4. Water source Water volume, in cubic miles Percent of total water Oceans317,000,00097.24% Icecaps, Glaciers7,000,0002.14% Ground water2,000,0000.61% Fresh-water lakes30,0000.009% Inland seas25,0000.008% Soil moisture16,0000.005% Atmosphere3,1000.001% Rivers3000.0001% Total water volume 326,000,000100% Source: Nace, U.S. Geological Survey, 1967 http://ga.water.usgs.gov/edu/waterdistribution.html

5. East Coast of the U.S.

7. SONAR Sound Navigation Range The echo sounder calculates water depth by measuring time between emission of a sound signal directed toward the ocean floor and the return echo.

8. Atlantic Ocean Floor Profile

9. Ocean Profile

11. Topography of the Ocean Floor  Continental Shelf  Rift Zone  Seamount  Abyssal Plain  Continental Slope  Mid-Ocean Ridge  Ocean Trench  Submarine Canyon

12. Continental Shelf & Slope  Continental shelf – a relatively flat part of the continent covered by seawater. Lies between the coast and the continental slope.  Continental slope – steeply dipping surface between the continental shelf and the deep ocean basin.

13. Continental Shelf & Slope San Francisco Monterey Bay The shelf break marks a distinct change in the slope of the sea floor from the flat continental shelf to the steep sea floor of the continental slope.

14. CONTINENTAL SHELF About 8% of the global seafloor area Source of fish, both commercial and sport, and in some areas, oil and natural gas. Varies in size off the coasts of the U.S. West coast – narrow East coast - wide

15. CONTINENTAL SLOPE Gradually rises from the abyssal plain but climbs as much as 45 degrees as it approaches land. Continental Rise - sediment deposits at the base of the slope Slopes are often gouged by deep valleys or submarine canyons

16. Submarine Canyon HUDSON CANYON CONTINENTAL SLOPE CONTINENTAL SHELF HUDSON CANYON - First discovered in 1864

17. Submarine Canyons San Francisco Canyon leading into Monterey Bay Submarine canyons are v-shaped canyons cut into the continental slope. Many canyons are associated with major rivers such as the Congo, Hudson, and others. most canyons were originally formed during the last Ice Age when the water level was lower some are the result of earthquakes.

18. ABYSSAL PLAIN The true ocean floor Result of sediment drifting downward to fill depressions of the rocky ocean floor remains of marine life fine, clay-sized particles (ooze)

19. Abyssal Plain Continental shelf Abyssal Plain The abyssal plain is the flat, almost level area of the deep ocean basin. Continental slope OOZE!!!

20. Seamount Coast of central California Same area, different perspective A volcanic mountain found on an ocean basin. It is not a result of subduction or formed at the mid- ocean ridge. Possibly an island that has since eroded. seamounts Monterey

21. SEAMOUNT & GUYOT Isolated mountains rising from 3,000 to 10,000 feet above the surrounding seabed. Volcanic origin Seamounts are found in all oceans, but are more numerous in the Pacific Ocean, with over 2,000 identified. Guyots – flat-top seamounts

22. SEAMOUNT & GUYOT

23. Map of Seamounts K. Stocks. 2003. Map of Sampled Seamounts. SeamountsOnline: an online information system for seamount biology. World Wide Web electronic publication. http://seamounts.sdsc.edu.

24. Mid-Ocean Ridge Underwater mountain chain that rises from the ocean basins. Created by rising magma. Mid-Atlantic Ridge

25. Map view showing sea floor spreading at the Mid-Atlantic ridge.

26. MID-OCEAN RIDGE

27. Several mid-ocean ridges are longer than the longest mountain ranges on Earth. Can rise to above sea level to form islands Iceland and the Azores - Atlantic Ocean Galapagos Islands in the Pacific Ocean. Most of the ridges crest at a depth of about 8,000 feet

28. MID-OCEAN RIDGE Oceanic ridges have two peaks, separated by a rift valley. The valley ranges from 15 to 30 miles in width and contains an active seismic area. Example of the Mid-Atlantic Ridge AmericasAfrica / Europe

29. Rift Zone A system of cracks in Earth’s crust through which molten material rises. Rift zones are found in the middle of the mid-ocean ridges. Strange animal life and unique geologic structures have been found here.

30. Rift Zone Divergent zones are where two plates are moving apart Convection currents are rising, bringing up heat Earthquakes and volcanic activity

31. Volcanic ridge on zero- age crust, note small and larger volcanic cones. See cratered volcano at the top? The narrow, linear, bright features in the rest of the image are fault scarps. Uniform gray areas are sediment accumulating. Rift Zone 29° N

32. Black Smokers

35. Trench A deep trough on the ocean floor where oceanic crust is forced below continental or other oceanic crust.

36. Found at subduction zones (near continents and island chains) At least 26 trenches have been identified 22 are in the Pacific Ocean 1in the Atlantic Ocean (Puerto Rico Trench) 1in the Indian Ocean (Java Trench) TRENCH

38. Depths of major trenches exceed 18,000 feet, and vary from 10 to 22 miles in width. The deepest is the Challenger Deep, 35,810 feet deep, in the Marianas Trench {Mount Everest - 29,028 feet} Trenches are not the same: Peru-Chile Trench off the west coast of South America is nearly 1,100 miles long. The Japan Trench is 150 miles long and is the shortest. The Tonga Trench, located between New Zealand and Samoa, is the narrowest and straightest. The Kurile Trench between Japan and Kamchatka is the widest.

39. MarIana TrenchMarIana Trench