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Sea Floor Spreading Chapter 1-4
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Sea Floor Spreading Chapter 1-4.

Jan 17, 2018

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Noah Powell

Mid Ocean Ridges Mapped by sonar in mid 1900’s Curve like seams on a baseball along the sea floor Extend across all oceans Some are completely under water Some poke through Iceland
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Page 1: Sea Floor Spreading Chapter 1-4.

Sea Floor Spreading

Chapter 1-4

Page 2: Sea Floor Spreading Chapter 1-4.

Mid Ocean Ridges

• Mapped by sonar in mid 1900’s

• Curve like seams on a baseball along the sea floor

• Extend across all oceans• Some are completely

under water• Some poke through – Iceland

Page 3: Sea Floor Spreading Chapter 1-4.

How were these ridges formed?

• Studied by American geologist Harry Hess in 1960’s

• Thought Wegner may have been right

• Proposed idea of sea floor spreading

Page 4: Sea Floor Spreading Chapter 1-4.

Sea Floor Spreading• Sea floor spreads apart at

mid ocean ridge as new crust is added.

• Molten material erupts from ridge, cools into a strip of new rock

• Older rock moves outward as it is replaced by new molten rock

• Cause ocean floors to move like conveyor belts carrying continents with them

Page 5: Sea Floor Spreading Chapter 1-4.

Evidence from Molten Material

• Pillow shaped rocks found along mid ocean ridge by the crew of the submarine Alvin.

• Rocks can only be formed by molten material that cools quickly under water.

Page 6: Sea Floor Spreading Chapter 1-4.

Evidence from Magnetic Stripes

• Scientists pattern of magnetized “stripes” of rock on ocean floor

• Hold record of reversals of Earth’s magnetic field

Page 7: Sea Floor Spreading Chapter 1-4.

Evidence from Drilling Samples

• Drilling ship Glomar Challenger brought up samples from ocean floor that showed rocks further away from ridge were older and closer rocks were younger

Page 8: Sea Floor Spreading Chapter 1-4.

Why doesn’t the ocean floor keep on getting wider

• Part of the ocean floor sinks back into the mantle at deep ocean trenches by the process of subduction

Page 9: Sea Floor Spreading Chapter 1-4.

Subduction

• As new, hot oceanic crust moves away from the mid ocean ridge, it cools down and becomes more dense.

• Gravity causes denser crust to sink down into trenches

Page 10: Sea Floor Spreading Chapter 1-4.

Subduction and the Earth’s Oceans

• Ocean floor is renewed about every 200 million years because of seafloor spreading and subduction.

• Pacific Ocean is shrinking because it’s numerous trenches are swallowing more crust than is being formed

• Atlantic ocean is growing because it has less trenches