We call the core of the sun as photo sphere. Its temperature is 14 million kelvin. Where as the outer atmosphere is comparatively cooler with temperature 6000 kelvin. It is named as chroma sphere.
The temperature of the Earth's layers increases from the crust towards the core. The outermost layer, the crust, has the lowest temperature, while the inner core has the highest temperature. This gradient is due to the heat generated by radioactive decay in the core and the residual heat from the Earth's formation.
Pressure increases as we move from the crust towards the inner core of the Earth. This is due to the increased weight of the overlying rock layers exerting greater force on the materials below. The extreme pressure at the Earth's core is a key factor in maintaining the solid state of the inner core despite its high temperature.
The temperature generally increases as you move from the Earth's surface towards the center. The outermost layer, the crust, has variable temperatures. The mantle beneath the crust is solid but can slowly flow, and its temperature increases with depth. The core, consisting of the outer liquid core and the inner solid core, is the hottest layer, with temperatures reaching over 5000 degrees Celsius at the inner core.
Temperature, pressure, and density increase as you move from the Earth's crust to the inner core.
The four main layers of the Earth are the crust, the mantle, the outer core and the inner core. The temperature in the mantle is estimated to be about 1000 degrees Celsius. Temperature in the inner core can reach up to 3700 degrees Celsius.
The temperature of the Earth's layers increases from the crust towards the core. The outermost layer, the crust, has the lowest temperature, while the inner core has the highest temperature. This gradient is due to the heat generated by radioactive decay in the core and the residual heat from the Earth's formation.
Pressure increases as we move from the crust towards the inner core of the Earth. This is due to the increased weight of the overlying rock layers exerting greater force on the materials below. The extreme pressure at the Earth's core is a key factor in maintaining the solid state of the inner core despite its high temperature.
The temperature generally increases as you move from the Earth's surface towards the center. The outermost layer, the crust, has variable temperatures. The mantle beneath the crust is solid but can slowly flow, and its temperature increases with depth. The core, consisting of the outer liquid core and the inner solid core, is the hottest layer, with temperatures reaching over 5000 degrees Celsius at the inner core.
Temperature, pressure, and density increase as you move from the Earth's crust to the inner core.
The density generally decreases as you move from the earth's inner core to the crust. The inner core is the most dense layer, followed by the outer core, mantle, and then the crust. This is due to variations in the composition and temperature of each layer.
The four main layers of the Earth are the crust, the mantle, the outer core and the inner core. The temperature in the mantle is estimated to be about 1000 degrees Celsius. Temperature in the inner core can reach up to 3700 degrees Celsius.
pressure decreases
the inner core has to be really hot so when the hotness reaches the crust it feels normal because if the inner core was a normal temperature that when the hotness gets to the crust it would be freezing!
The Earth's interior has several layers in order from outer to inner: the crust, mantle, outer core, and inner core. These layers vary in composition, temperature, and physical properties.
Inner core Outer core Mantle Crust Hydrosphere Atmosphere
The earth has four layers, the crust, mantle, outer core, and inner core.
As one progresses from the lithosphere towards the inner core of the Earth, the density generally increases. The inner core is the densest layer of the Earth due to the high pressure and temperature conditions, while the lithosphere, being the outermost layer, has lower density materials like rocks and soil.