Earth Shaping Chapter 16. Earth Shaping Theory It was a gradual change over time. In early...
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![Page 1: Earth Shaping Chapter 16. Earth Shaping Theory It was a gradual change over time. In early 1900’s Alfred Wegener proposed the theory of continental.](https://reader031.fdocuments.in/reader031/viewer/2022032604/56649e5c5503460f94b5496f/html5/thumbnails/1.jpg)
Earth ShapingEarth ShapingChapter 16Chapter 16
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Earth Shaping TheoryEarth Shaping Theory It was a gradual change over time. In early 1900’s Alfred Wegener proposed the
theory of continental drift. Scientist DID NOT support his theory
because at that time he could not explain his theory.
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Current Continental Drift Current Continental Drift TheoryTheory
The earth is constantly changing. In addition to the effects of weathering and erosion, there are much larger scale changes occurring due to the movement of large plates in the lithosphere.
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HOW DO WE KNOW HOW DO WE KNOW THIS?THIS?
Wegener developed his idea based upon 4 different types of evidence:
1. Fit of the Continents
2. Fossil Evidence
3. Rock Type and Structural Similarities
4. Paleoclimatic Evidence
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Earth’s Earth’s LayersLayers
Inner Core - made of ironInner Core - made of iron
Outer Core–molten(liquid)Outer Core–molten(liquid)
Mantle – most of Earth’s massMantle – most of Earth’s mass
Crust- rocky and brittle, can fractureCrust- rocky and brittle, can fracture
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How do we know?How do we know?Measuring seismic wavesMeasuring seismic waves
The speed of the wave determines the type The speed of the wave determines the type of rock it is traveling throughof rock it is traveling through
Do waves travel faster in solids or liquids? Do waves travel faster in solids or liquids?
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TWO TYPES OF CRUSTS:TWO TYPES OF CRUSTS:
Oceanic – thin, dense rockOceanic – thin, dense rock
Continental- thick, low densityContinental- thick, low density
LITHOSPHERE-Outer LITHOSPHERE-Outer part of the crust; part of the crust; divided into divided into tectonic platestectonic plates
ASTHENOSPHERE- ASTHENOSPHERE- the tectonic the tectonic plates are on the plates are on the asthenosphereasthenosphere
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Plate MovementPlate MovementContinental Drift – the movement of the Continental Drift – the movement of the
tectonic platestectonic plates
Theory -Theory -that continents drift apartthat continents drift apart
*Proposed by Alfred Wegner *Proposed by Alfred Wegner *Fossil evidence*Fossil evidence
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Sea Floor SpreadingSea Floor SpreadingMagma Rises in mid –ocean ridges or cracks called Magma Rises in mid –ocean ridges or cracks called
fissuresfissures
1. Forms new crust1. Forms new crust
2. Moves horizontally2. Moves horizontally
3. Older crust moves further out 3. Older crust moves further out
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Magnetic ReversalsMagnetic Reversals Earth’s north and south Earth’s north and south
magnetic poles change magnetic poles change placesplaces
Can be seen in the Can be seen in the oceanic crustoceanic crust
Magnetic minerals align Magnetic minerals align with magnetic fieldwith magnetic field
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SupercontinentSupercontinent
Pangea – all of the Pangea – all of the continents were continents were joined togetherjoined together
Gradually drifted Gradually drifted apart over time.apart over time.
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Plate Tectonic TheoryPlate Tectonic Theory3 Possible Forces3 Possible Forces
Ridge PushRidge PushConvectionConvectionSlab pull/SubductionSlab pull/Subduction
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Ridge PushRidge Push – –
gravity causes gravity causes oceanic crust oceanic crust (lithosphere) to (lithosphere) to sink, subsidencesink, subsidence
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Convection Slab PullConvection Slab Pull Hot rock rises while Hot rock rises while
cool rock sinks cool rock sinks Causes the Causes the
lithosphere to move lithosphere to move sidewayssideways
Subduction Zone- when Subduction Zone- when oceanic lithosphere (crust) oceanic lithosphere (crust) is more dense causing the is more dense causing the edge to sink and pull the edge to sink and pull the rest of the plate with itrest of the plate with it
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African, North American, South American, Eurasian, Australian, African, North American, South American, Eurasian, Australian, Antarctic, and Pacific plates. Several minor plates also exist, Antarctic, and Pacific plates. Several minor plates also exist, including the Arabian, Nazca, and Philippines plates. including the Arabian, Nazca, and Philippines plates.
7 Tectonic Plates
MOVEMENT: MOVEMENT:
*Different *Different directions & directions & speedsspeeds
*2-10cm per year *2-10cm per year (the speed your (the speed your fingernails grow)fingernails grow)
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Plate BoundriesPlate Boundries Convergent – come togetherConvergent – come together Divergent – pull apartDivergent – pull apart Transform – slide past each otherTransform – slide past each other
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ReviewReview
Magma moves in _______Magma moves in _______
currents due to change in currents due to change in temperatures.temperatures.
convection
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When rock layers come together it is a When rock layers come together it is a ________________
boundary.boundary.
When they pull apart it is a When they pull apart it is a
_________ boundary._________ boundary.
boundary.boundary.
convergent
divergent
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Tectonic plates are large pieces of Tectonic plates are large pieces of ______________________
A rock is made of 2 or more A rock is made of 2 or more ________________________
lithosphere
minerals
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1
2
3
What rock type is at 1?What rock type is at 2?What rock type is at 3?