WebMagma generation beneath MORs occurs through decompression melting of upwelling mantle in response to plate separation. The melt-producing region is believed to be on … WebAlthough silica-rich magmas have lower temperatures than silica-poor magmas, a high degree structure gives them higher viscosity. Rises in temperature and in water content break down the structure of magmas and decrease their viscosity. Therefore, a water-rich magma is more fluid than a dry magma of the same composition.
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