Liquid.
Liquid
The outer core is kept in a liquid state due to a combination of high temperature, estimated to be between 4400°C and 6100°C, and high pressure, estimated to be around 1.4 million atm at the inner boundary with the inner core.
The inner core is solid due to high pressure preventing the temperature from melting the iron-nickel alloy. The outer core is liquid because the lower pressure allows for the metal to remain in a molten state.
At standard temperature and pressure, chlorine will be a gas.
The extremely high pressure at the inner core drives the melting point of the iron and other materials up beyond the temperature of the inner core. Therefore they remain solid. The pressure in the outer core is lower sop the melting point is below the temperature in this region and so it is a liquid.
Liquid
The outer core is kept in a liquid state due to a combination of high temperature, estimated to be between 4400°C and 6100°C, and high pressure, estimated to be around 1.4 million atm at the inner boundary with the inner core.
The inner core is solid due to high pressure preventing the temperature from melting the iron-nickel alloy. The outer core is liquid because the lower pressure allows for the metal to remain in a molten state.
The Earth's inner core is solid despite having higher temperatures than the outer core due to the immense pressure at that depth. The pressure is so high that it forces iron and nickel into a solid state, even at temperatures exceeding 5,000 degrees Celsius. In contrast, the outer core is under lower pressure, allowing the materials to remain in a liquid state. This interplay between temperature and pressure is crucial in determining the physical state of materials within the Earth's interior.
that depends on the temperature and pressure, at room temperature and pressure argon is a gas
At standard temperature and pressure, chlorine will be a gas.
The extremely high pressure at the inner core drives the melting point of the iron and other materials up beyond the temperature of the inner core. Therefore they remain solid. The pressure in the outer core is lower sop the melting point is below the temperature in this region and so it is a liquid.
The outer core is liquid because it is under high pressure which lowers the melting point of the metals present in it. The inner core is solid because the immense pressure at the Earth's center, combined with the high temperature, keeps the iron and nickel in a solid state.
The pressure in Earth's outer core ranges from approximately 1.5 million to 3.5 million times atmospheric pressure at sea level. This immense pressure is generated by the weight of the overlying materials and is crucial for maintaining the liquid state of the outer core, which is primarily composed of molten iron and nickel. The combination of high pressure and temperature in this layer plays a significant role in the generation of Earth's magnetic field.
This depends on the nature of the material, structure, temperature, pressure.
Temperature and pressure
They are in this state due to the high temperatures (they have melted). Also note that they are not liquid in the inner core even at the even higher temperatures because of the intense pressure also acting.