Earthquake Internet Project
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Compared to the rest of the planet, the Earth's solid crust is incredibly thin - like the skin of an apple. If you started drilling in your backyard, you would go through 25-40 miles of this solid rock - which sounds like a lot, except that after that you would hit 1,800 miles of very hot liquefied metal before reaching the planet's solid core.
Check out this site to learn more about the layers of the Earth:
http://volcano.und.edu/vwdocs/vwlessons/lessons/Earths_layers/Earths_layers2.html
So the land we walk on is really just a thin, brittle crust floating on a huge ball of molten goo. Or, more accurately, it's a bunch of pieces of crust, called plates, sliding around on goo (very slowly), rubbing against each other. Where these plates meet, you'll find faults -- breaks in the Earth's crust where the blocks of rock on each side are moving in different directions, in sudden starts and stops.
Land along faults will stay stationary for years, even decades at a time, building up pressure When enough pressure builds, the land will shift abruptly and with great force. The result is an earthquake.
For more information about what causes earthquakes, check out How Earthquakes Work
Fast Facts
(Source for all fast facts is USGS)
WebQuest Online
Exercise
In this journey around the Web, we'll discover what causes earthquakes, how
scientists can figure out their exact location, where they occurred last week
and much, much more! Click on the Web site(s) after each question to find your
answer.
1. Around 1912, German meteorologist Alfred Wegener developed a theory called continental drift. He believed that about 225 million years ago, giant landmasses gradually shifted and broke apart to form the continents as we know them today. How many original "supercontinents" did Wegener's theory of continental drift assume?
http://www.exploratorium.edu/faultline/index.html
http://www.thetech.org/exhibits/online/quakes/waves/p&s_waves.html
http://www.thetech.org/exhibits/online/quakes/grams/
http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/tectonics_landforms/faulting_p2.html
http://pubs.usgs.gov/gip/dynamic/fire.html
http://www.see.leeds.ac.uk/structure/dynamicearth/subduction/ringofire/index.htm
http://www.pbs.org/wnet/savageearth/hellscrust/html/sidebar3.html