High temperature and high pressure are inferred to occur within Earth's stiffer mantle. As depth increases in the mantle, both temperature and pressure increase. This combination of high temperature and pressure allows for the solid rock to exhibit ductile behavior, resulting in the flow of solid material over long periods of time.
Stiffer mantle.
The pressure of 1.0 million atmospheres is inferred to be in the inner core of Earth. The inner core is a solid layer composed mostly of iron and nickel under extremely high pressure due to the surrounding layers of Earth exerting force on it.
The temperature range within the stiffer mantle is between 500 and 900 degrees Celsius. This region is known as the upper mantle and is composed of solid rock that can deform under high pressure and temperature.
The pressure within the stiffer mantle ranges from about 14 GPa (gigapascals) at the upper boundary to over 136 GPa at the core-mantle boundary. This high pressure contributes to the solid-state behavior of the mantle material despite its high temperature.
The temperature at the boundary between the asthenosphere and the stiffer mantle is estimated to be around 1300-1400 degrees Celsius. This is where the rock starts to become more rigid due to the increase in temperature and pressure as you move deeper into the Earth.
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Stiffer mantle.
Stiffer mantle.
The pressure of 1.0 million atmospheres is inferred to be in the inner core of Earth. The inner core is a solid layer composed mostly of iron and nickel under extremely high pressure due to the surrounding layers of Earth exerting force on it.
The temperature range within the stiffer mantle is between 500 and 900 degrees Celsius. This region is known as the upper mantle and is composed of solid rock that can deform under high pressure and temperature.
is the temperature if the stiffer mantle above or below its melting point
is the temperature if the stiffer mantle above or below its melting point
is the temperature if the stiffer mantle above or below its melting point
The pressure within the stiffer mantle ranges from about 14 GPa (gigapascals) at the upper boundary to over 136 GPa at the core-mantle boundary. This high pressure contributes to the solid-state behavior of the mantle material despite its high temperature.
The temperature at the boundary between the asthenosphere and the stiffer mantle is estimated to be around 1300-1400 degrees Celsius. This is where the rock starts to become more rigid due to the increase in temperature and pressure as you move deeper into the Earth.
Its about .1 to 1.5 million atmosheres.
Its about .1 to 1.5 million atmosheres.