Bathymetry of the Ocean Floor

1. Bathymetry of the Ocean Floor • echo soundings (1920’s) • ocean was not deepest in the center

2. Echo sounding- not always accurate Fig. 4-2a, p. 79

3. Figure 3.1- An Echo Sounding of US East Coast

4. Figure 3.3- Side-scan SONAR (Sound Navigation and Ranging)

5. Figure 3.2- Multibeam SONAR (Sound Navigation And Ranging)

6. Satellites Can Be Used to Map Seabed Contours With the use of satellite altimetry, sea surface levels can be measured more accurately, showing sea surface distortion. (left) Distortion of the sea surface above a seabed feature occurs when the extra gravitational attraction of the feature “pulls” water toward it from the sides, forming a mound of water over itself.

7. Figure 3.B

8. Figure 3.C

9. Figure 3.5

10. Figure 3.6

11. Fig. 4-5, p. 82

12. Figure 3.7

13. Shape of the Ocean Floor • shallow extensions of the continents extended seaward underwater

14. Figure 3.8

15. Shape of the Ocean Floor • Submerged outer edge of the continents are called continental margins • Deep-sea floor beyond these is called the ocean basin

16. Fig. 4-7, p. 83

17. Continental Margins • Passive margins – • continental margins not located on plate boundaries • Atlantic-type margins

18. Continental Margins • Active margins- • continental margins on the edge of convergent or transform plate boundaries • Pacific-type margins

19. Fig. 4-8, p. 84

20. Figure 3.7

23. Continental Margins • Continental Shelves • Shallow, submerged extension of a continent • broad, gently sloping

24. Figure 3.8

25. Fig. 4-9, p. 85

26. Continental Margins • Width of Continental Shelf is determined by : • proximity to a plate boundary • current speed in the region • sea-level

27. Fig. 4-8, p. 84

29. Continental Margins • Shelf break – • transition between the continental shelf and the continental slope • Occurs at about 140m (360 ft) • Continental Slopes • Steeper than the shelf

30. Figure 3.8

31. Continental Margins • Continental rises • base of continental slope covered by a blanket of accumulated sediment • gradual slope • on Passive margins only

32. Fig. 4-9, p. 85

34. Fig. 4-7, p. 83

35. Figure 3.6

36. Continental Margins • Submarine Canyons • cut into the continental shelf and slope • formed by turbidity currents (avalanche-like sediment movements)

38. Figure 3.10a

39. Submarine Canyon Off of The coast Of New Jersey

41. Figure 3.11

42. Ocean Basin • thick layer of sediment (up to 5 km or 3mi thick) covering basaltic rocks • Make up more than ½ of the earth’s surface

43. Ocean Basin • Oceanic ridges • Underwater mountain chain • an active spreading center • offset at regular intervals by transform faults

44. Fig. 4-16a, p. 89

45. Figure 3.15

46. Figure 3.19

47. Ocean Basin • Hydrothermal vents • 1977 Robert Ballard & J F Grassle • average temp is about 8-16oC (46-61oF) much warmer than the typical 3-4oC (37-39oF) • support a unique community of organisms that depend on chemosynthetic bacteria

48. Figure 3.17

49. Fig. 4-19, p. 91