convection currents
convection currents
convection currents
convection currents convection currents convection currents
it is water cycle
it is water cycle
water cycle
because of the heat of the place and slow movement of the hydrologic cycle
Heat transfer in the Earth's mantle drives the movement of the Earth's crust through the process of convection. As mantle material heats up, it becomes less dense and rises, causing the overlying crust to move. At the same time, cooler mantle material sinks back down, completing the cycle of heat transfer and driving the continuous motion of tectonic plates.
Earths crust is made of several large tectonic plates. These plates slowly move in three ways. 2 plates may move along side each other, away from each other or toward each other. if 2 plates of equal density collide it will result in rocks being crumpled upward forming mountains. if one plate has less density then the other then the plate with more density will slide beneath the less dense plate
The energy that drives Earth's rock cycle primarily comes from Earth's interior, specifically from the heat generated by radioactive decay in the mantle and core. This heat drives processes like convection currents in the mantle, which in turn contribute to the movement of tectonic plates and the formation of new rocks through processes like melting and solidification.
it is water cycle
The movement between Earth's surface and the air is called the water cycle. This cycle involves the continuous circulation of water through the atmosphere, land, and oceans, driven by processes such as evaporation, condensation, precipitation, and runoff.
Heat from the earth's core causes the mantle to flow in a convection cycle. As the mantle near the core heats up, it rises, carrying heat and causing the plates to move sideways due to drag. As the mantle cools near the surface, it sinks back down, completing the cycle. This continuous flow of heat and movement of the mantle is responsible for the movement of tectonic plates on Earth's surface.
The term for the circular movement of material inside Earth's mantle is convection. This process is driven by heat from the Earth's core, causing molten rock to rise, cool, and then sink back down in a continuous cycle.