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Page 160. Daily Question. At which type of plate boundary would you find mafic igneous rocks? Explain Would the rocks be basalt, gabbro, or could both rock types occur? Explain . Fig. 6.6. Plate Tectonics and Igneous Rocks. Ophiolite Complex. Oceanic Crust Marine Sediment
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Daily Question • At which type of plate boundary would you find mafic igneous rocks? Explain • Would the rocks be basalt, gabbro, or could both rock types occur? Explain
Fig. 6.6 Plate Tectonics and Igneous Rocks
Ophiolite Complex Oceanic Crust Marine Sediment Pillow Basalts Sheeted Dikes Gabbro
Fig. 6.6 Plate Tectonics and Igneous Rocks
Cinder Cones • Built from ejected lava fragments • Have steep slopes (controlled by angle of repose – the steepest angle at which material remains stable) • Small – 300 m (1000 ft) high, 2 km in diameter
Composite Cones - Stratovolcano • Most encircle the pacific ocean (ring of fire) as part of magmatic arcs • Large – ~1 km high, 5 - 25 km wide • Symmetrical structure • Composed of alternating lava flows and pyroclastic deposits • Product of high viscosity magma • Have violent eruptions Mount Rainer
Fig. 6.6 Plate Tectonics and Igneous Rocks
Produced by rising plume of mantle material (mantle plume) • They are stationary – plates move over the hotspots
Basalts produced by hot spots are chemically different from basalts produced at MOR
Hot Spot Under Hawaii • Notice linear layout of islands • Could determine plate movement rate for data • Island continually being formed
Shield Volcanoes • Broad, slightly domed strucutre • Large structure 9 km (~6 miles) high & 50 km (~30 miles) wide • Produced by fluid (low viscosity) lava • Example: Mauna Loa, Kilauea, other island chains
Hot Spot Example – Continental • Yellowstone