Unformatted text preview: 4. Oceanic crust gets more dense as it cools and gets older 5. Convergent Plate Boundaries 1. Where old oceanic crust is destroyed. 2. Can be any kind of crust 3. Density rules. 4. Deep earthquakes. 5. Volvanoes. 6. Trenches....
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- Spring '09
- Plate Tectonics, Convergent boundary, oceanic crust, new oceanic crust, Evan Price