The mantle has no huge source of heat of itself. The mantle is in continuous convection, and is also conducting heat from the outer core and in turn from the inner core.
In the core materials, themselves mainly nickel and iron, are also many of the heavy radioactive elements. The radioactive decay of these is the ultimate source of the heat of the Earth's Core. It is believed to have a temperature about the same as the surface of the Sun, over 5000 deg C.
The tremendous heat locked into earth's molten core is continually heating the mantle.
Answer:
There are several factors at play. All of these forces emit heat which transfers to the mantle:
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The Earth's core and mantle would have cooled down by now (4500 million years of cooling) if the heat in the centre were just residual heat from the Earth's formation.
When the Earth was forming and entirely molten, all the heavy elements will have sunk into the core of the planet, separating themselves out into layers of increasing density (this layering would have been disturbed somewhat by convection movements). This would mean that the very heavy radioactive elements would have moved to the core and it is the decay processes of these that is keeping the interior of the earth hot and has been driving plate tectonics and volcanic activity. In essence the planet is a slow fission reactor/bomb.
Also the latent heat of crystallisation of the solid core form the molten core will be releasing heat slowly.
The heat inside Earth primarily comes from two sources: residual heat from its formation, and the decay of radioactive elements in the mantle and core. This heat drives the movement of material in the Earth's interior, creating processes like mantle convection and the generation of Earth's magnetic field.
The Earth's mantle has two main layers: the upper mantle and the lower mantle. These layers are distinguished by differences in their composition, temperature, and behavior. The upper mantle extends from the crust to a depth of about 410 miles (660 kilometers), while the lower mantle extends from about 410 miles (660 kilometers) to approximately 1,800 miles (2,900 kilometers) below the Earth's surface.
Temperature is about 2000 to 3000 degrees celsius maybe less.The mantle is hot but not the hottest layer.It is is the second layer of the Earth. The mantle is the thickest layer of the earth, it is the layer of the earth beneath the crust.Upper mantle and Lower mantle are the two parts of the mantle, The lower mantle is deeper and denser than the upper mantle .
, a liquid outer core that is much less viscous than the mantle, and a solid inner core.
Examples of heat sources could be grouped into two (2) based on there origin. They are; 1. Natural Heat Sources. The natural heat sources could be sub-divided into two; a. External Source, e.g Sun. b. Internal Source, e.g Geothermal, i.e. Magma. 2. Man-made Heat Sources. These includes heat generated from; a. Electricity, e.g Electric Cooker and Oven. b. Fire, e.g Coal.
the mantle plume There are two source of heat in the earth's interior. The main two sources are fire and breathing heat.
The two main sources of Earth's internal heat energy are residual heat from the planet's formation over 4.6 billion years ago and the decay of radioactive isotopes within the Earth's mantle. The heat generated by these processes contributes to the movement of tectonic plates and drives geological activity on the planet.
the mantle plume There are two source of heat in the earth's interior. The main two sources are fire and breathing heat.
Two sources of thermal energy in Earth's interior are residual heat from the planet's formation over 4.5 billion years ago and radioactive decay of elements like uranium, thorium, and potassium within the Earth's crust and mantle.
The two main sources of heat within Earth are primordial heat left over from the planet's formation over 4.5 billion years ago, and radiogenic heat produced by the decay of radioactive isotopes in the mantle and crust. These heat sources drive geological processes such as mantle convection and plate tectonics.
The two main sources of heating in the Earth are radioactive decay of elements like uranium, thorium, and potassium in the mantle, and residual heat from the Earth's formation over 4.5 billion years ago. These heat sources contribute to the movement of tectonic plates and drive processes like mantle convection and volcanic activity.
Beneath the surface of the earth temperature remains the same. Within the Earth, irregular convection cells within the mantle transfer heat from the core to the surface of the planet. Volcanoes and earthquakes are two examples of heat transferring from the interior to the surface.
The heat inside Earth primarily comes from two sources: residual heat from its formation, and the decay of radioactive elements in the mantle and core. This heat drives the movement of material in the Earth's interior, creating processes like mantle convection and the generation of Earth's magnetic field.
The Earth system is powered by energy from two major sources: the Sun and the planet's internal heat.
the sun and the moon
about 1mile or two b4 it gets to the mantle. tys, mii
Yes, the heat source for convection currents in the mantle is primarily from the radioactive decay of elements within the Earth, not the sun. This heat causes molten rock in the mantle to move in convection currents, which in turn drive plate tectonics and other geological processes on the Earth's surface.