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Tiêu đề Seafloor Features and Plate Tectonic Boundaries
Trường học University of Oceanography and Geography
Chuyên ngành Geography and Oceanography
Thể loại Lecture Note
Năm xuất bản 2023
Thành phố Sample City
Định dạng
Số trang 37
Dung lượng 1,56 MB

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Nội dung

slope Abyssal plain Continental rise Continental slope Seafloor Features: Continental Margins Abyssal plain... Abyssal Hills linear hills Seafloor spreading center e.g., East Pacific R

Trang 1

Today’s Tunes

Fathoms Below / Under the Sea

From soundtrack of Disney’s The Little Mermaid

Trang 2

Continental shelf

Submarine canyons (cut into the c slope)

Abyssal

plain

Continental rise

Continental slope

Seafloor Features: Continental Margins

Abyssal

plain

Trang 3

Abyssal Hills (linear hills)

Seafloor spreading center (e.g., East Pacific RISE or Mid-Atlantic RIDGE)

Deep Ocean

Trang 4

Seafloor Features: Deep Ocean

Plate Tectonic Boundaries

Transform Faults, Fracture Zones

Trang 5

The Shifting Crust

Trang 6

Continental Drift

Alfred Wegener -1912

– large “supercontinent” (Pangea) existed and

then split into pieces

– fossil & glacial deposit evidence

Wegener not able to provide MECHANISM for his theory

Major mechanism later found in the OCEANS

Trang 7

Seafloor Spreading &

Plate Tectonics

Harry Hess - 1960s

– new ocean basins form from volcanism

– ocean floor forms IN BETWEEN pieces that

have split

– SEAFLOOR SPREADING

Trang 8

Seafloor Spreading &

Plate Tectonics

Theoretical breakthrough

– PLATE TECTONICS

– surface of earth composed of “plates”

( LITHOSPHERE ) that move on a “conveyor belt” ( ASTHENOSPHERE )

Trang 10

Evidence for Continental Drift

Fit of the continents

Correlation of mountain belts

Diversity of species

correlation of dinosaur species (Pangea)

isolation of mammal species (after breakup)

Glaciers

Trang 11

Important Quote

“Relationships known since early in the century yet the validity of continental drift was not generally recognized until the late 1960’s”

It took ocean floor data to solidify ideas and convince scientific community!

The oceans rule!

Trang 13

One Mechanism

seafloor-spreading

lithosphere

asthenosphere

Trang 15

Another Mechanism

subduction

world’s most explosive volcanos are formed over

subduction zones

Oregon’s Cascades Mtns over Cascadia Subduction Zone

– Juan de Fuca plate under N American plate

Trang 16

“Munch and Crunch”

“MUNCH” - subduction of oceanic plate under continent or ocean

– oceanic crust is thin and dense

– dives

“CRUNCH” - collision of continental plates

– India into Tibet and China

– continental crust is thick and light

Trang 18

Sliding By

Transform faults

– plates neither created nor destroyed

Transform faults are active

Fracture zones are inactive extensions of transforms

– “fossil transforms”

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Young & Old

Oldest seafloor - 200 million years

Oldest land - billions of years

With seafloor spreading, is the earth expanding?

Why is seafloor so young relative to continents?

SUBDUCTION

“law of conservation of ocean floor”

Trang 23

Divergent Plate Boundaries

Divergent - seafloor spreading

– mid-ocean ridges or rises

– Mid-Atlantic RIDGE, East Pacific RISE

Trang 24

Translational - strike-slip faulting

– transform faults (active) - San Andreas Fault – fracture zones (inactive) - Mendocino FZ

Trang 25

downgoing plate breakage causes earthquake

like potato chip breaking off in bean dip

Trang 28

Extra Slides not covered in lecture, but cover valuable info that can help in lab too

Trang 29

Proof for Seafloor Spreading

What made people believe in seafloor spreading? (poor Wegener!)

changes in inclinations of magnetic field

Earth’s magnetic field a mystery

currents in liquid core one hypothesis

Trang 31

SF Spreading Proof - 2

Earth’s magnetic field flips back & forth

magma freezes magnetic minerals

minerals lines themselves up w/ prevailing field of earth

anomaly in field is the key - normal (positive) or reversed

(negative)

Vine and Matthews noted this in the ‘60s and flagged this as PROOF for seafloor spreading

Trang 33

200 Ka

Trang 37

Driving Forces

“Slab pull” versus “ridge push”

Ridge Push - rising, hot rock pushes plates apart at spreading center

Slab Pull - gravity pulls cooled, dense

plates back down into mantle at

subduction zone

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