It sounds as if you are asking a question related to the theory of Plate Tectonics. Plate subduction and seafloor spreading contribute to the rising and falling of the mantle below the asthenosphere. These forces create convection cells which transfer heat to and from the interior of the earth.
Resources that may help you further:
1. USGS website "Some Unanswered Questions-What Drives the Plates?"
2. Plate Tectonics-The Gale Encyclopedia of ScienceEd. K. Lee Lerner and Brenda Wilmoth Lerner. Vol. 5. 4th ed. Detroit: Gale, 2008. p3391-3399. COPYRIGHT 2008 Gale, Cengage Learning 3. Earth Science: Plate Tectonics: The Unifying Theory of Geology, Ed. K. Lee Lerner and Brenda Wilmoth Lerner. Vol. 2. In Context Series Detroit: Gale, 2009. p710-716. COPYRIGHT 2009 Gale, Cengage Learning page 710
False.
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.
Heat is transferred from the interior to the surface of the Earth through a process called convection. In the Earth's mantle, hot material rises towards the surface, carrying heat with it. This movement creates convection currents that transfer heat from the interior to the surface.
Tectonic Plate Movement
tectonic plate motion
tectonic plate motion
The mantle is responsible for releasing about 80 percent of the heat generated from Earth's interior. This heat is primarily produced by the decay of radioactive elements within the mantle and is transferred to the surface through convection currents and tectonic plate movements.
Heat is transferred through the Earth primarily through conduction, where heat is passed from one particle to another. In the Earth's interior, heat is also transferred by convection, where hot material rises and carries heat with it. Additionally, heat can be transferred through radiation, in which energy is emitted as electromagnetic waves.
Heat within Earth's interior is primarily transferred by conduction, convection, and radiation. Conduction occurs when heat moves through solid materials, such as rocks, by direct contact. Convection involves the movement of molten rock in the mantle, where hot material rises and cooler material sinks, creating currents that transfer heat. Radiation plays a minimal role in the Earth's interior since it is more effective in vacuum conditions rather than through solid materials.
Earth's heat is transferred by convection, which is the movement of heat through a fluid due to differences in temperature. It is also transferred by conduction, which is the direct transfer of heat through a material due to a difference in temperature between two points.
You don't transfer convection. Rather, convection is a process whereby heat energy is transferred.
Heat beneath Earth's surface is transferred primarily through conduction, where heat is transferred from the hot interior of the Earth to the cooler outer layers. This process is aided by the slow movement of molten rock in the mantle, known as mantle convection, which helps distribute heat throughout the planet's interior. Additionally, some heat is also transferred through hot fluids like magma and water moving through fractures and faults in the Earth's crust.