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Approximately 5500 K.
Pressure increases significantly, from 10-4 GPa to 24 GPa.
It is characterized by its ability to flow due to high temperatures.
It reaches up to 6371 km.
The inner core is hotter, at about 5500 K.
It is in a liquid state.
Approximately 136 GPa.
The lower mantle has higher pressure and temperature.
About 4300 K.
It is around 410 GPa.