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.
The Earth's interior is made up of four layers, the crust, mantle, outer core and the inner core. In the mantle, temperatures range between 500 to 900 degrees Celsius at the upper boundary with the crust; to over 4,000 degrees Celsius at the boundary with the outer core.
Earth's mantle reaches temperatures of about 3700°C.
The Earth's mantle has a wide range of temperatures, ranging from 500 to 900 degrees Celsius (932 to 1652 degrees Fahrenheit) near the upper boundary with the crust, to approximately 4,000 degrees Celsius (7,232 degrees Fahrenheit) near the boundary with the outer core.
1000-1500 degrees Celsius
is the mantle hotter or colder the the inner core
the average temperature for the Earth's lower mantle is 5400 degrees
Anywhere from 932 to 1652 degrees Fahrenheit.
The mantle is hot, with temperatures ranging from about 500 to 900 degrees Celsius. This heat is primarily generated by the radioactive decay of elements within the Earth's interior, as well as residual heat from the Earth's formation.
The upper layer of the Earth of how I'd describe is It's hot and is 1000 degrees
The Earth's interior is made up of four layers, the crust, mantle, outer core and the inner core. In the mantle, temperatures range between 500 to 900 degrees Celsius at the upper boundary with the crust; to over 4,000 degrees Celsius at the boundary with the outer core.
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 .
Earth's mantle reaches temperatures of about 3700°C.
In Fahrenheit the Earth's mantle is ranged from 1400 degrees to 1600 degrees Fahrenheit.
A mantle is a layer of hot rocks.
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.
In Fahrenheit the Earth's mantle is ranged from 1400 degrees to 1600 degrees Fahrenheit.
The Earth's mantle has a wide range of temperatures, ranging from 500 to 900 degrees Celsius (932 to 1652 degrees Fahrenheit) near the upper boundary with the crust, to approximately 4,000 degrees Celsius (7,232 degrees Fahrenheit) near the boundary with the outer core.