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Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

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Sea-Floor CH 4 Prentice Hall p.123-129 Spreading
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Page 1: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

Sea-FloorSea-Floor

CH 4 Prentice Hallp.123-129

CH 4 Prentice Hallp.123-129

SpreadingSpreading

Page 2: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.
Page 3: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

• Harry Hess- American Geologist• 1960- Proposed Sea-Floor

Spreading– The process that continually adds

new material to the ocean floor.– Occurs at the mid-ocean ridge, • new material rises from the mantle

and erupts. • The molten material spreads out

pushing older rock to the side.

Sea-Floor Spreading

CD RiftEvidence

Page 4: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

• Occurs at the mid-ocean ridge, new material rises from the mantle and erupts.

• The molten material spreads out pushing older rock to the side.

Sea-Floor Spreading

CD RiftEvidence

Page 5: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

• 1900’s Scientists Mapped the Ocean Floor

• Used Sonar- a device that bounces sound waves off of underwater objects and records echoes of the sound waves.

ClimateMapping the Ocean Floor

Page 6: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

ClimateMapping the Ocean Floor

• Mapped the Mid-Ocean Ridge– East Pacific Rise– Mid-Atlantic Ridge• Rift Valley, a central valley twice as deep as Grand

Canyon

Page 7: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

• Alvin- a submersible unit traveled to the central valley of the mid-ocean ridge.– Found Pillow Lava• Indicates that new molten material has formed.• It cooled quickly underwater

Molten Material

Page 8: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

Life Around the Mid-Ocean Ridge

Page 9: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

Parts of the Ocean Floor

CD RiftEvidence

Page 10: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

Magnetic Reversals

• Earth has a Magnetic North and a South Pole

• The poles have reversed in the past.

• The reversals are recorded in the igneous rock.– Serve as a record of the

magnetic field. CD RiftEvidence

Page 11: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

Magnetic Reversals• Basalt contains iron• The bits of iron line up in the direction of the

poles.• When the rock hardens completely, the

direction of the poles is recorded in the rock.– Permanent “magnetic memory”

CD RiftEvidence

Page 12: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

• Glomar Challenger- A drilling Ship– Drilled through 6km of

water.– Determined that the age

of the rock was younger at the ridge and older away from the ridge.

– Shows that sea floor spreading is taking place.

Drilling the Ocean Floor

CD RiftEvidence

Page 13: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

The Ocean Floor

Page 14: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

Convection and Sea

Page 15: Sea-Floor CH 4 Prentice Hall p.123-129 CH 4 Prentice Hall p.123-129 Spreading.

The Ocean Floor


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