The convection currents will eventaully stop because there is no heat to keep them moving.
When the heat source is removed from a fluid, convection currents in the fluid will eventually slow down and dissipate as the fluid cools. The fluid will then return to a more quiescent state with less movement and mixing.
It'll stop flowing when all of the material has reached th same temperature.
The heat in the Earth's interior comes from two main sources: the radiogenic heat produced by the radioactive decay of isotopes in the mantle and crust and the primordial heat left over from the formation of the Earth.
The heat source that drives convection currents inside the Earth is primarily from the decay of radioactive elements within the Earth's core. This heat causes the material in the mantle to become less dense and rise, creating convection currents that drive the movement of tectonic plates.
Convection currents in the asthenosphere drive the movement of tectonic plates, causing them to slowly drift and interact with each other. This movement leads to various geological processes such as the formation of mountains, earthquakes, and volcanic activity.
When a liquid or gas is no longer heated, the heat source that drives convection currents is removed. As a result, the temperature differential that causes the fluid to circulate diminishes, and eventually the convection currents will slow down and stop as the fluid reaches thermal equilibrium.
When the heat source is removed from a fluid, convection currents in the fluid will eventually slow down and dissipate as the fluid cools. The fluid will then return to a more quiescent state with less movement and mixing.
c. eventually stop. As the heat source is removed, the temperature gradient that drives convection currents diminishes, eventually leading to the cessation of the currents as the fluid reaches thermal equilibrium.
The difference in temperature and density is the cause of convection currents in the earths mantle. Convection currents are the flow that transfers heat within a fluid.
The difference in temperature and density is the cause of convection currents in the earths mantle. Convection currents are the flow that transfers heat within a fluid.
The convection currents running through the asthenosphere are widely believed to be the source of movement of the tectonic plates.
When the heat source is removed from a fluid undergoing convection, the fluid will cool down and convective currents will eventually dissipate due to the diminishing temperature difference that drives the flow. The fluid will likely return to a state of thermal equilibrium.
convection currents
The difference in temperature and density is the cause of convection currents in the earths mantle. Convection currents are the flow that transfers heat within a fluid.
Bad grammar.
It'll stop flowing when all of the material has reached th same temperature.
Convective currents in the fluid will gradually decrease and eventually stop as the fluid returns to a more uniform temperature profile. Without the heat source driving the convection, the fluid will gradually reach thermal equilibrium through conduction.