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Plate Tectonics and Earthquakes ectives: Students will learn key terms associated wit plate tectonic processes. (Part A) Students will understand the specific plate motions associated with divergent, convergent, and transform plate boundaries (Part B) Students will gain a global view of EQ’s (where EQ’s typically occur). (Part C) Students will evaluate and apply concepts from lab parts A, B, and C to answer criti thinking questions. (Part D)
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Plate Tectonics and Earthquakes

Feb 24, 2016

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Plate Tectonics and Earthquakes. Objectives: Students will learn key terms associated with plate tectonic processes. (Part A) Students will understand the specific plate motions associated with divergent, convergent, and transform plate boundaries. (Part B) - PowerPoint PPT Presentation
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Page 1: Plate Tectonics and Earthquakes

Plate Tectonics and EarthquakesObjectives:• Students will learn key terms associated with plate tectonic processes. (Part A)

• Students will understand the specific plate motions associated with divergent, convergent, and transform plate boundaries. (Part B)

• Students will gain a global view of EQ’s (where EQ’s typically occur). (Part C)

• Students will evaluate and apply concepts from lab parts A, B, and C to answer critical thinking questions. (Part D)

Page 2: Plate Tectonics and Earthquakes

The Plate Tectonic Model

• The plate tectonic model describes surface features, geologic environments, and patterns of EQ’s and volcanism.• Ridged lithospheric plates (continents + ocean floor) ride along the soft layer (like hot wax) called the asthenosphere• Plates spread apart, collide, and slide past one another. • EQ’s, crustal deformation, and volcanism take place at plate boundaries.

EarthquakePatterns

VolcanismPatterns

lithosphere

Asthenosphere (upper mantle)

Page 3: Plate Tectonics and Earthquakes

Plate Boundaries

Divergent Boundary – plates move AWAY from each other

Convergent Boundary – plates move TOWARD each other

Transform Boundary – plates SLIDE past each other

Page 4: Plate Tectonics and Earthquakes

Divergent Boundary:• plate material separating

ocean plate divergence Extensional forcescreate EQ’s

continental divergence

Extension createsfaulting

• Earthquake activity

Page 5: Plate Tectonics and Earthquakes

Ocean-Cont Ocean-Ocean Cont-Cont

Convergent Boundary:• interaction of two plates moving toward one another

making contact– hence, collision or convergence• collisions produce earthquakes, volcanic activity, and

crustal deformation

Subduction zone Subductioin

zoneOregon-Washington

CoastAleutian Island(Alaska area)

Himalayan Mountains

Page 6: Plate Tectonics and Earthquakes

ocean-continent

ocean-ocean

cont-cont

• thinner and more dense plate subducts• subducted plates melt (160 km) below the surface, and magma rises• EQ’s occur along the subduction zone, and magma plumes rise• typically, the older plate will subduct (more dense) beneath younger plate material• melting plate material rises, creating volcanic arc systems• most EQ’s occur within the subduction zone

• two plates converge with the same density• same density prevents subduction• extensive deformation

• Earthquake activity

Page 7: Plate Tectonics and Earthquakes

Transform Boundary:• two plates are sliding past one another

• lack the spectacular features associated with divergent/convergent boundaries• marked by linear valleys (slices through the earth’s crust)• shallow-focused EQ’s occur along the slip area of the sliding plates

SAF

Page 8: Plate Tectonics and Earthquakes

Transform boundaries offsettingspreading ridges

• Typical EQ’s occur along the transform boundary. Earthquakes

Cross-sectional view of the SAFand associated LA faults

• SAF – transform motion• LA faults- vertical motion SAF-transform fault

Los Angeles

Page 9: Plate Tectonics and Earthquakes

What moves or drives the plates?What could Wegener have told the geological society?

Only a Model – Think Convection

Convection – heat transfer through a liquid or gas that results in circular movement of particles

Hot water rises

Cooler water sinks

Page 10: Plate Tectonics and Earthquakes

Rise

Fall

Earth Crust

mantlemantle

The Earth’s MantleCan you see the convection?

Page 11: Plate Tectonics and Earthquakes

Mantle operates like a “lava lamp,” producingswelling and shrinking of magma plumes.

Earth’s Surface

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Page 12: Plate Tectonics and Earthquakes

Latitude and Longitude• Where are you on earth?

Latitude/Longitude• a grid system used to locate features on

the earth’s surfaceLatitude: • parallel lines that move north

and south• 0o latitude = equator

Longitude:• meridian lines that move east

and west • 0o longitude is through Greenwich, England 11

Page 13: Plate Tectonics and Earthquakes

Los Angeles, Ca 350 N-lat, 1210 W-longSpokane, Wa 470 N-lat, 1180 W-longNew York, NY 420 N-lat, 750 W-long 12

Page 14: Plate Tectonics and Earthquakes

Latitude (+)Longitude (-)

Latitude (-)Longitude (-)

EastWest

North

South

Latitude (+)Longitude (+)

Equator

Prime M

eridianLatitude (Latitude (-)Longitude (+)

Page 15: Plate Tectonics and Earthquakes

A

B

C

DE

15 N-lat, -132 W-long

52 N-lat, 78 E long

-18 S-lat, -162 W-long-55 S-lat, -15 W-long

-25 S-lat, 136 E long

13

Page 16: Plate Tectonics and Earthquakes

Plate Tectonics Lab:• Part A: Plate tectonic definitions

• use lab text• use textbook resources in classroom

• Part B: Identification of plate boundaries• use lab text, colored pencils• use textbook resources in classroom

• Part C: Plotting EQ location• use provided long/lat handouts• use colored pencils

• Part D: Critical thinking questions• use parts A, B, and C and your

synthesizing brain.