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The temperature of the mantle is greater at Point B than Point A. The temperature of the mantle is determined by its depth which is greater at Point B than Point A. The deeper the mantle the hotter and more pressurized it is and so the temperature at Point B will be greater than at Point A.

Temperature can also be affected by other factors such as the composition of the mantle and the presence of radioactive elements. In this case since both points are in the same area and have similar composition the temperature will be determined by the depth.

To summarize the temperature of the mantle is greater at Point B than Point A because it is deeper and thus more pressurized and hot.

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Alvah Stokes

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Related Questions

Where is the temperture of the mantle material greater at point B or point C?

The temperature of mantle material is generally greater at point B, which is closer to the Earth's core. As we move away from the core towards the Earth's surface (point C), the temperature tends to decrease.


Where is the density of the mantle material greater at point A or point B?

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Where is the density of the material greater at point B or point C explain why?

To determine where the density of the material is greater, we need to consider factors such as pressure, temperature, and composition at points B and C. Generally, if point B is deeper within a material or subjected to higher pressure than point C, it will likely have a greater density due to the compression of particles. Conversely, if point C is at a higher temperature or in a less compact state, its density may be lower. Thus, without specific information about the conditions at points B and C, we cannot definitively conclude which has greater density.


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