1. Chp 11: Sea Floor-ancient mariners

2. Chp 11: Sea Floor Map showing 4 major oceans, sea floor topography=bathymetry

3. Chp 11: Sea Floor ALVIN submersible used to survey the sea floor

4. Sampling the sea floor: a.Clamshell sampler taking a sea floor sample b. Piston core falls to sea floor penetrates sediment, then is retrieved with sediment in barrel.

5. Chp 11: Sea Floor JOIDES Resolution vessel-drills in deep oceans to recover Sediments and basalts to study history of Earth

6. Chp 11: Sea Floor DSDP core from ocean drilling- crosses the Cretaceous-Tertiary Boundary; the dark gray layers in middle are the sediments produced in middle of ocean as result of asteroid impact at end of Cretaceous Period.

7. Chp 11: Sea Floor Continental Margins and deep sea Continental Margins and deep sea: a.Continental Margins- subdivided by bathymetry (depth) 1. Continental shelf: down to 200m 2. Continental slope: steep slope, down to 2500m? 3. Continental rise: gentle slope, down to 3000m? b. Deep Ocean sea floor- essentially the deep ocean 1. Abyssal Plain- generally flat lying, central ocean plains 2. Oceanic trench- where subduction occurs, deepest portion of ocean. 3. Mid-ocean Ridges: subsea mountain ranges, volcanic centers, where molten lava extruded on sea floor, generates new oceanic crust. -where Submarine hydrothermal vents are found. Known as ‘black smokers’ a unique ecosystem exists here-bacteria, animals, plants….now hypothesized as possible means by which life began on Earth in PreCambrian-more than 600MYA

8. Generalized Profile of Sea Floor showing features of margins also Sea Level Mid Ocean ridge Continental Margin Continental Shelf Continental Slope Oceanic trench Abyssal Plain Continental Margin Continental Shelf Continental Slope Continental Rise

9. Chp 11: Sea Floor architecture Mid ocean ridges Trenches

10. Chp 11: Sea Floor

11. Continental Margins Continental Margins: a.Two types of Continental margins: 1. Passive: within a plate, lack volcanic activity (US E Coast) 2. Active: leading edge of continental plate-where subduction occurs (along western edge of S America) b. Sedimentary features common along continental margins 1. Submarine canyons- deep, steep sided canyons on shelves and slopes. Most can be related to sea level fall during last Ice Age when rivers extended to edge of present day shelf. 2. turbidity currents- sediment-water mixtures that are denser than sea water; flow down canyons onto slope where form ‘fans’ 3. Submarine fans- deposition by turbidity currents of overlapping wedge shaped sediment piles referred to as ‘submarine fans’

12. Chp 11: Sea Floor

13. Note thickest sediments occur offshore major deltas today, or where major deltas existed in geologic past. (yellow-red-orange is thickest)

14. Age of Sea Floor: oldest sea floor is in blue (Jurassic) youngest sea floor is along mid ocean ridges Sea floor fractures: where mid ocean ridges are offset perpendicular to ridge itself

15. Profile thru mid ocean ridge- vertical succession of layers=ophiolite

16. Chp 11: Sea Floor Deep Sea Sedimentation: see Fig 11-19 in book!! a.Most deep sea sediment is fine grained material- silt and clay sized-because most transport mechanisms can move coarse material (sand and gravel) far from shore. 1. most material is wind blown dust and ash from continents and islands, or shells of micro- scopic organisms that fall to sea floor after organism dies- referred to as Pelagic sediments- meaning the settled from suspension far from land. Several types of Pelagic sediment are common: 1. Pelagic clay: red to brown, composed of clay sized particles from continents or islands. covers most of the deep ocean basins. 2. Ooze: composed mostly of shells of microscopic marine organisms and plants - calcareous ooze: Calcium carbonate skeletons of tiny marine organisms (forams) - siliceous ooze: silica skeletons of single celled animals (radiolarians) or plants (diatoms) b. coarse grained sediments are delivered to deep ocean in several ways- a. ice rafting: icebergs transport coarse material into ocean, deposit it as ice melts b. turbidites: high energy flows transport coarse material far from continental shelf edge

17. Chp 11: Sea Floor Imaging the sea floor and beneath the sea floor: 1.Imaging the sea floor: side-scan sonar 2.Imaging shallow depth beneath sea floor: sub bottom profiler (up to 100 m or so….) 3. Imaging greater depths beneath sea floor: seismic reflection data (up to several kilometers)

18. Chp 11: Sea Floor-Side Scan sonar ‘fish’ towed behind vessel, emits sound waves that are reflected back to sensor, produces ‘picture’ of sea floor surface.

19. Chp 11: Sea Floor-side scan sonar deployment

20. Side scan sonar – sediment waves, escarpment

21. Chp 11: side scan sonar-note central no data zone

22. Side Scan sonar-iceberg marks

23. Chp 11: Sea Floor

24. Sub bottom or Echo Profile- reflects off sea floor, returns to vessel, gives profile of depth but actually measured in TIME

25. Chp 11: Sea Floor

30. Chp 11: Sea Floor topography Mid-ocean ridges: where new crust forms, extrusive igneous Trenches: deepest portions of ocean-where subduction occurs (oceanic plate dives beneath continental plate or other oceanic plate). Guyots and Seamounts: -guyot-eroded, flat topped volcanic island. Due to erosion at sea level…. -seamount-never reached sea level, has sharp, cone profile Atolls: coral reefs that grow around edges of guyot, form circular islands

31. Sea Floor- a. trenches b. other features??- -guyots -seamounts

32. Chp 11: Sea Floor

35. Chp 11: Sea Floor-Atolls, Tahiti

36. Chp 11: Sea Floor- Reefs Most reefs are constructed in warm, tropical climates by algae. Some cold water reefs are known today also.

37. Chp 11: Sea Floor-Deep Sea Resources Resources from the ocean: a.Continental shelf-slope-rise: -drilling for hydrocarbons (oil and gas) -shelf: dredging for diamonds etc off river mouths -methane hydrate: gas in form of ‘ice’- undeveloped resource -phosphorites: phosphorus deposits in shallow water b. Abyssal plain: -manganese nodules: round, softball size nodules that are concentric layers around a central object; precipitate rare elements out of sea water into these layers. Not economic to date…. A significant legal question….Economic Exclusion Zones declared by countries with ocean boundaries….200 nautical miles from shore…. - sulphide deposits at midocean ridges: deep water, not feasible now….

38. Chp 11: Sea Floor-Summary 1.Profile of sea floor: continental shelf down slope onto -abyssal plain - mid-ocean ridges -trenches: deepest spots in oceans 2. Sampling of sea floor-oceanography -coring apparatus retrieve actual sediment samples -submarines -dredging -Deep sea drilling: academic research 3. Age of oceans- result of plate tectonics; oldest sediment is Jurassic (approx 180 MYA).

39. Chp 11: Sea Floor

40. Chp 11: Sea Floor- Summary Imaging the sea floor and beneath the sea floor: 1. Side scan sonar: imaging sea floor 2. sub bottom profiler- imaging shallow depths beneath sea floor (up to 100+m or more) 3. Seismic Reflection- imaging sea floor to depths in kilometers beneath the sea floor. Sea floor topographic features: -guyots -seamounts -atolls -reefs Economic uses: drill for oil and gas- shelf to slope dredge shallow water offshore rivers for minerals, ores…

41. Chp 11: Sea Floor- Summary Deep sea sedimentation: Several types of Pelagic sediment are common: 1. Pelagic clay: red to brown, composed of clay sized particles from continents or islands. covers most of the deep ocean basins. 2. Ooze: composed mostly of shells of microscopic marine organisms and plants - calcareous ooze: Calcium carbonate skeletons of tiny marine organisms (forams) - siliceous ooze: silica skeletons of single celled animals (radiolarians) or plants (diatoms) b. coarse grained sediments are delivered to deep ocean in several ways- a. ice rafting: icebergs transport coarse material into ocean, deposit it as ice melts b. turbidites: high energy flows transport coarse material far from continental shelf edge

42. Chp 11: Sea Floor- Summary Continental margins:2 types recognized 1. Passive: intra plate, rare volcanic activity; US E Coast 2. Active: plate margin where subduction occurs, typified by volcanic activity; west coast of S America Continental Margins- subdivided by bathymetry (depth) 1. Continental shelf: down to 200m 2. Continental slope: steep slope, down to 2500m? 3. Continental rise: gentle slope, down to 3000m? b. Abyssal Plain- essentially the deep ocean 1. Abyssal Plain- generally flat lying, central ocean plains 2. Oceanic trench- where subduction occurs, deepest portion of ocean. 3. Mid-ocean Ridges: subsea mountain ranges, volcanic centers, where molten lava extruded on sea floor, generates new oceanic crust. -where Submarine hydrothermal vents are found: high temperature, volcanic gases