1. Sea-Floor Spreading Chapter 1, Section 4 Pages 33-39

2. The Mid-Ocean Ridge The longest chain of mountains in the world The longest chain of mountains in the world Extends into all of Earth’s Oceans Extends into all of Earth’s Oceans Most of the mountains lie under the ocean Most of the mountains lie under the ocean In the mid 1900’s, scientists used sonar to map it In the mid 1900’s, scientists used sonar to map it

3. Evidence for Sea-Floor Spreading Harry Hess proposed the following in 1960: Harry Hess proposed the following in 1960: 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. 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.

4. Evidence 1 Molten Material Molten Material Alvin (A submarine) and its crew found molten material that had quickly hardened after erupting under water Alvin (A submarine) and its crew found molten material that had quickly hardened after erupting under water

5. Evidence 2 Magnetic Stripes Magnetic Stripes Reversal of magnetic field causes iron in ocean floor to line up in the direction of Earth’s magnetic poles Reversal of magnetic field causes iron in ocean floor to line up in the direction of Earth’s magnetic poles When the poles are reversed, the iron faces the opposite direction causing “stripes” in the ocean floor When the poles are reversed, the iron faces the opposite direction causing “stripes” in the ocean floor

6. Evidence 3 Drilling Samples Drilling Samples The Glomar Challenger, a drilling ship in 1968 gathered samples of the ocean floor The Glomar Challenger, a drilling ship in 1968 gathered samples of the ocean floor The age of the rock from the samples were older the farther away they got from the Mid-ocean ridge. The age of the rock from the samples were older the farther away they got from the Mid-ocean ridge.

7. Subduction at Deep-Ocean Trenches A deep-ocean trench forms where the oceanic crust bends downwards. A deep-ocean trench forms where the oceanic crust bends downwards. Subduction is the process by which the ocean floor sinks beneath a deep- ocean trench and back into the mantle Subduction is the process by which the ocean floor sinks beneath a deep- ocean trench and back into the mantle

8. Subduction-cntd. Convection currents push new crust at the M.O.R. away from the ridge and towards Convection currents push new crust at the M.O.R. away from the ridge and towards New crust is hot, but it cools and becomes more dense, getting bulled below the trench New crust is hot, but it cools and becomes more dense, getting bulled below the trench At deep-ocean trenches, subduction allows part of the ocean floor to sink back into the mantle, over tens of millions of years At deep-ocean trenches, subduction allows part of the ocean floor to sink back into the mantle, over tens of millions of years

9. Subduction and Earth’s Oceans Pacific Ocean- it is shrinking because subduction is happening faster than new crust is being added Pacific Ocean- it is shrinking because subduction is happening faster than new crust is being added Atlantic Ocean- it expanding because new crust is being faster than subduction Atlantic Ocean- it expanding because new crust is being faster than subduction