Title: Plate Tectonics
1Plate Tectonics
2Plate Tectonics - Targets
- Describe tectonic plate movement, types of
boundaries and boundary features.
3Plate TectonicsPlate Movements7 major plates
usually named after continent or ocean which they
are on.
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5Plate Tectonics Vocab
- Lithosphere
- The rocky, rigid layer of the earth including the
crust and the upper mantle - Asthenosphere
- The plastic-like layer of the earth located
beneath the lithosphere
6Pieces of the lithosphere (plates) float on the
asthenosphere.
- Hot magma rises cooler magma sinks creating
convection currents (like boiling water)
7- Convection Current As a material heats (water,
magma, etc.) it rises, as it rises it cools, as
it cools it sinks, as it sinks it heats, as it
heats it rises. - It is a cycle that continues.
8Basalt high density
Granite low density
What happens when two plates collide?
9Plate Tectonics
- When plates collide or slide apart, volcanoes
earthquakes occur. - Most (90) volcanoes earthquakes occur in the
Ring of Fire around the Pacific Ocean.
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11Continental drift - Pangaea
12Is This Man Insane?
- Alfred Wegener (1880-1930)
- Created the Theory of Continental Drift around
1912 - Was not the first to suggest the idea, but was
the first to present and publish evidence - Most Scientists did not agree with his theory
until long after his death (until the 1960s)
13Is This Man Insane?
- Why didnt other scientists agree?
- Even though Wegener had extensive evidence that
the continents were once connected, he could not
explain what made the continents move. - He thought that the continents were moving
through the ocean floor, like icebreakers plowing
through ice sheets - He believed centrifugal forces (earths spinning)
and tidal forces (the pull of the moon and sun)
were responsible for moving the continents
14What evidence did Wegener Have?
1. Puzzle-like fit of the continents The
continental shelves of present-day continents
match up
15What evidence did Wegener Have?
- 2. Fossils
- fossils of identical plants and animals found on
opposite sides of the Atlantic - fossils found in areas that indicate a climate
utterly different from the climate of today - fossils of tropical plants, such as ferns and
cycads, are found today on the Arctic island of
Spitsbergen and Antarctica
16Fossils of Gondwanaland
17Fossils from Pangaea Animation
18What evidence did Wegener Have?
- 3. Mountains
- the Appalachian mountains of eastern North
America match with the Scottish Highlands - the distinctive rock strata of the Karroo system
of South Africa are identical to those of the
Santa Catarina system in Brazil
19What evidence did Wegener Have?
- 4. Glacial Evidence
- Glacial straitions (created by glacial movement)
are found in areas that are warm in the present
day. (Africa and Australia)
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21What might the Earth look like in 50 million
years?
22What might the Earth look like in 150 million
years?
23What might the Earth look like in 250 million
years?
http//science.nasa.gov/headlines/y2000/ast06oct_1
.htm
24Plate Tectonics Vocab
- Subduction
- when oceanic crust sinks into the mantle and is
recycled - Only occurs at Oceanic-Continental convergent and
oceanic-oceanic convergent boundaries
25- Paleomagnetism-
- Earths magnetic field has switched several times
in history and is recorded in rocks - Used to develop the theory of plate tectonics
- Shows a mirror image of magnetic strips on either
side of mid-ocean ridges
265 Types of Plate Boundaries
- Convergent Boundaries
- Continental-continental convergent
- Oceanic-continental convergent
- Oceanic-oceanic convergent
- 2. Divergent Boundaries
- 3. Transform Boundaries
27Continental-Continental Convergent (C-C)
- When two pieces of land collide, both are pushed
upwards because of the low specific gravity of
continental crust - Results in landforms such as Mountains
(Himalayas, Appalachians) - Can cause earthquakes and very rare volcanism
28Locations of C-C boundaries
The Rocky mountains.
The Appalachians mountains
The Himalayan mountains
29Oceanic-Continental Convergent
- When oceanic crust and continental crust collide,
the oceanic crust (higher density) subducts
underneath the continental crust (lower density) - Results in landforms such as
- Volcanic Mountains (Cascades Mountains in US,
Andes Mountains in S. America) - Trenches (Peru-Chile Trench)
- Commonly causes earthquakes and volcanism
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31Cascade Mountains
32Oceanic-Oceanic Convergent
- When two pieces of oceanic crust collide, the
older oceanic crust (higher density) subducts
underneath the younger continental crust (lower
density) - Results in landforms such as
- Volcanic Island Arcs (Japan, Phillippines,
Aleutian Islands) - Trenches (Marianas trench, Japan Trench)
- Commonly causes earthquakes and volcanism
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35Locations of O-O Convergent Boundaries
36Divergent Boundaries
- When magma comes to the surface at a rift or
mid-ocean ridge, creating new crust and causing
plates to move away from each other - Results in landforms such as mountains, mid-ocean
ridges (Mid-Atlantic Ridge), rift valleys
(African Rift Valley), and islands (Iceland) - Can cause earthquakes and volcanism
37Divergent Boundaries on Land
38Locations of Divergent Boundaries
39Rift Valley in Iceland
40Transform Boundaries
- Where two plates slide horizontally past each
other with no vertical movement - Same as Strike-slip and shear faults
- Results in landforms such as faults (San Andreas
Fault) - Can cause earthquakes and very rare volcanism
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42Locations of Transform Boundaries
San Andreas Fault
43Amount of Movement
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46Evidence of continental drift magnetic reversals
Oldest Rocks
Youngest Rocks
47Divergent boundary Example mid-ocean ridge
Convergent boundary Example Cascade mountains
(west USA)
48Transform boundary Example San Andreas Fault, CA
Fault crack in Earths crust where movement
occurs.
49Plate Boundaries
Where in the world can we find examples of each
boundary? What features would you expect at each
boundary?