Upload
dora-mcdowell
View
223
Download
0
Tags:
Embed Size (px)
Citation preview
An InteractiveAdventure
Press Space Bar to Continue
To end session – Press Here
Level 1 – Earth’s Surface – The Lithosphere Level 2 – Earth’s Mantle - The Asthenosphere Level 3 – The Outer Core Level 4 – The Inner Core How do we KNOW these levels exist? Explore the Depths - Test Your Knowledge
The Lithosphere
The Lithosphere is the upper surface of the
earth composed of the SOLID upper mantle
which is made up of the earth’s crust including
bothOceanic Crust
andContinental Crust.Press to continue
The Lithosphere
The various Continental Plates
link together to make up the Lithosphere.
Press to continue
The Earth’s Mantle
The earth’s mantle actually exists in two distinct
layers. The upper Mantle is composed of rock with the consistency of plastic(like silly putty) called
The AsthenosphereThe Asthenosphere
The lower layer of the Mantle is rigid and solid.
Press to continue
The Earth’s Mantle
The AsthenosphereThe AsthenosphereThe continental plates drift over the soft asthenosphere as the heat of the earth’s core rises creating currents that Result inContinental Drift.
Press to continue
The Outer Core
The Outer Core of the Earth consists
of liquid rock composed of Iron with 12% sulphur silicon, oxygen,
nickel and potassium
Press to continue
The Inner Core
The Inner Core of the Earth consists of
SOLID rock composed of Iron
with 10-20% nickel.
Some physicists believe that the movement of
electrical charges between the inner and outer core produce the earth’s magnetic field. Press to continue
How do we KNOW these levels exist?Seismologists study Earthquakes. Earthquakes produce shock waves
that travel through the earth and can be measured on the other side of the
earth.
P waves (primary waves) go through solid and liquid.
The vibrate differently passing through solids than when they pass in
liquid.S waves (secondary waves)
only go through solids.
Press to continue
How do we KNOW these levels exist?
P waves (primary waves) go through solid and liquid. They vibrate differently passing through solids than when they pass in
liquid.S waves (secondary waves)
only go through solids.
Press to continue
A. Level 1 – The LithosphereB. Level 2 – The AsthenosphereC. Level 3 – The Outer CoreD. Level 4 – The Inner Core
Please “CLICK” on the Correct Answer
CORRECT… Way to GO!!!
Press to continue
OH NO… Good Shot – TRY AGAIN!
Press to continue
A. Level 1 – The LithosphereB. Level 2 – The AsthenosphereC. Level 3 – The Outer CoreD. Level 4 – The Inner Core
Please “CLICK” on the Correct Answer
CORRECT… Way to GO!!!
Press to continue
OH NO… Good Shot – TRY AGAIN!
Press to continue
A. Level 1 – The LithosphereB. Level 2 – The AsthenosphereC. Level 3 – The Outer CoreD. Level 4 – The Inner Core
Please “CLICK” on the Correct Answer
CORRECT… Way to GO!!!
Press to continue
OH NO… Good Shot – TRY AGAIN!
Press to continue
A. Level 1 – The LithosphereB. Level 2 – The AsthenosphereC. Level 3 – The Outer CoreD. Level 4 – The Inner Core
Please “CLICK” on the Correct Answer
CORRECT… Way to GO!!!
Press to continue
OH NO… Good Shot – TRY AGAIN!
Press to continue
A. Level 1 – The LithosphereB. Level 2 – The AsthenosphereC. Level 3 – The Outer CoreD. Level 4 – The Inner Core
Please “CLICK” on the Correct Answer
CORRECT… Way to GO!!!
Press to continue
OH NO… Good Shot – TRY AGAIN!
Press to continue
A. Level 1 – The LithosphereB. Level 2 – The AsthenosphereC. Level 3 – The Outer CoreD. Level 4 – The Inner Core
Please “CLICK” on the Correct Answer
CORRECT… Way to GO!!!
Press to continue
OH NO… Good Shot – TRY AGAIN!
Press to continue
Thank you for using this Tutorial
Resources
Unless indicated otherwise, all scientific information and graphics are taken fromMonroe, J., Wicander, R., and Hazlett, R. (2007) Physical Geology: Exploring the Earth.
6th Edition. California: Thomson Brooks/Cole.
“Major Tectonic Plates of the World” graphic retrieved April 13, 2008 from http://rst.gsfc.nasa.gov/Sect2/F1-15.jpg
Continental “Convection Currents” graphic retrieved April 13, 2008 from http://www.stvincent.ac.uk/Resources/EarthSci/Tectonics/images/convection.gif