The heat is derived from initial impacts during Earth's accretionary past, from pressure of overlying material, and from the decay of radioactive material. Keeping it hot has mainly been a function of the radioactive decay and the insulation created by the size of the planet.
The geothermal gradient is expressed as an increase in temperature with a corresponding increase in depth from the surface. Magma formation occurs at depth and slowly lowers in temperature as it rises to the surface. The source of the heat that relates to the geothermal gradient is due to radioactive decay, gravitational friction, and remnant heat from Earth's formation.
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Thx Alot
I belive that Nuclear reactions in the earth's core heats magma.
Some belive that friction of iron in the earth's core due to rotations of earth.
After lava comes to the surface of the Earth is cools off, thus does not stay hot. While still in the Earth it is kept hot by the Earth's core.
Radiation keeps magma hot of course
The innermost layer, the inner core, is very hot but not molten.
The pressure from the outer core, mantle, and crust sqeeze it to a solid although is is fiery hot.
27 MILLION degrees Farenheight way way way hotter than Venus's surface and Earth's CORE!
Planets are, in general, by-products of the birth of a star. As the stars form from accretion, so do the planets. Heavy elements like iron and even the heaviest elements at the upper end of the periodic table can become part of a planet's core. The core of a planet usually exists of these heavy elements. The pressure and isolation from the upper layers of the planet cause the core to stay molten and hot. Though not all planetary cores are hot, some are, and we might look at Earth to figure out how a planet's core gets hot. There are three things that contribute to the Earth's core temperature. The original formation of the Earth by accretion created heat when gravity compressed the material. We also see that bombardment of the planet by asteroids and other matter which created tremendous heat which has not completely cooled. In the case of the earth, the major impact that formed the moon would have re-melted the surface if it had begun to solidify at that point. The other sources of heat are the friction/movement of the various parts and substances. This can be due to crustal shift or the strong gravity of a nearby mass periodically compressing the planet. The is also the fact that the primary source of Earth's core heat (90+%) is from the radioactive decay of radioactive materials in the core. A planet's core is hot because of residual heat of formation, or from friction generated by repeated compression by a nearby massive body, or from impacts of other bodies, or from the natural shifts of crustal material, or from the decay of radioactive materials within it.
Under neathe Hell is nothing because Hell is in the core\middle of the earth. S o in Hell it is very hot:(
The outer core is the only molten layer of the Earth. == ==
The innermost layer, the inner core, is very hot but not molten.
magma
Among other things, it keeps the core hot (and molten).
the outer core
Earth's core is an essential part of it, it also has molten parts or components. So, yes, it's hot. :)
The earth's core contains radioactive elements and as these decay they release heat. This heat keeps the earth's core hot.
For sure. It was almost like a molten lava planet. It was so hot, that heavier elements like iron sunk to to core of the Earth.
Understanding that the core of the Earth is still hot and semi-molten.
Yes, to the best of our understanding it is made of molten Iron.
outer core
The center of the earth is the core. It is full of molten hot magma. It is generally pictured as red when seen in drawings.