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Sea Floor Part 3

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Sea Floor. Part 3. Underwater volcanic eruption! COOL. http:// www.youtube.com/watch?v = hmMlspNoZMs. Trenches . Sediments. Thicker the farther away from the ridge. Two types Lithogenous Biogenous Composed of CaCO3 or SiO2. Diatoms. Radiolarians. Foraminiferans. Coccolithophorids. - PowerPoint PPT Presentation

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Page 1: Sea Floor

Sea Floor

Part 3

Page 3: Sea Floor

Trenches

Page 4: Sea Floor
Page 5: Sea Floor

Sediments

• Thicker the farther away from the ridge. • Two types – Lithogenous – Biogenous • Composed of CaCO3 or SiO2

Page 6: Sea Floor

Diatoms

Page 7: Sea Floor

Radiolarians

Page 8: Sea Floor

Foraminiferans

Page 9: Sea Floor

Coccolithophorids

Page 10: Sea Floor

Microfossils

• The organisms that produce biogenous sediments are microscopic or close to it.

• Sediment particles are sometimes called microfossils.

• Can determine past climate– Carbon dating– Ratios of magnesium to calcium, isotopes of

oxygen

Page 11: Sea Floor

Continental Margins

• Continental Shelf• Continental Slope• Continental Rise• Abyssal Plain

• Draw a diagram and label each margin – take notes on your diagram about its characteristics

Page 12: Sea Floor

Passive and Active Margins

Page 13: Sea Floor

Active vs. Passive Margins

• Active • Passive

Page 14: Sea Floor

Deep Ocean Basins

• The abyssal plain– Rises at a gentle slope towards the mid ocean

ridge system. • Flat with some channels, low abyssal hills,

plateaus and rises• Seamounts• Mariana Trench- 36,163 ft deep

Page 15: Sea Floor

Hydrothermal Vents

• Central rift valley• Black smokers• Life discovered around the hydrothermal vents

• http://www.youtube.com/watch?v=rFHtVRKoaUM