1. CHAPTER 3 Marine Provinces

2.  Bathymetry – measuring ocean depths  It was once thought that the deepest parts of the ocean were in the middle of the ocean basins ○ But that is now known not to be true

3.  Fathom ○ Standard unit of measurement for ocean depth ○ 1.8 meters (~6ft)

4. Measuring bathymetry  Ocean depths and topography of ocean floor  “Sounding” Rope/wire with heavy weight ○ Known as lead lining ○ When it hit bottom, it would be pulled up and measured ○ That’s where the term “fathom” came from, 1 fathom = outstretched arm  Echo sounding Reflection of sound signals 1925 German ship Meteor

5. Measuring bathymetry  Precision depth recorder (PDR) 1950s Focused beam Helped confirm plate tectonics  Multi-beam echo sounders  AND  Side-scan sonar More detailed “picture” of sea floor

6. Measuring bathymetry Fig. 3.2

7. Measuring bathymetry  Satellite measurements – measure ocean surface that corresponds with bathymetry Deep areas like trenches exert lower gravitational pull, higher areas such as seamounts exert more gravitational pull Differences affect sea level that can be detected by satellite  Seismic reflection profiles looks at ocean structure beneath sea floor

8. Ocean provinces  3 major provinces Continental margins Continental margins ○ Shallow-water areas close to shore Deep-ocean basins Deep-ocean basins ○ Deep-water areas farther from land Mid-ocean ridge Mid-ocean ridge ○ Submarine mountain range

9. Continental margins  Passive or active  Passive Not close to any plate boundary No major tectonic activity Example: east coast of United States

10. Continental margins  Active (2 types) Associated with convergent or transform plate boundaries Much tectonic activity  1 - Convergent active margin Oceanic-continental convergence Example: western South America  2 - Transform active margin Associated with transform plate boundaries Example: Coastal California along the San Andreas fault

11. Continental margin features  Continental shelf  Shelf break  Continental slope  Continental rise

12. Continental shelf shelf break  Extends from shoreline to shelf break  Shallow, low relief, gently sloping  Similar topography to adjacent coast  Average width 70 km (43 m) but can extend to 1500 km (930 m)  Average depth of shelf break 135 m (443 ft)

13. Continental slope  Change in gradient from shelf  Average gradient 4 o  Submarine canyons turbidity currents  Submarine canyons cut into slope by turbidity currents Mixture of seawater and sediments Move under influence of gravity Erode canyons Deposit sediments at base of slope

14. Continental slope and submarine canyons

15. Continental rise  Transition between continental crust and oceanic crust Submarine fans Submarine fans

16. Deep ocean basin features  Abyssal plains  Volcanic peaks  Ocean trenches  Volcanic arcs

17. Abyssal plains  Very flat depositional surfaces from base of continental rise  Suspension settling  Suspension settling of very fine particles  Sediments cover ocean crust irregularities  Well-developed in Atlantic and Indian oceans

18. Volcanic peaks  Poke through sediment cover  Below sea level: Seamounts, tablemounts, or guyots Seamounts, tablemounts, or guyots at least 1 km (0.6 m) above sea floor Abyssal hills seaknolls Abyssal hills or seaknolls are less than 1 km  Above sea level: Volcanic islands Volcanic islands

19. 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

20. Ocean trenches

21. Volcanic arcs  Landward side of ocean trench  Island arc Chain of islands, e.g., Japan  Continental arc Volcanic mountain range, e.g., Andes Mountains

22. Mid-ocean ridge  Longest mountain chain  On average, 2.5 km (1.5 miles) above surrounding sea floor  Wholly volcanic  Divergent plate boundary

23. Mid-ocean ridge features  Central rift valley, faults, and fissures  Seamounts  Pillow basalts  Hydrothermal vents Deposits of metal sulfides Unusual life forms  Fracture zones transform faults  Fracture zones and transform faults

24. Mid-ocean ridge features  Oceanic ridge Prominent rift valley Steep, rugged slopes Example: Mid-Atlantic Ridge  Oceanic rise Gentler, less rugged slopes Example: East Pacific Rise

25. Volcanic features of mid-ocean ridge  Pillow lava or pillow basalts Hot lava chilled by cold seawater Smooth, rounded lobes of rock

26. Volcanic features of mid-ocean ridge  Hydrothermal vents Heated subsurface seawater migrates through cracks in ocean crust ○ Warm-water vents <30 o C or 86 o F ○ White smokers >30 o C <350 o C or 662 o F ○ Black smokers > 350 o C

27.  Unusual biological communities Able to survive without sunlight Chemosynthesize instead of photosynthesize Archaeon bacteria and bacteria oxidize hydrogen sulfide gas to provide food

28. Fracture zones and transform faults  Long linear zones of weakness offset axes of mid-ocean ridge  Transform faults  Transform faults: movement in opposite directions ○ Still seismically active  Fracture zones  Fracture zones: extensions of transform faults (aseismic) ○ Beyond offset segments of oceanic ridge

29. Ocean Literacy Standards  1b - An ocean basin’s size, shape and features (islands, trenches, mid-ocean ridges, rift valleys) vary due to the movement of Earth’s lithospheric plates. Earth’s highest peaks, deepest valleys and flattest vast plains are all in the ocean.  5g - There are deep ocean ecosystems that are independent of energy from sunlight and photosynthetic organisms. Hydrothermal vents, submarine hot springs, methane cold seeps, and whale falls rely only on chemical energy and chemosynthetic organisms to support life.

30. Sunshine State Standards  SC.7.E.6.1 Describe the layers of the solid Earth, including the lithosphere, the hot convecting mantle, and the dense metallic liquid and solid cores.  SC.7.E.6.3 Identify current methods for measuring the age of Earth and its parts, including the law of superposition and radioactive dating.  SC.7.E.6.4 Explain and give examples of how physical evidence supports scientific theories that Earth has evolved over geologic time due to natural processes.  SC.7.E.6.5 Explore the scientific theory of plate tectonics by describing how the movement of Earth's crustal plates causes both slow and rapid changes in Earth's surface, including volcanic eruptions, earthquakes, and mountain building.  SC.7.E.6.7 Recognize that heat flow and movement of material within Earth causes earthquakes and volcanic eruptions, and creates mountains and ocean basins.  SC.912.E.6.1 Describe and differentiate the layers of Earth and the interactions among them.  SC.912.E.6.3 Analyze the scientific theory of plate tectonics and identify related major processes and features as a result of moving plates.  SC.912.E.6.5 Describe the geologic development of the present day oceans and identify commonly found features.