Seafloor spreading
Cold Front (:
Low pressure
Harry hess' hypothesis was hot/less dense material rises up the Earth's crust toward the mid-ocean ridges. When the seafloor breaks apart, magma is forced upward and through the cracks. It cools, and becomes a new seafloor. When it moves away from the mid-ocean ridge, it becomes denser and sinks. This helps form ridges.
Warm air :d
The tornado is not a direct result of the interacting air masses. When a warm and cold air mass collide the warm air, being less dense, is forced upward. If the warm air mass is unstable enough, this upward forcing triggers the formation of thunderstorms. If other conditions are right, these storms may go on to produce tornadoes.
pressure
WARM
Cold Front (:
Harry hess' hypothesis was hot/less dense material rises up the Earth's crust toward the mid-ocean ridges. When the seafloor breaks apart, magma is forced upward and through the cracks. It cools, and becomes a new seafloor. When it moves away from the mid-ocean ridge, it becomes denser and sinks. This helps form ridges.
Low pressure
Basaltic magma is forced upward in a vent
The results of air being forced upward is rising temperature. If air is pressurized it gets warm because the particles have to move more quickly.
dr
fold mountain
Harry hess' hypothesis was hot/less dense material rises up the Earth's crust toward the mid-ocean ridges. When the seafloor breaks apart, magma is forced upward and through the cracks. It cools, and becomes a new seafloor. When it moves away from the mid-ocean ridge, it becomes denser and sinks. This helps form ridges.
Warm air :d
The tornado is not a direct result of the interacting air masses. When a warm and cold air mass collide the warm air, being less dense, is forced upward. If the warm air mass is unstable enough, this upward forcing triggers the formation of thunderstorms. If other conditions are right, these storms may go on to produce tornadoes.