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1 Lab 06 ONLINE LESSON

Lab 06 ONLINE LESSON

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Lab 06 ONLINE LESSON. If viewing this lesson in Powerpoint Use down or up arrows to navigate. If viewing this lesson in Flash Use the control bar to navigate. Do take notes as we peruse through this lesson…. Plate Tectonics. - PowerPoint PPT Presentation

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Page 1: Lab 06             ONLINE        LESSON

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Lab 06 ONLINE

LESSON

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If viewing this lesson in Powerpoint

Use down or up arrows to navigate

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If viewing this lesson in Flash

Use the control barto navigate

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Do take notes as we peruse through this

lesson…

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Plate Tectonics

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Plate Tectonics is a geologic idea that states

the surface of the planet is covered by a series of

rigid plates that move…

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These plates move away each other

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These plates move toward each other

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These plates move past each other

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Plate Tectonics is driven by heat within the interior

of the planet…

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A current theory suggests that radioactive materials are

the source for the earth’s internal heat…

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This heat melts the surrounding rock

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Melted rock (magma) rises to the surface and

pushes the plates…

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There are three types of plate boundaries

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Divergent, Convergent and

Transform

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Divergent boundary: the plates move away from

each other

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Convergent boundary: the plates move toward

each other

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Transform boundary: the plates move past each

other

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A transform boundary: cuts across a divergent

boundary…

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A divergent boundary is also referred to as a spreading center,

such as the Mid Atlantic Ridge…

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A divergent boundary is a part of the earth’s

surface where new crust is formed…

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A convergent boundary is also

known as a subduction zone…

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Subduction is the process of pushing

seafloor crust into the interior of the

planet…

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A convergent boundary is where

crust is destroyed and massive earthquakes

occur…

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A transform boundary is also known as a

fracture zone or fault…

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The San Andreas Fault is a well known transform fault in this area…

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Earthquakes occur at all of these

boundaries because solid rock is moving against solid rock…

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The bigger earthquakes occur at the convergent and

transform boundaries…

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But small and shallow earthquakes can

occur at transform and divergent boundaries…

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Shallow earthquakes occur at divergent

boundaries because the crust is thin…

5 -10 km thick…

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The following is a map of many

divergent, convergent and transform boundaries…

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Plate Tectonics can be thought of as a

grand unifying theory in geology…

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Meaning that many geologic phenomena are associated with

Plate Tectonics

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And can be explained by Plate Tectonics

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At convergent boundaries …volcanoes,

earthquakes and mountains and deep sea

trenches can be formed…

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Right click to play

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Also at convergent boundaries …the deepest

earthquakes occur

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Subducted seafloor is pushed into the interior of the

planet….

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As much as 650 kilometers

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At divergent boundaries …heat,

volcanoes, earthquakes and new

seafloor can be formed…

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Since new seafloor is formed at the divergent

boundaries…the notion of seafloor spreading can

also be observed…

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Seafloor crust is made primarily of iron rich (MAFIC)

minerals

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These MAFIC minerals are subject to the earth’s

magnetic field…

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Magma rises up from the interior of the planet…

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And punches through the ocean crust to form new

crust…

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The newly formed MAFIC crust can record the

prevailing magnetic field

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The earth’s magnetic field has changed direction over the course of the life of the

planet

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North has become south and the other way around…

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These magnetic reversals have been recorded in the

seafloor crust

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These records can tell us such things as the rate of movement of the plates…

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Each recorded event is a time marker…

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The newest crust is at the point where magma rises from the

interior of our planet…

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The older crust is further away…

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Oceanic crust as old as 200,000,000 years old can

be detected…

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How can spreading rates be determined from magnetic

reversals?

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Here is a section of the ocean floor’s magnetic

reversals…

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Seafloor spreading begins here…

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And ends up here…

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The distance of seafloor movement is read here…in

this case…1425 kilometers…

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The time is read here…in this case…78,000,000 years…

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Spreading rates are always noted in

cm/year

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1425 km = 142,500,000 cm

142,500,000 cm

78,000,000 years

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So the spreading rate is 1.83 cm/year

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Hot Spots are places on the planet where magma rises up to produce pinpoint

volcanic eruptions…

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There are about 40 hotspots on the planet…

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A hotspot can be described as a plume of magma rising up and punching through the crust…

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The Hawaiian Islands are an example of a hotspot…

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The hotspot plume is currently under the main island of

Hawaii…

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The Pacific Plate is moving northwest…

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The plates move while the plume is stationary…

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END

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