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Today’s Tunes  Fathoms  Below / Under the Sea From soundtrack of Disney’s The Little Mermaid Seafloor Features: Continental Margins Submarine canyons (cut into the c. slope) Abyssal plain Continental shelf Continental rise Abyssal plain Continental slope Seafloor spreading center (e.g., East Pacific RISE or Mid-Atlantic RIDGE) Deep Ocean Seamounts Abyssal Hills (linear hills) Seafloor Features: Deep Ocean  Plate Tectonic Boundaries Ridges or Rises Trenches Transform Faults, Fracture Zones The Shifting Crust Continental Drift  Alfred Wegener -1912 – large “supercontinent” (Pangea) existed and then split into pieces – fossil & glacial deposit evidence  Wegener not able to provide MECHANISM for his theory  Major mechanism later found in the OCEANS Seafloor Spreading & Plate Tectonics  Harry Hess - 1960s – new ocean basins form from volcanism – ocean floor forms IN BETWEEN pieces that have split – SEAFLOOR SPREADING Seafloor Spreading & Plate Tectonics  Theoretical breakthrough – PLATE TECTONICS – surface of earth composed of “plates” (LITHOSPHERE) that move on a “conveyor belt” (ASTHENOSPHERE) Evidence for Continental Drift  Fit of the continents  Correlation of mountain belts  Diversity of species – correlation of dinosaur species (Pangea) – isolation of mammal species (after breakup)  Glaciers Important Quote  “Relationships known since early in the century yet the validity of continental drift was not generally recognized until the late 1960’s”  It took ocean floor data to solidify ideas and convince scientific community!  The oceans rule! One Mechanism  seafloor-spreading  lithosphere  asthenosphere Another Mechanism  subduction  world’s most explosive volcanos are formed over subduction zones  Oregon’s Cascades Mtns. over Cascadia Subduction Zone – Juan de Fuca plate under N. American plate “Munch and Crunch”  “MUNCH” - subduction of oceanic plate under continent or ocean – oceanic crust is thin and dense – dives  “CRUNCH” - collision of continental plates – India into Tibet and China – continental crust is thick and light Sliding By  Transform faults – plates neither created nor destroyed  Transform faults are active  Fracture zones are inactive extensions of transforms – “fossil transforms” Young & Old  Oldest seafloor - 200 million years  Oldest land - billions of years  With seafloor spreading, is the earth expanding?  Why is seafloor so young relative to continents?  SUBDUCTION  “law of conservation of ocean floor” Convergent  Convergent - subduction – trenches – Tonga Trench, Cascadia Subduction Zone Divergent Plate Boundaries  Divergent - seafloor spreading – mid-ocean ridges or rises – Mid-Atlantic RIDGE, East Pacific RISE Translational  Translational - strike-slip faulting – transform faults (active) - San Andreas Fault – fracture zones (inactive) - Mendocino FZ Plate Boundaries  How do we know where these boundaries are?  bathymetry  earthquakes  deepest earthquakes at CONVERGENT boundaries (subduction zones/trenches)  downgoing plate breakage causes earthquake  like potato chip breaking off in bean dip Extra Slides not covered in lecture, but cover valuable info that can help in lab too Proof for Seafloor Spreading  What made people believe in seafloor spreading? (poor Wegener!)  changes in inclinations of magnetic field  Earth’s magnetic field a mystery  currents in liquid core one hypothesis SF Spreading Proof - 2  Earth’s magnetic field flips back & forth  magma freezes magnetic minerals  minerals lines themselves up w/ prevailing field of earth  anomaly in field is the key - normal (positive) or reversed (negative)  Vine and Matthews noted this in the ‘60s and flagged this as PROOF for seafloor spreading Grocery bar code Calibrated by agedating of rocks Last reversal 200 Ka Driving Forces  “Slab pull” versus “ridge push”  Slab Pull - gravity pulls cooled, dense plates back down into mantle at subduction zone  Ridge Push - rising, hot rock pushes plates apart at spreading center
 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                             
                                            