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 core of the sun is 15 million oK (Kelvin is the scientific scale) and the corona is 5800 oK. The corona is that temperature because sound waves produce intense heat and below the corona and photosphere are convection currents that bring heat to the surface.
It's estimated to be nearly 15 million degrees kelvin (15 million degrees C).
Deep in it's core, the sun is more than ten million degrees.
Sneighke began with: http://en.wikipedia.org/wiki/Sun
10,000 degrees F, the core is 1 million and the corona is 5 million degrees F
The temperature of the sun's core is 15000000° C (27000000° F)
The temperature increases. The average geothermal gradient is 25C/Km
well when you set your microwave to high it is about the same temperature as the surface of the sun but the core can get as hot as an exploding microwaved watermelon
In the center, the temperature is something like 16 million Kelvin. At the surface, almost 6000 Kelvin.
It increases.
From the Earth's crust to the inner core is about 3,950 miles.
When new crust is made, like at a spreading center, old crust must be destroyed, like at a subduction zone, where it is brought back into the inner earth and melted and recycled through.
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.
Density gets higher.
Below the Earth's crust is the mantle and outer and inner core.
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!
pressure decreases
From the Earth's crust to the inner core is about 3,950 miles.
When new crust is made, like at a spreading center, old crust must be destroyed, like at a subduction zone, where it is brought back into the inner earth and melted and recycled through.
Inner core Outer core Mantle Crust Hydrosphere Atmosphere
the break in the inner crust that is not filled with magma is called
Crust, mantle, outer core, inner core
From thick to thin: mantle, outer core, inner core, crust.
The crust is the top layer. Then there is the outer mantle, inner mantle, outer core, and inner core.
The inner core - the centre of earth - is solid and about 780 miles (1,250 km) thick. The inner core may have a temperature up to about 13,000°F (7,200°C = 7,500 K), which is hotter than the surface of the Sun. The inner core (which has a radius of about 750 miles (1,228 km) is solid.The Crust lies above the mantle and is the earth's hard outer shell which is composed of silicon, aluminum, calcium, sodium and potassium.
Crust, Mantle, Outer Core, Inner Core.
The Earth's crust is divided into several major tectonic plates that float on the semi-fluid asthenosphere below. These plates are in constant motion, leading to phenomena like earthquakes and volcanic activity along plate boundaries. The largest plates include the Pacific Plate, Eurasian Plate, and North American Plate.