Spreading centers with high spreading rates, such as those where plates are diverging rapidly, are characterized by a long, gently sloping ridge. the ridge forms as a well-developed magma chamber beneath causes the rock to swell upward. in contrast, spreading centers with slow spreading rates have poorly developed magma chambers and a well-defined rift valley developed at the center of the ridge. drag the appropriate labels to their respective targets. you do not need to use all labels. view available hint(s)
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Spreading centers with high spreading rates, such as those where plates are diverging rapidly, are c...
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