Title: Powerpoint Presentation Physical Geology, 10e
1Plate TectonicsChapter 18-20
2Plate Tectonics
- Plate tectonics - Earths surface composed of
thick plates that move - Intense geologic activity is concentrated at
plate boundaries - Combination of continental drift and seafloor
spreading hypotheses proposed in late 1960s
3Review Three Types of Plate Boundaries
But how do we know that plates move at all ?
Transform Convergent
Divergent
(strike-slip)
(subduction) (spreading)?
4Early Case for Continental Drift
- Puzzle-piece fit of coastlines of Africa and
South America has long been known
5Early Case for Continental Drift
- In early 1900s, Alfred Wegner noted South
America, Africa, India, Antarctica, and Australia
have almost identical rocks and fossils
- Glossopteris (plant), Lystrosaurus and
Cynognathus (animals) fossils on five continents
- Mesosaurus (reptile) in Brazil and South Africa
only
6Early Case for Continental Drift
- Wegner reassembled continents into the
supercontinent Pangaea - Late Paleozoic glaciation patterns on southern
continents explained reconstruction into
(Pangaea) Gondwanaland
7Early Case for Continental Drift
- Coal beds of North America and Europe indicate
Laurasia super continent
- Continental Drift hypothesis initially rejected
- Wegener could not come up with viable driving
force - continents should not be able to plow through
sea floor rocks
8The Earth's Magnetic Field Can Give Us Clues
9Paleomagnetism and Continental Drift
-
- Paleomagnetism magnetic minerals align and dip
with Earth's internal magnetic field lines - Steeper dip angles indicate rocks formed closer
to the magnetic poles
- Rocks with increasing age point to pole locations
increasingly far from present magnetic pole
positions
10Paleomagnetism and Continental Drift Revived
- Apparent polar wander curves for different
continents indicate plate movement ! - Wegner was right!
11Plate Tectonics and the Scientific Method
How does an idea become a theory ?
When Wegner first suggest the idea of Plate
tectonics what was it ? a) theory b)
hypothesis c) data d) proof What data was
later acquired to test this ? When did plate
tectonics become an accepted theory ?
12The Scientific Method
Step 1 A question is asked Step 2 Gather
data Step 3 Use data to propose a
hypothesis (Has this hypothesis been
tested yet ? NO! Step 4 Make a prediction
(based on hypothesis)? Step 5 Test prediction
(with new data) Step 6 Hypothesis becomes a
theory ! Yeah! (if predictions
and tests are good)
13Banded rocks on the seafloor
14Seafloor Spreading
Magnetic anomalies found on the seafloor parallel
to the spreading axis with alternating
polarity. At the spreading center magma melted
above Curie Temp, cooled, crystalized and
realigned magnetic rocks with the Earth's
magnetic field. The plates move apart, then
began melting again....
15a
16Southern California Coast Continental Shelf
Continental shelf is cut by submarine canyons
that channel sediments to the deep ocean.
17Does the Earth Breath ?
Earthquakes recorded along the Juan de Fuca
spreading ridge indicate that microseismic eq.
events coincide each day with low
tide. Gravitational attraction of the Moon and
Sun on the Earth disturbs ocean water (very
fluid). Which tides give you the best surf ?
18Mountain Belts
- Mountain belts are chains of mountain ranges
1000s of km long - Located along the edges of continents
- As mountains grow higher and steeper, erosion
rates increase (from running water and ice )
19Continents Grow During the Subduction Process
20Continental Cratons
- Ancient mountain belts have eroded nearly flat to
form the stable core of a continent (craton or
shield)
- Every continental plate has a central, old,
craton.
21Growth of Continents
- Continents grow larger as mountain belts evolve
along their convergent margins - New accreted terranes can be added to older
cratons with each episode of convergence
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