With all the heat under the crust into the mantle, the hot magma starts to move like any convection current so it goes up and then back around again to be reheated. at the top the convection current is so strong it pulls the plates apart and magma seeps up through and becomes lava.
warm air from ground rises and becomes less dense, goes higher then becomes colder since all the way up there theres no heat source and finally it becomes less dense and falls. this happens in a shape of dual bike tire like patterns. this repeats in a cycle.
when the it goes up it get less dense and when it goes down it still get less dense and it start all over
Convection is simply a heat transfer - for example the act of boiling water, heat is transferred from the cooker to the water container, thus heating the water
In a global convection cell, warm air rises at the equator due to the intense heating from the sun. This rising air then moves towards the poles, gradually cooling and sinking as it does so. The cooled air then flows back towards the equator along the surface to complete the convection loop. This process is responsible for creating and maintaining the global wind patterns and weather systems.
The Coriolis Effect is the phenomenon that effects global winds. A convection cell is a form of wind and this is the first part of the coriolis effect.
convection currents
Convection cycles and the coriolis effect i think.
It is bumping into the lihosphere
The Coriolis Effect is the phenomenon that effects global winds. A convection cell is a form of wind and this is the first part of the coriolis effect.
The Coriolis Effect is the phenomenon that effects global winds. A convection cell is a form of wind and this is the first part of the coriolis effect.
Chuck Norris Google
It turns because a convection cell is one big loop of a convection current
In a global convection cell, warm air rises at the equator due to the intense heating from the sun. This rising air then moves towards the poles, gradually cooling and sinking as it does so. The cooled air then flows back towards the equator along the surface to complete the convection loop. This process is responsible for creating and maintaining the global wind patterns and weather systems.
The Coriolis Effect is the phenomenon that effects global winds. A convection cell is a form of wind and this is the first part of the coriolis effect.
The Coriolis Effect is the phenomenon that effects global winds. A convection cell is a form of wind and this is the first part of the coriolis effect.
I think the convection cell might affect the crust because the convection cell is bigger than the crust.
I think the convection cell might affect the crust because the convection cell is bigger than the crust.
I think the convection cell might affect the crust because the convection cell is bigger than the crust.
I think the convection cell might affect the crust because the convection cell is bigger than the crust.
It refers to a region in which convection occurs.