2000 celcius
The temperature of a plastic mantle can vary depending on its usage. When used for heating purposes, the mantle typically reaches temperatures between 200-500 degrees Celsius. It is important to always follow manufacturer's guidelines and safety precautions when using a plastic mantle.
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.
The arrows shown in the asthenosphere represent the inferred slow circulation of the plastic mantle by a process called mantle convection. This process involves the movement of heat from the Earth's core towards the surface, creating a pattern of circulation that drives plate tectonics and other geologic phenomena.
It's only soft and plastic in that it is not as hard as the brittle rock of the crust and uppermost mantle.
The mantle is inferred to have convection currents that cause tectonic plates to move. Heat from within the Earth creates these currents, leading to the movement of the rigid plates on the Earth's surface.
The temperature of a plastic mantle can vary depending on its usage. When used for heating purposes, the mantle typically reaches temperatures between 200-500 degrees Celsius. It is important to always follow manufacturer's guidelines and safety precautions when using a plastic mantle.
Stiffer mantle.
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.
The temperature in Earth's plastic mantle, which is part of the upper mantle, is typically inferred to range from about 500 to 900 degrees Celsius (932 to 1,652 degrees Fahrenheit) near the lithosphere-asthenosphere boundary. As you go deeper into the mantle, temperatures can increase significantly, reaching up to 3,000 degrees Celsius (5,432 degrees Fahrenheit) near the core-mantle boundary. These temperatures are crucial for the ductility of the mantle material, allowing for the slow convection processes that drive plate tectonics.
thez nuts
The arrows shown in the asthenosphere represent the inferred slow circulation of the plastic mantle by a process called mantle convection. This process involves the movement of heat from the Earth's core towards the surface, creating a pattern of circulation that drives plate tectonics and other geologic phenomena.
The inferred temperature at the interface between the stiffer mantle and the asthenosphere is closest to approximately 1300 to 1500 degrees Celsius (2372 to 2732 degrees Fahrenheit). This temperature range is crucial for the behavior of the asthenosphere, as it becomes partially molten and more ductile, allowing for mantle convection and tectonic plate movement.
the average temperature for the Earth's lower mantle is 5400 degrees
The asthenosphere is a plastic layer of rock located in the upper mantle, below the lithosphere (earth's crust and uppermost mantle). It is responsible for the movement of tectonic plates due to its partially molten and ductile nature.
It's only soft and plastic in that it is not as hard as the brittle rock of the crust and uppermost mantle.
The mantle is inferred to have convection currents that cause tectonic plates to move. Heat from within the Earth creates these currents, leading to the movement of the rigid plates on the Earth's surface.
It is the mantle that is inferred to have convection currents that cause tectonic plates to move. Heat from the Earth's core creates these currents, which drive the movement of the rigid plates on the Earth's surface.