Remember that the earth's mantle extends from a few tens of miles below the crust across several thousand miles to near the core. The mantle comprises about 85% of the volume of the earth. The core, you'll recall, is only a bit over 4,000 miles in diameter, and the diameter of the earth is a bit short of 13,000 miles. There's a lot of mantle, isn't there? The mantle is divided into two basic parts, the outer mantle and the mantle (inner mantle).
The temperature around the outer mantle is about 300 to 500 °Celsius. At the outer core where it bounds the mantle, the temperature is a bit short of 4500 °Celsius. That's a big temperature gradient.
You'll find links below to relevant articles, and you'll also find that the data presented varies a bit, as it should. No one has actually been very far "into" the earth, and, though we are a clever lot, we only have a limited way to "look into" the earth and see what's going on. Couple that with what we see looking around out here and you'll get some variation in what is thought to be inside. between 100 to1600 Celsius
the average temperature for the Earth's lower mantle is 5400 degrees
2000 celcius
there are 7 layers in earths mantle.
the mantle
the earth's mantle is brown
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.
mantle
you will find it in earths mantle because it is a kind of an igneous rock
The difference in temperature and density is the cause of convection currents in the earths mantle. Convection currents are the flow that transfers heat within a fluid.
The difference in temperature and density is the cause of convection currents in the earths mantle. Convection currents are the flow that transfers heat within a fluid.
The difference in temperature and density is the cause of convection currents in the earths mantle. Convection currents are the flow that transfers heat within a fluid.
the earths mantle is very hot were cornstarch is not hot at all