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Description
The figure shows how magma rises at the center of the divergent boundary, also called a mid-ocean ridge, creating new oceanic crust. The newly created crust is pulled from the ridge on each side due to tension forces from the magma within the mantle that pulls the crust away. |
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Instructions Notice that as the seafloor spreads, it gets deeper. What could cause this to happen? |
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Keywords ERESE, divergent plate boundary, spreading center, mid-ocean ridge, divergent plate margin, seafloor spreading, divergent plate boundaries |
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Copyright Owner Enduring Resources for Earth Science Education (ERESE) |
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