 | Yes, about 89–90% under |
| Glycerin | 1.26 | Yes, only about 73% under |
How deep a floating object sits tells you its density. By Archimedes' principle, the fraction underwater equals the object's density divided by the liquid's density.7
fraction under = 0.917 ÷ 1.00 ≈ 92%
A water molecule is one oxygen atom joined to two hydrogen atoms, bent at an angle of about 105°, like a V.3 The oxygen end carries a slight negative charge and the hydrogen ends carry slight positive charges.2
Opposite charges attract, so the hydrogen of one molecule is pulled toward the oxygen of a neighbour. This attraction is called a hydrogen bond.2 It is much weaker than the bonds inside a molecule, only about 5 to 10% as strong.5
In liquid water, the molecules are moving so fast that hydrogen bonds constantly break and re-form.3 Because no bond lasts, molecules can tumble around and crowd close to each other.
As water freezes, the molecules slow down enough for the hydrogen bonds to hold. Each molecule links to four neighbours, and together they form an open lattice of six-sided rings.34 (The four neighbours are arranged in 3D, like the corners of a pyramid. From above, the pattern looks like a honeycomb.) That rigid, open structure holds the molecules farther apart than in the liquid, leaving empty space in the middle of every ring.23 More space for the same molecules means lower density, so ice floats.
Most liquids get denser all the way down to their freezing point. Water gets denser as it cools only until about 4 °C (39 °F), where it hits its maximum density.1 Between 4 °C and 0 °C, some molecules already start forming open, ice-like arrangements, so the water expands again and gets lighter.4
In autumn, the surface of a lake cools first. Cold surface water is denser, so it sinks, and warmer water rises to take its place. This mixing goes on until the whole lake reaches about 4 °C.1
After that, the surface water keeps cooling, but now it gets lighter, so it stays on top. The surface reaches 0 °C and freezes first, while the bottom stays near 4 °C.1 The floating ice works like a lid that insulates the water below, so fish and plants survive the winter.23
If ice sank, or if water were densest at its freezing point, lakes could freeze from the bottom up.1 That's why the odd behaviour of one small molecule matters so much for life on Earth.
Icebergs are chunks of freshwater ice that broke off glaciers, which formed from snow falling on land.11 They float in salty sea water, which is a bit denser than fresh water (about 1.025 g/cm³).6 Using the float rule, 0.917 ÷ 1.025 ≈ 0.89, so roughly nine-tenths of the ice sits below the waterline. NASA puts it as "as much as 90 percent of any iceberg lies below the sea surface."9 That hidden bulk is what makes icebergs so dangerous to ships. In April 1912, the Titanic hit one and sank.10
Because water expands as it freezes, ice forming inside a closed pipe pushes hard on the walls. The American Red Cross warns that this pressure can break metal or plastic pipes, no matter how strong they are.12
Salt lowers the temperature at which water freezes, which is why towns spread it on icy roads: how does salt melt ice. Snowflakes are ice too, grown from vapour into six-sided crystals high in the clouds: how does snow form. And icebergs float in sea water that is salty for a reason of its own: why is the ocean salty.
Ice is less dense than liquid water. When water freezes, its molecules lock into an open, honeycomb-shaped crystal with empty space in every ring. The same amount of water takes up about 9% more room, so a cube of ice weighs less than the same-sized cube of water, and it floats.
First, ice is less dense than liquid water (about 0.92 g/cm³ versus about 1.00 g/cm³), and anything less dense than the liquid around it floats. Second, the reason it is less dense: hydrogen bonds hold the molecules in ice in an open hexagonal pattern, farther apart than in the liquid.
In liquid water, hydrogen bonds keep breaking and re-forming, so molecules can crowd close together. In ice, every molecule is held by hydrogen bonds to four neighbours in a rigid, open lattice of six-sided rings. That lattice has more empty space, so the density drops by about 9%.
Ice (about 0.92 g/cm³) is less dense than water (about 1.00 g/cm³) but denser than pure alcohol (about 0.79 g/cm³). An object floats only in a liquid that is denser than it is, so ice floats in water and sinks in alcohol.
The liquid is less dense than ice. That happens in pure alcohol, for example. Ordinary ice in ordinary water always floats. Special 'heavy ice' made from heavy water is denser than normal water and does sink.
A floating object sinks until it pushes aside its own weight of liquid, so the fraction underwater equals its density divided by the liquid's density. Ice is about 90% as dense as sea water, so about nine-tenths of an iceberg sits below the surface.
Water is densest at about 4 °C. As a lake cools below that, the colder water becomes lighter and stays at the surface, where it freezes. The floating ice then acts like a lid that helps keep the water below from freezing, so fish survive the winter.