If convection in the mantle increased, it could lead to more dynamic geological activity at the Earth's surface. This might result in increased volcanic activity and more frequent earthquakes as tectonic plates are pushed and pulled more vigorously. Additionally, the crust could experience more uplift and subsidence in certain areas, potentially altering landscapes and impacting ecosystems. Overall, the increased mantle convection would likely lead to a more geologically active and unstable crust.
Convection
mantle.
The proces is called convection
The circulation within Earth's mantle is called mantle convection. This process involves the movement of hot material rising and cool material sinking in the mantle, creating convection currents that drive plate tectonics.
convection currents in the mantle provide the basic driving forces for plate motions.
Asssasssin crees
the convection currents will stop
convection currents in the upper mantle
Convection in the earth's mantle.
Convection
the heat makes it rise up
Convection
convection currents in the mantle
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 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.
mantle.