PRAYOGX Learn · Classes 9–12
Physics

Why Is Ice Slippery?

Key points

  • Pressure melting is the old idea, but a person's weight lowers ice's melting point by only a fraction of a degree, and ice is slippery even near −30 °C.
  • Friction: a sliding skate or shoe heats the surface and melts a thin water film.
  • Premelting (Faraday): a very thin liquid-like layer covers ice even below 0 °C.
  • Newer research suggests loosely bound surface molecules that roll like ball bearings; the full answer is still debated.

Three explanations

IdeaWhat it saysVerdict
Pressure meltingWeight melts the ice under youToo small: lowers the melting point by a fraction of a degree
Frictional meltingSliding heats and melts a thin filmTrue for moving skates and feet
Premelting (Faraday)A liquid-like layer exists on ice below 0 °CConfirmed; explains slipperiness even when standing still

Why pressure is not enough

Pressure lowers ice's melting point by only about 0.0074 °C per atmosphere. Even on a thin skate blade, a person's weight shifts it by a fraction of a degree, yet ice stays slippery at temperatures far below that, around −30 °C.

Still an open question

Experiments show water molecules at the ice surface are loosely bound and mobile. Some researchers describe them as tiny ball bearings; how much each mechanism contributes is still being studied. Science keeps some questions open, and that is part of the fun.

Try it yourself

Goal: Test the pressure-melting idea: find out when your weight could melt ice, and when it never could.

  • Set your mass and choose shoes, skates or one skate edge.
  • Compare your pressure with the red mark, the pressure needed.
  • Try −0.2 °C on a skate edge: when does it work?
  • Make the ice colder and read the mass it would take.

Open the simulation full screen

Quick quiz

4 questions. Choose an answer for each, then submit to see your score and the explanations.