The temperature of the Earth's mantle varies with depth, generally ranging from about 500 to 900 degrees Celsius (932 to 1,652 degrees Fahrenheit) near the upper mantle, and increasing to approximately 3,000 degrees Celsius (5,432 degrees Fahrenheit) as one approaches the lower mantle. The exact temperature can vary based on location and geological conditions.
Temperature is about 2000 to 3000 degrees celsius maybe less.The mantle is hot but not the hottest layer.It is is the second layer of the Earth. The mantle is the thickest layer of the earth, it is the layer of the earth beneath the crust.Upper mantle and Lower mantle are the two parts of the mantle, The lower mantle is deeper and denser than the upper mantle .
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.
The lithosphere is the upper portion of the mantle. Its temperature is around 300 to 500 degrees Celsius. The lower portion of the mantle, which is the asthenosphere, has a temperature of around 4500 degrees Celsius.
120-300
The inner mantle, also known as the lower mantle, is a layer of Earth's mantle located beneath the upper mantle and above the outer core. It is primarily composed of solid silicate minerals, such as perovskite and magnesiowüstite, and remains solid due to the immense pressure it experiences. Although it is hot, with temperatures reaching up to 4,000 degrees Celsius (7,200 degrees Fahrenheit), the pressure prevents it from melting. The inner mantle plays a crucial role in the dynamics of plate tectonics and the geologic activity of the Earth.
In Fahrenheit the Earth's mantle is ranged from 1400 degrees to 1600 degrees Fahrenheit.
In Fahrenheit the Earth's mantle is ranged from 1400 degrees to 1600 degrees Fahrenheit.
H'm, i think it is either mantle of mantle and the crust of earth combined .so it is probably mantle
the earth's mantle is in ligiud form because it varys from 1600 to 4000 degrees farinhite .
the average temperature for the Earth's lower mantle is 5400 degrees
The temperature in the Earth's lower mantle is estimated to be between 1,600 and 2,200 degrees Celsius.
700 degrees celsius
The temperature in the Earth's mantle can be anywhere from 500 to 900 degrees Celsius. Closer to the core of the Earth, the temperature can reach 4,000 degrees Celsius.
The temperature of the Earth's mantle can vary but generally ranges between 500 to 900 degrees Celsius near the top (upper mantle) to over 4,000 degrees Celsius near the bottom (lower mantle). This heat comes from the Earth's interior and drives processes like mantle convection and plate tectonics.
1000-1500 degrees Celsius
According to Scientists, the earthâ??s mantle temperature averages between 4,000 to 6,700 degrees Fahrenheit or 2,200 to 3,700 degrees Celsius.
The temperature of the Earth's mantle can range from 1,300 to 2,400 degrees Celsius (2,372 to 4,352 degrees Fahrenheit). These temperatures vary depending on the location within the mantle and can be influenced by factors such as depth and proximity to the core.