temperatureA measure of how energetic a substance's particles are on average: it tracks their average kinetic energy. A thermometer reports this average, not how much energy the whole sample holds.A thimble of boiling water and a huge pot of boiling water have the same temperature, 100 °C at sea level, because their molecules carry the same average energy of motion.
thermal energyThe sum of the energy of every particle in a sample, from their motion and from how they are arranged against the pulls between them. It depends on how much matter there is, its temperature and its state.The lake at 15 °C holds far more thermal energy than the campfire kettle at 90 °C, because it contains billions of times more water molecules.
heatEnergy that moves from a warmer object or region to a cooler one because of their temperature difference. In science, heat is energy on the move, not something an object stores.Heat flowed from the student's warm hand into the ice cube, so the hand cooled and the ice melted.
kinetic energyThe energy an object or particle has because it is moving. The faster a particle of a given mass moves, the more kinetic energy it has.As the soup warmed, its water molecules gained kinetic energy and moved faster on average.
state changeA change of a substance from one state (solid, liquid or gas) to another. The particles stay the same; only their motion and spacing change. Also called a change of state or phase change.Ice melting into water is a state change, because both are made of the same water molecules.
melting pointThe temperature at which a pure solid turns into a liquid. The liquid freezes at this same temperature. For water it is 0 °C at normal air pressure.Gallium's melting point is about 30 °C, so a piece of it can melt in a warm hand.
boiling pointThe temperature at which a liquid boils, forming bubbles of its own vapor throughout. It depends on air pressure: water boils at 100 °C at sea level and at a lower temperature high in the mountains.Rubbing alcohol boils at a lower temperature than water, since its molecules attract one another less strongly.
evaporationThe change from liquid to gas at a liquid's surface, as the most energetic particles escape. It happens at many temperatures, not only at the boiling point, and it cools the liquid left behind.Evaporation of sweat from your skin carries energy away and cools you, even though the sweat never boils.
condensationThe change from gas to liquid, as gas particles lose energy and their attractions hold them together when they collide. It releases energy to the surroundings.Condensation of water vapor from the air formed the drops on the outside of the cold can.
sublimationThe change from solid straight to gas without becoming a liquid first. Dry ice (solid carbon dioxide) sublimes at normal air pressure; snow can slowly sublime on dry, sunny, windy days.Sublimation shrank the block of dry ice in the cooler, yet it left no puddle.
depositionThe change from gas straight to solid without becoming a liquid first, as when water vapor turns into ice crystals on a surface colder than 0 °C. It releases energy.Deposition of water vapor from the air coated the car windshield with feathery frost overnight.
insulatorA material that slows the transfer of thermal energy. Many insulators, such as foam, wool and bubble wrap, work by trapping still air, which carries energy poorly.The foam cooler is a good insulator, so the ice inside gained energy from the hot beach air very slowly.