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-Floor Spreading, ,& Plate Boundaries

Lecture 21

Prop: Test 3 Invitations

Alfred Wegener’s Evidence for Continental Drift

1. Continental “Fit” 2. Similar Rocks, Ages 3. Similar Fossils 4. Widespread Glaciation

Pangaea = Gondwanaland + Laurasia

Source: http://vishnu.glg.nau. edu/rcb/Penn.jpg

1 Alfred Wegener’s Evidence for Continental Drifts Was NOT Accepted in USA. Problem: No Mechanism for Continents to Plow Through

Answer lies on & in the Sea Floor - Ch. 18 + 19 in Text

WW II

http://www.geocities.com/Pentagon/2560/bowph1.jpg http://www.spe.sony.com/movies/da sboot/ Submarine Science Mapping of Basins

http://members.microdsi.net/shirschm/Welcome.index.html

Seismic & Sonar Study Reveals Sea-Floor Topography Geophysicists’s Answers Life’s Important Questions

Spongebob Theme Song Lyrics

Are ya ready kids? Aye Aye Captain! I CAN'T HEAR YOU! AYE AYE C APTAIN! ohhhhhh!!!!

Who lives in a pineapple under the sea? SPONGEB OB SQUAR EPANTS! Absorbant and yellow and poreous is he SPONGEB OB SQUAR EPANTS! His nautical nonsense be somethin you wish SPONGEB OB SQUAR EPANTS! Then drop on the deck and flop like a fish! SPONGEB OB SQUAR EPANTS! Ready?

SPONGEB OB SQUAR EPANTS! SPONGEB OB SQUAR EPANTS! SPONGEB OB SQUAR EPANTS!

SPONGEYB OB SQUAR EPAAAANTS

2 Know these mega-scale • Continental Slope • Continental Rise • • Mid-Ocean Ridge (~ Mid-Ocean Rise) • Trench

Know differences between Oceanic Crust and Continental Crust

Ocean Basin See Figures 18.5 to 18.16 in Plummer & Others 10th ed.

Ocean Basin Bathymetry See Figures 18.5, 18.15 in Plummer & Others 10th ed.

3 Cold War More Submarine Science Magnetic Anomalies in Ocean Basin

Deep-Sea Magnetic Anomalies

Deep Sea Drilling Project (DSDP) Studied Geology of Ocean Basins Continental Record = Incomplete Deep Ocean Basin Record Was Thought to be More Complete Glomar Challenger Harry Hess

4 Magnetic Anomalies: Atlantic Ocean South of Iceland New Ocean Crust Created at Mid-Ocean Ridges: Spread Centers

DSDP Surprise Finding:

Ocean Basins are <200,000,000 y Old Much Younger than the Continents

Very Young at the Mid Ocean Ridges

Age of the Ocean Basins

5 Birth of an Ocean Basin?

Spreading at the Red Sea: Break-Up of Asia and Africa

Note a “Failed” Arm of Rifting in East Africa

Break-Up of a Continent and Origin of an Ocean Basin

Problem:

If New Crust is Created at Mid- Ocean Ridges,

Where is Old Crust Consumed to Balance the New Crust?

6 Where is Old Crust Consumed to Balance the New Crust?

Answer Lies in Deep-Focus .

Earthquakes Occur in Brittle (Elastic) Lithosphere

Lithosphere 70 - 100 km Asthenosphere

Distribution of All Earthquakes (Deep and Shallow Focus)

7 Subduction Zones: Ocean-Ocean Margin

Subduction Zones: Ocean-Continent Margin

Deep-Focus Quakes Only in Subduction Zones

8 Isotherms in Subduction Zones

400o C

600o C

Japan Trench &

Back-Arc and Fore-Arc “Basins” See Figure 19.35 in Plummer & Others 9th ed.

9 Subduction Zones & Volcanoes

Spread Centers Feed Subduction Zones

Missing Mechanisms for Continental Drift: Sea Floor Spreading & Subduction

Continents are Passive “Boats”

10 How Are Mountains Built? First a Brief Review of Sea Floor Spreading

Himalayas

Break-Up of a Continent and Origin of an Ocean Basin

Missing Mechanisms for Continental Drift: Sea Floor Spreading & Subduction

Continents are Passive “Boats”

11 Spread Centers Feed Subduction Zones

Subduction Zones: Ocean-Ocean Margin

Subduction Zones: Ocean-Continent Margin

12 Orogeny (Mountain Building) in the Himalayas

Continental Lithosphere Will NOT Flush Down Subduction Zones

Orogeny in Himalayas

13 Orogeny in Himalayas

Orogeny in the Himalayas

Orogeny - Mountain Building - Supply

14 Orogeny - Mountain Building - Glaciation

Plate Margins:

• Spread Centers (Mid-Ocean Ridges) • Subduction Zones (Trenches) • Transform Faults

Plate Margins:

15 Transform Faults & Fracture Zones

Transform Faults

San Andreas Fault: Right-Lateral

Left-Lateral Offset!! Why?: Fault is Produced by Offset, vs. Offset Produced by Fault

16 Transform Faults: Three Causal Scenarios

Plate Motion on a Sphere

Plate Motion on a Sphere Requires Transform Faults Because of Different Rates of Motion

17 The Plates

The Plates: Pacific-Centered View (Distorted by Mercator Map Projection)

What Drives Plate ?

1. Convection Cells in Mantle 2. Sinking of Cool, Dense Plates 3. Mantle Plumes - Hot Spots

18 Convection Cells

Convection Cells in Mantle

19 Mantle Plumes

Mantle Plumes Under Continents

20 • Known “Hot Spots”

Hawaiian Islands

Mantle Plumes - Hot Spots

Numbers = Age of Rock in Millions of Years

21 Sinking of Cool, Dense Plates

Seamount

Volcanoes Surrounded by Fringing Coral Reefs

Atolls: Submerged Volcanos Support Reefs Only in Warm Clear Tuamoto Islands NASA

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