Yes. It's true that slow movements of mantle rock called convection transfer heat in the mantle
No, the main heat source for the mantle (as well as the core) is radioactive decay of elements like uranium within the mantle itself (or core, respectively). Heat rising from the core into the already hot mantle does set up the differential heat profile that drives much of the mantle convection, but even without the additional core heat the mantle would convect (but slower) so that its heat would rise to the crust.
The hottest part of the mantle is believed to be near the core-mantle boundary, where temperatures can reach up to 4000 degrees Celsius. This intense heat is due to the heat generated by the Earth's core and the slow heat conduction through the solid rock of the mantle.
The heat source for the convection currents in the mantle is primarily the heat leftover from Earth's formation and the heat produced by radioactive decay of elements within the mantle. The heat from the Sun does not directly drive mantle convection, although it does play a role in surface processes like weather and climate.
The moons heat does pass through the mantle but it hardly makes heat. its is mostly cold day and night.
No, slow movements of mantle rock called convection transfer heat in the mantle. Convection occurs due to the heat generated by the radioactive decay of elements in the mantle causing molten rock to rise and cooler rock to sink in a continuous cycle.
Hotspots and geysers transfer heat from the Earth's mantle to the Earth's surface.
Convection currents in the mantle are mainly caused by the heat generated from the radioactive decay of elements within the Earth's interior. This heat creates temperature differences in the mantle, causing warmer, less dense rock to rise and cooler, denser rock to sink, driving the movement of mantle material in a continuous cycle.
radioactivity
Geologists believe that the upper mantle portion of the asthenosphere is primarily heated by the residual heat left over from the formation of the Earth, known as radiogenic heat. This heat is generated by the decay of radioactive isotopes present in the mantle. Other sources of heat include the heat transferred from the core and the heat produced by ongoing mantle convection.
The source of heat in the mantle primarily comes from the decay of radioactive elements like uranium, thorium, and potassium. This process releases energy in the form of heat which contributes to the high temperatures within the Earth's mantle.
Heat in the Earth's mantle is a driving force behind hotspots and geysers. Hotspots are areas where magma plumes rise from the mantle, creating volcanic activity at the surface. Geysers are hot springs that erupt periodic jets of water and steam due to the heating of groundwater by magma and heat from the mantle. Both hotspots and geysers stem from the heat within the Earth's mantle that affects the surface geology.