sea floor
DESCRIPTION
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 PresentationTRANSCRIPT
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
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
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
Passive and Active Margins
Active vs. Passive Margins
• Active • Passive
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
Hydrothermal Vents
• Central rift valley• Black smokers• Life discovered around the hydrothermal vents
• http://www.youtube.com/watch?v=rFHtVRKoaUM