The inner core of the Earth is solid due to high pressure pushing in on it from all directions, which prevents it from melting even though it is extremely hot. The heat generated by the decay of radioactive elements also helps maintain the inner core's solid state.
The phase changes of matter are melting (solid to liquid), freezing (liquid to solid), vaporization (liquid to gas), condensation (gas to liquid), sublimation (solid to gas), and deposition (gas to solid). These transitions occur due to changes in temperature and pressure.
When you cool a liquid and it changes phase, it becomes a solid.
The inner core of the Earth is solid due to the immense pressure that exists in the center of the planet. Although the temperature is extremely high, reaching up to 5,700 degrees Celsius (10,300 degrees Fahrenheit), the pressure keeps the iron and nickel in a solid state.
The inner core is solid because of the immense pressure at that depth, which keeps the iron and nickel in a solid state despite the high temperatures. In the outer core, where pressure is slightly lower, the higher temperatures cause the iron and nickel to be in a liquid state.
The change is called melting.Another term is liquefaction.
The high pressure at the center of the Earth keeps the inner core in a solid phase, despite the extreme temperatures. The pressure prevents the iron in the inner core from melting, maintaining its solid structure.
The inner core of the Earth is believed to be a solid, composed mainly of iron and nickel. The intense pressure at the Earth's core keeps it in a solid state, despite the high temperatures.
The earth's inner core is solid composed of nickel iron alloy. It is solid despite the very high temperature because of the very high pressure.
The phase changes of matter are melting (solid to liquid), freezing (liquid to solid), vaporization (liquid to gas), condensation (gas to liquid), sublimation (solid to gas), and deposition (gas to solid). These transitions occur due to changes in temperature and pressure.
Phase changes requiring the addition of heat energy are the phase changes from solid to liquid, liquid to gas, and solid to gas. These phase changes are termed melting (solid to liquid), evaporation (liquid to gas), and sublimation (solid to gas).
The inner core of Earth is believed to be in a solid state, primarily composed of iron and nickel. This solid inner core is surrounded by a liquid outer core, which is responsible for generating the planet's magnetic field through convection currents and the movement of molten metal. The extreme pressure at the center of the Earth keeps the inner core solid despite the high temperatures.
Liquid to solid is a phase change.
The inner core is solid.
Earth's inner core is solid.
When you cool a liquid and it changes phase, it becomes a solid.
The inner core of the Earth is solid, honey. It's hotter than a summer day in Death Valley, but the pressure down there is so intense that it keeps it solid. Think of it like trying to melt a popsicle in a sauna - not gonna happen.
The liquid to gas phase change is vaporizing; the reverse is condensing. The other phase changes are: - solid to liquid: melting - liquid to solid: freezing - solid to gas: sublimation - gas to solid: deposition