How does the temperature of the Earth's mantle compare to the other layers of the Earth? The mantle is the same temperature as the core

To compare the temperature of the Earth's mantle with the other layers, we need to look at the structure of the Earth, which consists of the crust, mantle, outer core, and inner core. Here are the approximate temperature ranges for each layer: 1. **Crust**: The temperature in the Earth's crust varies widely, typically ranging from about 0°C to 1,000°C, depending on depth and location. 2. **Mantle**: The temperature of the mantle increases with depth, ranging from about 500°C near the crust to approximately 4,000°C at the boundary with the outer core. 3. **Outer Core**: The outer core is liquid and has temperatures ranging from about 4,000°C to 6,000°C. 4. **Inner Core**: The inner core is solid and has temperatures that can reach up to about 5,000°C to 7,000°C. From this comparison, we can conclude that: - The mantle is significantly cooler than the outer core and inner core. - The mantle's temperature is higher than that of the crust but lower than that of the outer and inner cores. Therefore, the statement "The mantle is the same temperature as the core" is incorrect. The mantle is cooler than the core.