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With time the magma may migrate away from its sources, creating a gradual increase in depth of the axis as the pressure within it gradually wanes This phenomenon may explain the noncoincidence of magma chamber and rise culmination noted by Mutter et al (1988) The brittle shell overlying the magma stretches and cracks and magma intrudes so that eruptions follow the path of magma migration After eruption the removal of supporting magma gives rise to the formation of an axial summit graben Evidence for the pulselike, episodic spreading of ridges, in which sea oor spreading occurs by fracturing, dike injection and copious volcanism, has been provided by seismological studies and direct observation (eg Dziak & Fox, 1999;.

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Here are some useful tips to keep in mind while cutting plastic in this way: Don t worry about what Sheryl Crow (or Rod Stewart) might say here, the first cut isn t the deepest. But it does need to be the most accurate, so take your time. By the same token, the deeper you try to make the groove the first time, the greater the chance that the knife will slip because of the pressure. This can cut you, and mess up the project as well. You can also tape the edges of the pattern for added stability. Look straight down from above at what you re cutting. When cutting the buttons, slice just around the shape, not on it or inside it. This gives you a margin of error for things to fit. (As I always say, too much is better than not enough.)

Frequency (Hz)

<map name= navbar > <area shape= rect coords= 1,1,30,33 href= home.html alt= Home Page > <area shape= circle coords= 65,64,62 href= contacts.html alt= Information > <area shape= default href= index.html > </map>

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