Sea Floor Spreading Theory.ppt
- 1. Sea Floor Spreading EQ: What is the process of sea-floor spreading?
- 2. Mid-Ocean Ridge • Mid-Ocean Ridge: The undersea mountain chain where new ocean floor is produced; a divergent plate boundary
- 4. Sonar • Sonar: A device that determines the distance of an object under water by recording echoes of sound waves
- 5. The sonar is used to map the ocean floor Sonar bounces sound waves off underwater objects and then records the echoes of these sound waves The time it takes for the echo to arrive indicates the distance to the object
- 6. Evidence for Sea-Floor Spreading In the 1960s, Harry Hess examined maps of the mid ocean ridge. He proposed that the ocean floors move like conveyor belts, carrying the continents with them.
- 7. Sea-Floor Spreading The process by which molten material adds new oceanic crust to the ocean floor
- 8. What evidence did scientists find for sea-floor spreading in the 1960s? • Evidence from molten material • Evidence from magnetic stripes • Evidence from drilling samples
- 9. Evidence From Molten Material • Alvin’s crew found strange rocks shaped like pillows or like toothpaste squeezed from a tube • Such rocks can form only when molten material hardens quickly after erupting under water • The presence of these rocks showed that molten material has erupted again and again from cracks along the central valley of the mid-ocean ridge. http://www.pmel.noaa.gov/vents/nemo/explorer/concepts/pillow_lava.html
- 10. Scientists discovered that the rock that makes up the ocean floor lies in a pattern of magnetized “stripes” 780,000 years ago, magnetic poles reversed themselves • If they reversed today, the needle in a compass would point south instead of north The rock in the ocean is made of iron, which began as molten material Evidence From Magnetic Stripes
- 11. Evidence From Drilling Samples • When scientists sampled the rocks, they found that the further away from the ridge the rocks were the older they were • The younger rocks were always in the center of the ridges
- 13. Deep-Ocean Trenches • A deep valley along the ocean floor through which oceanic crust slowly sinks towards the mantle
- 14. Subduction • Subduction: The process by which oceanic crust sinks through a deep- ocean trench and back into the mantle; a convergent plate boundary
- 15. Guide For Reading: What happens to the ocean floor at deep ocean trenches? • At deep-ocean trenches, two plates collide causing the denser of the two plates to dive back to the mantle. This process is known as subduction. • Over tens of million of years, this material melts back into molten material and may rise again as new oceanic crust.
- 16. Guide For Reading: What is the process of sea-floor spreading? • At the mid-ocean ridge, molten material rises from the mantle and erupts. The molten material then spreads out, pushing older rock to both sides of the ridge. • Over tens of millions of years, the process continues until the oldest ocean floor collides with the continental crust • The more dense oceanic crust subducts (sinks) back into the mantle at a deep- ocean trench
- 18. Subduction in the Pacific Ocean • Subduction in the Pacific Ocean is occurring at a greater rate than sea- floor is expanding • This is caused by the large amount of trenches
- 19. Subduction in the Atlantic • The Atlantic Ocean is expanding at a greater rate than subducting • This is because of the low number of trenches in the Atlantic • Over time the entire ocean gets larger and pushes against the continents