Abstract
In this lesson students will analyze the
structure of the Earth’s interior using the findings
of two geologists and information from the past week’s
lesson.
Purpose –Apply knowledge to determine the physical
structure of the Earth.
Objectives
Students
will be able to:
1. Create a model of the Earth that is consistent with scientific understanding
of earthquake waves.
National Science
Education Standard:
CONTENT STANDARD
D – Earth and Space Science
THE ORIGIN AND EVOLUTION OF THE EARTH SYSTEM
•
Interactions among the solid earth, the oceans, the atmosphere, and organisms
have resulted in the ongoing evolution of the earth system. We can observe
some changes such as earthquakes and volcanic eruptions on a human time
scale, but many processes such as mountain building and plate movements
take place over hundreds of millions of years.
Teacher
Background
For
the past century geologists have described the earth
as having
4 layers, the crust, mantle, outer and inner
cores. The nature, composition and interaction among these
layers is more debatable. Andrija Mohorovicic, a Croatian
scientist, established that there was a difference in the
velocity that earthquake waves traveled in the mantle as
compared to the crust. This difference marked a ‘discontinuity’ that
informs us where the mantle and the crust meet. Measuring
P and S waves, Mohorovicic also noted that they do not
pass through the earth in a straight line. He established
that the mantle is denser that the crust.
The
German geologist, Beno Gutenberg, also used information
about how waves
traveled to establish the nature of the
earth’s structure.
http://volcano.und.nodak.edu/vwdocs/vwlessons/lessons/Ch1CMB/Content1.html
Earth’s
Structure
http://www.zephryus.demon.co.uk/geography/resources/earth/struc.html
Seismic
Waves and the Earth’s Interior
http://eqseis.geosc.psu.edu/~cammon/HTML/Classes/IntroQuakes/Notes/waves_and_interior.html
Related
and Resource Websites
Earth Science Archives
http://www.madsci.org/posts/archives/mar2001/985815079.Es.r.html
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