continental crust vs. oceanic crust

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CONTINENTAL CRUST vs. OCEANIC CRUST. Solar Wind. Earth or Ocean. How many oceans?. Continental Drift. Alfred Wegner 1912 German geophysicist. Super continent:. Pangea. Panathalassa. 2 sections:. Laurasia. Gondwanaland. Problem with Wegner’s theory:. Finally accepted in :. - PowerPoint PPT Presentation

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CONTINENTAL CRUST vs. OCEANIC CRUST

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Solar Wind

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Earth or Ocean

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How many oceans?

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Continental Drift

Alfred Wegner 1912 German geophysicist

Super continent: Pangea Panathalassa

2 sections: Laurasia

Gondwanaland

Problem with Wegner’s theory:

Finally accepted in : 1960

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Why no one believed him?

1. Wegner said the continents could plow through the continental crust.

2. Said the continents moved because of the gravitational pull of sun and moon.

3. Said the spinning of the earth also caused continents to move.

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Mid Ocean Ridge

Post WW II b/c of sonar use to track submarines

Cmdr. Harry Hess leaves sonar on full time

Mtns. avg 1.5 miles high

Responsible for creating …..

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EVIDENCE the CD occurred• Glacial Evidence:– 300 million year old Glacial remains found in India,

Africa, Australia, S. America– Whole world covered with ice?

These continents used to be located at the north and south poles

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Fossil evidence

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More evidence• Palm tree fossils found in Arctic regions

• Coral fossils found in present day cold climates

• Maps of continent locations

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Magnetic reversals

Molten rock contains: MAGNETITE

animate

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Sea floor spreading

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Age of the sea floor confirmation

GLOMAR EXPLORER

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Types of ocean sediments: 4Lithogenous

Hydrogenous

Biogenous

Cosmogenous

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Ocean Sediment details

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Project Nekton

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HRE??

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Continental vs. Oceanic

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Divergent Boundaries

Convergent Boaundaries

Plate Movements

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Transform Boundaries

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Continental Margin

Continental Shelf:Gentle angleSm. Pt. of Oceans½ mile – 450 mile wideVERY rich in sea life

Continental Slope:Actual boundary of the continentsVery steep angle

Continental Rise:Where the sedimenthas accumulated

Abyssal Plain:Deep sea floorHas:Hills, guyotsvolcanoes

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Active vs. Passive margins

Steep shelf, slope and there is no riseLots of Earthquake and volcanic activityEx. Western edge of S. American coast

Wide Shelf, gentle slope, long rise, lots of sedimentGeologically inactive b/c no plates are subductingEx. East coast USA

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mid ocean ridge and hydrothermal vents

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