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CHAPTER 3 Marine Provinces
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Continental margins Fig. 3.6
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Measuring bathymetry Fig. 3.3a
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Continental margins Passive Not close to any p _______b_________
No major t_________ activity Example: ____________
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Continental margins Active Convergent active margin
Associated with c________ or t_________ plate boundaries Much t________ activity= Convergent active margin Oceanic-continental convergence Example:
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Continental margins Transform active margin
Associated with transform plate boundaries Example:
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Continental Shelf= Continental slope=
Submarine canyons cut into slope by turbidity currents Mixture of seawater and sediments Move under influence of gravity Deposit sediments at base of slope
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Continental slope and submarine canyons
Fig. 3.9a
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Abyssal plains Fig. 3.11
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Volcanic peaks Poke through sediment cover Below sea level:
Seamounts, or guyots at least 1 km (0.6 m) above sea floor Above sea level: Volcanic islands
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Ocean trenches Linear, narrow, steep-sided
Associated with subduction zones Deepest parts of ocean Mariana Trench, 11,022 m (36,161 ft) Majority in Pacific Ocean
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Ocean trenches Fig. 3.12
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Volcanic arcs Landward side of ocean trench Island arc Continental arc
Chain of islands, e.g., Japan Continental arc Volcanic mountain range, e.g., Andes Mountains
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Mid-ocean ridge Longest mountain chain
On average, 2.5 km (1.5 miles) above surrounding sea floor Wholly volcanic Basaltic lava Divergent plate boundary
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Rift valley, faults, and fissures
Downdropped rift valley at central crest Cracks (fissures) and faults common Fig. 3.17
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Volcanic features of mid-ocean ridge
Hydrothermal vents Heated subsurface seawater migrates through cracks in ocean crust Warm-water vents <30oC or 86oF White smokers >30oC <350oC or 662oF Black smokers > 350oC
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Hydrothermal vents Fig. 3.16a
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Hydrothermal vents Dissolved metals precipitate to form metal sulfide deposits Unusual biological communities Able to survive without sunlight Archaeons and bacteria oxidize hydrogen sulfide gas to provide food
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End of CHAPTER 3 Marine Provinces
Fig. 3C
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