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Ch 9 Notes Mr. Russo Beaumont High School

Mr. Russo Beaumont High School Divergent boundary Convergent boundary Transform fault boundary Oceanic Ridge Rift Valley Seafloor Spreading

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Page 1: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Ch 9 NotesMr. Russo

Beaumont High School

Page 2: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Divergent boundary Convergent boundary Transform fault

boundary Oceanic Ridge Rift Valley Seafloor Spreading

Subduction Zone Trench Continental Volcanic

Arc Volcanic Island Arc Paleomagnetism Hot Spot

Ch 9 Vocab Matrix (Pg 45)

Page 3: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

We will be able to describe the 4 pieces of evidence for the theory of continental drift.

Objective: Ch 9.1 Pg 47

Page 4: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Continental Drift – The continents had once been joined to form a single supercontinent◦Proposed by Alfred Wegner

Continental Drift

Page 5: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Pangaea – The supercontinent (All Land)◦Continents broke apart and drifted to their current position

Pangaea

Page 6: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Continental Puzzle – Continents appear to form a puzzle that can be put together

What evidence supports continental Drift?

Page 7: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading
Page 8: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Matching Fossils – Several of the same types of fossils on different landmasses

What evidence supports continental Drift?

Page 9: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Rock Types and Structures – Mountain belts that end on one coastline seem to reappear on a landmass across the ocean

What evidence supports continental Drift?

Page 10: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Ancient Climates – Found evidence of glacial ice in countries that shouldn’t have any glaciers

What evidence supports continental Drift?

Page 11: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading
Page 12: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Objective

Page 13: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

The upper mantle and the crust act like a strong rigid layer. ◦This layer is called the lithosphere

Ch 9.2What is the theory of plate tectonics?

Page 14: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

The lithosphere lies on top of the weaker mantle called the ASTHENOSPHERE

Page 15: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Plate – Plates are sections of the lithosphere◦7 Major plates◦Largest – Pacific Plate

◦Plates move 5cm/yr

Plates

Page 16: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Convergent

Divergent

Transform

What are the 3 types of plate boundaries?

Page 17: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Divergent Boundary – Occur when two plates move apart

Example – East African Rift Valley

Divergent Boundary

Page 18: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Example – East African Rift Valley

Page 19: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Convergent boundary – Occur when two plates move together

Convergent Boundary

Page 20: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Transform Boundary – When two plates grind past each other◦Example – San Andreas

Transform Boundary

Page 21: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Every Plate contains all 3 types of boundaries

Page 22: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Oceanic Ridge – Elevated area in the ocean, found along divergent boundaries

Ch 9.3Oceanic Ridge

Page 23: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Rift Valley – Deep faults found along divergent boundaries

Rift Valley

Page 24: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Seafloor Spreading – The process by which plate tectonics produce new lithosphere

Oldest part of the ocean floor is 180 million years old.

Seafloor Spreading

Page 25: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Subduction Zone – When one plate is forced down beneath another plate. (Convergent Boundary)

Subduction Zone

Page 26: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Trench – Surface Feature produced during a subduction zone.

Trench

Page 27: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Continental Volcanic Arc – When a continental and ocean plate collide, they produce volcanoes on the land.

Continental Volcanic Arc

Page 28: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Volcanic Island Arc – When 2 ocean plates collide, they produce volcanoes in the middle of an ocean, forming islands

Volcanic Island Arc

Page 29: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Mountains are formed when two continent plates collide.

Example – Himalayas in South Asia

Mountains

Page 30: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Transform Fault – Earthquakes – At Transform faults, plates grind past without destroying the lithosphere and produce earthquakes.

Example – San Andreas Fault , CA

Transform Fault - Earthquakes

Page 31: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Convergent Boundaries – Lithosphere is destroyed

Divergent Boundaries – Lithosphere is created

Transform Boundaries– Lithosphere is neither created nor destroyed.

Notice

Page 32: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Paleomagnetism – Study of changes in Earth’s magnetic field

Ch 9.4Paleomagnetism

Page 33: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Normal Polarity – Same magnetism as present day magnetic field

Normal Polarity

Page 34: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Reverse Polarity – Rocks that show opposite magnetism then present day

Reverse Polarity

Page 35: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

The discovery of strips of rocks of alternating polarity across the ocean ridges.

What evidence supports theory of plate tectonics?

Page 36: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

The youngest crust (Seafloor) is at the ridge crest, the oldest crust is further away

How old is the seafloor?

OldestYoungest

Page 37: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Hot Spot – A rising plume of mantle that creates a volcanic area (Hawaii)

Hot spot supports idea that the plates move over Earth’s surface

Hot spot

Page 38: Mr. Russo Beaumont High School  Divergent boundary  Convergent boundary  Transform fault boundary  Oceanic Ridge  Rift Valley  Seafloor Spreading

Shaded Region – Reverse Polarity

White Region – Normal Polarity