A conveyor belt is an assembly of a belt rotating around two pulleys. Either one or both of the pulleys of the conveyor belt system are powered to rotate; when they rotate, the belt moves as well, transporting the materials on the belt from one place to another.
The first conveyor belt was invented by a man named Richard Sutcliffe in 1905. They used them in coal mines which caused a big transformation in the mining industry.
Glacial meltwater acts as a lubricant between ice sheets and the ground, and, like a conveyor belt, moves the ice sheet.Answered by Kellie H. - 182 days ago at 5:04pm on Oct 24 2012
A Conveyor belt's head pulley is also known as the drive pulley, its on this end of a conveyor system where the motorized pulley is installed. At this point the conveyed material is discharged "wherever" and the belt wraps around and begins its return cycle. The head pulley is at the discharge so that the conveyed material is "pulled" through the system vs. having the tail pulley motorized which would be forcing the system to "push" the belt containing the conveyed material.
assembly line
The Great Ocean Conveyor Belt is also called thermohaline circulation.
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The simplified pattern of ocean currents,looks like a conveyor belt,moving water between the oceans
The global current conveyor belt begins on the surface of the ocean near the pole in the North Atlantic.
thermohaline circulation
because thats the way it is Whoever wrote this must be an absolute genius. The real answer is that when THE EARTH SPINS IT CREAATES THE NEW OCEAN FLOOR WHICH ALSO CREATES THE CONVEYOR BELT
The global oceanic conveyor belt, is a unifying concept that connects the ocean's surface and thermohaline (deep mass) circulation regimes, transporting heat and salt on a planetary scale.
The simplified pattern of ocean currents,looks like a conveyor belt,moving water between the oceans
The global current conveyor belt begins in the North Atlantic Ocean, where warm water from the Gulf Stream moves northward to the Arctic. This warm water eventually cools and sinks in the Labrador Sea, starting a deep current that travels southward along the ocean floor.
A conveyor belt. There is not a special name for it.
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The hypothesis of seafloor spreading is likened to a conveyor belt because new oceanic crust is continuously formed at mid-ocean ridges, moves away in opposite directions, and eventually subducts back into the mantle at deep-sea trenches. This process is similar to how a conveyor belt moves material in one direction while continually creating and discarding it at different points.