The general result is to make the ocean basin wider.
There are many possible forces or mechanism associated by continental movement.include;sea-floor spreadingthermal plume phenomenaslab-push at mid oceanic ridge.slab-pull at subduction zoneNote that all this mechanism work together
One would need a fluid (water, air or the like) and something to drive currents within it. Here's the skinny right from our friends at Wikipedia: "Convection in the most general terms refers to the movement of currents within fluids (i.e. liquids, gases, and rheids)." Jumping off from there, let's look at an example of a heat transfer possibility. When we use the oven, the kitchen gets warm. There is a bit of thermal radiation, but skip that and just check the convection side. Air (a fluid) is against the outside of the oven door. As heat from the door is transferred to the air, it becomes less dense than the air around it, and it rises. Some "new" cooler air takes its place and the process continues. A convection current has spontaneously arisen. The process of heat transfer drives the convection cycle; it sets up those currents in the air around the oven. Soon the kitchen is warmer than it used to be.
counter clockwise
Generally, currents moving away from the equator tend to be warmer, while currents moving towards the equator tend to be cooler. This is because warm water near the equator is carried away by ocean currents towards higher latitudes, where it cools down and then returns towards the equator as a cooler current.
The time it takes for magma to complete a circular convection flow can vary depending on factors such as temperature, viscosity, and the size of the magma chamber. In general, this process can take anywhere from days to centuries.
Because of the Influence of the Coriolis Effect, the general motion of surface currents in the north Atlantic is to the right. In the south Atlantic the general motion is to the left.
Because Of The Infulence Of The Coriolis Effect, The General Motion Of Surface Currents In The North Atlantic Is To The Right. In The South Atlantic The General Motion Is To The Left. -Hope This Helped!
No, convection currents can vary in strength and direction depending on factors such as temperature gradients, fluid properties, and boundary conditions. In general, convection currents result from the movement of fluids due to differences in temperature, but the specific behavior can be influenced by a variety of factors.
Because Of The Infulence Of The Coriolis Effect, The General Motion Of Surface Currents In The North Atlantic Is To The Right. In The South Atlantic The General Motion Is To The Left. -Hope This Helped!
There is always some convection current moving somewhere, and all earthquakes (except man-made induced ones) in general can be attributed to the convection movements of the lower and upper mantle. However, the 1976 Tangshan earthquake is believed to be a result of the Amur Plate/Subplate rotating and grinding against the Eurasian Plate.
General Atlantic was created in 1980.
Convection-currents in the Mantle, and spreading-ridge pressure from the emerging basalt along constructive plate boundaries. The processes come under the general heading of 'Plate Tectonics'.
Atlantic General Hospital was created in 1993.
There are three general methods of energy transfer: conduction (transfer through direct contact between objects), convection (transfer through fluid motion like air or water currents), and radiation (transfer through electromagnetic waves).
There are many possible forces or mechanism associated by continental movement.include;sea-floor spreadingthermal plume phenomenaslab-push at mid oceanic ridge.slab-pull at subduction zoneNote that all this mechanism work together
The Atlantic
Convection oven is an example. A convector is a general name for something that transfers heat by convection.