| To learn some geology, 
                          try pouring a cool cocktail. Plate tectonics may be about to be 
                          turned on its head. Instead of being heated from below 
                          like water on a stove, the Earth's interior could have 
                          more in common with a neat gin on the rocks.  While geologists agree that the plates 
                          of the Earth's crust are constantly moving, nobody is 
                          quite sure why. Some believe that heat from within the 
                          Earth causes convection currents in the molten interior 
                          that drive the plates. But geophysicist Don Anderson 
                          of the California Institute of Technology in Pasadena 
                          thinks the convection could be triggered by the plates 
                          themselves. Efforts to model mantle convection based 
                          on heat from below have failed.  "Those convection calculations 
                          have never come up with plate tectonics or anything 
                          resembling the present situation on Earth," Anderson 
                          says.  Thinking about the problem from the 
                          top down may be the key. The new view is that where 
                          the hot mantle comes into contact with the relatively 
                          chilly crust above, it cools and sinks. The same thing 
                          happens when you order a drink on the rocks, says Anderson. 
                         "If you put two ice cubes in a 
                          glass of gin, the gin next to the ice cubes will get 
                          cold and sink." By studying the pattern of the plates 
                          today and in the past, Anderson concludes that the Earth 
                          is in a transitional state between so-called "ideal 
                          configurations" – low-energy, stable states 
                          seen in other spherical systems such as buckyballs and 
                          viruses.  "If things ever settle down to 
                          an equilibrium state, then the ideal number of plates 
                          seems to be somewhere around 12," he adds.  Although Earth does have roughly 12 
                          plates, they have widely different shapes and sizes. 
                          It's an unstable configuration but may eventually even 
                          out into patterns where three similar plates meet at 
                          triple junctions. This is typical of systems in nature 
                          that are controlled by surface processes, and Anderson 
                          speculates that the Earth's plates are controlling the 
                          interior, not vice versa.  "It shows that plate tectonics 
                          is much more powerful than people thought," he 
                          says.  If Anderson is right, geologists may 
                          have to reconsider why some volcanoes appear where they 
                          do. Volcanic activity where two plates collide can easily 
                          be blamed on plates melting as one is forced under the 
                          other. But when volcanoes emerge in the middle of a 
                          plate, geologists usually invoke a narrow plume of hot 
                          mantle rising up from deep within the Earth and bursting 
                          through the crust.  Anderson, however, believes that weak 
                          spots in the plates rather than plumes control where 
                          the hot magma erupts onto the surface.
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