The temperature in the Earth's lower mantle is estimated to be between 1,600 and 2,200 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.
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.
1000-1500 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.
The Earth's mantle temperature ranges from about 500°C to 900°C near the upper boundary, and it can reach up to 3000°C near the lower boundary.
the average temperature for the Earth's lower mantle is 5400 degrees
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.
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 .
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.
1000-1500 degrees Celsius
The asthenosphere is the lower portion of the Earth's mantle. Its temperature ranges from 1000 degrees Celsius to 2500 degrees Celsius.
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.
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.
The temperature can reach 1800 degrees Celsius in the Earth's mantle, specifically in the lowermost part called the lower mantle. This high temperature is due to the immense pressure and heat generated by the movement of tectonic plates and radioactive decay within the Earth's interior.
The Earth's mantle has two main layers: the upper mantle and the lower mantle. These layers are distinguished by differences in their composition, temperature, and behavior. The upper mantle extends from the crust to a depth of about 410 miles (660 kilometers), while the lower mantle extends from about 410 miles (660 kilometers) to approximately 1,800 miles (2,900 kilometers) below the Earth's surface.
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.
The upper mantle is a hot area of earths interior that is less dense than the lower mantle. It goes from 250 kilometers to 600 kilometers or150 miles to 400 miles. Its composition is Silicon Oxygen Iron and Magnesium. It is a liquid.