Geology module 1
.docx
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School
Utah Valley University *
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Course
1010
Subject
Geography
Date
Jan 9, 2024
Type
docx
Pages
3
Uploaded by DukeWildcatMaster999
Background Information:
After you read the book chapters, reviewed the slides, and watched the videos, I hope you are able to explain
why earth has layers: earth is made of different elements that have different densities. During the early
formation of the earth, less dense elements rose toward the surface and denser elements sank toward the
center of the earth which led to the formation of layers. In this activity, it provides you further evidence why the
core has a small volume percentage relative to the whole earth volume, but it accounts for a much bigger
weight percentage of the earth. Ultimately, I am hoping you reach the conclusion that the earth core is made of
denser elements (such as iron and nickel) compared to the mantle and crust. Complete the questions below
and see it yourself.
Earth’s Layering
1.
Calculate the % of the whole volume of the Earth that is occupied by the core and mantle, respectively.
The formula of the volume of a sphere is
4
3
πr
3
where r is the radius of the sphere and π=3.14. The
radius of the Earth is 6371 km, the radius of the core is 3471 km. The crust is so thin relative to the
mantle and the core that you can ignore it in your calculations. PLEASE SHOW EACH STEP THAT
LEADS TO YOUR FINAL ANSWER.
Tips for this question: 1) don’t be scared of numbers, you’ll have fun with them once you like them; 2)
calculate the volume of the whole earth first using the given equation
4
3
πr
3
; 3) then calculate the
volume of the core using the given equation
4
3
πr
3
; 3) now you can use the volume of the core
divided by the volume of the whole earth to get the percentage of the core; 4) use 100% minus the
percentage of the core you get in the previous step to get the percentage of the mantle since we are
ignoring the volume of the crust.
Here is my example on how to calculate the earth’s volume using the given equation:
V=
4
3
πr
3
=
4
3
*3.14 * (6371 km)
3
= 1.08 x 10
12
km
3
4
3
πr
3 =
V
πr= 3.14
4
3
*3.14 * (3471 km)
3
/ =
4
3
*3.14 * (6371 km)
3
=
25.82%
r=3471 km
2.
Now you have calculated the % of the mantle and core
relative to earth
by volume
, respectively.
Scientists have also calculated the % of the mantle and core relative to the earth
by weight
, which are
68% and 31%, respectively. Explain why the percentages are very different in terms of volume vs.
weight. (Hint: think about which layer is composed of the densest elements…)
I think it is because of the materials that make up the certain parts of the earth. The core is really dense and
made up of heavy metals. Whereas the mantle is made up of other materials that don’t weigh as much. Even
though they make up more of the earth, they are going to weigh less pound for pound than the core.
3.
Review these properties of Earth’s interior compositional and physical layers. While you do not need to
memorize thicknesses or densities, you should memorize composition and state, and be able to draw a
picture, to scale, of all of Earth’s layers. In your drawing, you can ignore the thickness of the crust and
use a line to represent the thickness of the crust, and then draw the mantle, inner core, and outer core,
to scale.
(Tips for drawing: click the “Insert” tab in Google Doc, then select “Drawing” in the dropdown
menu, click “New”, select the third to last icon to draw circles. Note: if you press “Control” while you are
drawing the circles, you will get a perfect shaped circle. Also when you are in “Drawing” window, you
should be able to insert text boxes to layer the layers. Alternatively you can do the drawing using other
tools (e.g. Microsoft Paint) and paste the drawing back to your google doc)
Layers
Thickness
Composition
State/Density
Oceanic crust
3-10 km
Si, O, Fe, Mg, Al = Basalt
2.9 g/cc SOLID
Continental crust
30-50 km
Si, O Al = Granite
2.7g/cc SOLID
Mantle
2900 km
Mg, Fe, Si, O
4.5 g/cc SOLID
Outer core
2200 km
Fe, Ni (S, Si)
11 g/cc LIQUID
Inner core
1300 km
Fe, Ni (S, Si)
16 g/cc SOLID
Crust
Inner core
Outer Core
Mantle
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