The hydrological cycle describes the continuous movement of water on, above, and below the Earth's surface. It involves evaporation of water from oceans, rivers, and land into water vapor in the atmosphere, followed by condensation of water vapor into clouds and precipitation as rain or snow back onto land and oceans, where some infiltrates soil and becomes groundwater, and some runs off into rivers and lakes or returns to the oceans, completing the cycle. The major processes are evaporation, transpiration, condensation, precipitation, infiltration, and runoff, driven primarily by energy from the sun.