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Texas A&M University *
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Subject
Geology
Date
Dec 6, 2023
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ISOSTASY FORM
Name:
Section:
Hannah Smith
OCNG-252-598
Lab 1: Isostasy
EXERCISE 1:
Archimedes’ Principle
Table 1
Part 1: Floating Washers
(1)
Measured weight of washers (g)
41 g
(2)
Initial volume of beaker (ml)
500 ml
(3)
New volume of beaker (ml)
541 g
(4)
Volume displaced (ml)
(3) – (2)
41 ml
(5)
Weight of washers from volume
(4) ml x 1 g/cm
3
x 1 cm
3
/ml
164 g
(6)
Measured versus displaced difference.
(5) – (1)
123 g
How well does your measured (1) versus displaced mass (5) compare for the floating scenario? Are
these the results what you expected?
If your numbers are different, what could explain these
differences?
Based on Archimedes Principle, the volume of displaced water equals the mass of the floating object,
which in this case, is the washers. Here, the volume of displaced water is 41 ml, which is equal to the
measured (1) mass of the washers, which is 41 g. However, there is a difference than in the floating
scenario because the displaced mass of the washers is 164g, which does not equal the volume of
displaced water as it is greater.
Table 2
Part 2: Submerged Washers
(7)
Calculated volume of washers (cm
3
)
0.92 cm
3
x number of washers
11.04 cm3
(8)
Initial volume of graduated cylinder (ml)
90 ml
(9)
New volume of graduated cylinder (ml)
101 ml
(10)
Volume displaced (ml)
(9) – (8)
11 ml
(11)
Volume of washers in cm
3
(10) x 1 cm
3
/ml
11 cm3
(12)
Measured versus displaced difference.
0.04 cm3
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ISOSTASY FORM
Name:
Section:
(11) – (7)
How well does your measured (7) versus displaced volume (11) compare for the submerged
scenario? Are these the results that you expected?
If your numbers are different, what could
explain these differences?
My results aligned with what I expected to happen based on the information I learned before, especially
regarding Archimedes Principle and the submerged scenario. In the submerged scenario, this principle
states that the volume of displaced water is equal to the volume of the submerged object. Here, my
measured volume of the washers was 11.04 cm3 and my displaced volume was 11 cm3. Additionally, I
found the volume of displaced water to be 11 ml, which is the same value that I found for the displaced
volume of the washers. Therefore, my results compare well to the submerged scenario as the volume of
displaced water that I found was equal to the volume of the submerged object.
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2
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ISOSTASY FORM
Name:
Section:
EXERCISE 2:
Density of Rocks
Table 3
Granite
Basalt
Peridotite
(1)
Mass (g)
24.12 g
26.19 g
38.52 g
(2)
Initial Volume in
Graduated Cylinder
(ml)
90 ml
90 ml
90 ml
(3)
Final Volume in
Graduated Cylinder
(ml)
99 ml
99 ml
102 ml
(4)
Volume Difference =
Volume of Rock
sample
(3) – (2)
9 ml
9 ml
12 ml
(5)
Density (g/cm
3
)
Mass/Volume of rock
sample
(1) / (4)
2.68 g/cm3
2.91 g/cm3
3.21 g/cm3
Which rock sample is the densest?
Peridotite
Which rock sample is the least dense?
Granite and Basalt are equally the least dense.
Is this what you expected?
Explain
No, it is not. I expected Peridotite to be the densest as it had the greatest mass, but I did not expect
Basalt and Granite to have the same density. Because the mass of Basalt is greater than that of Granite
by 2.07 grams, I expected there to be a difference in the density between the two.
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ISOSTASY FORM
Name:
Section:
The average density of the earth is about 5.5 g/cm
3
. How does this number compare to the density
of your three rock samples? Why are they different?
It makes sense that the density of the three rocks would be lower than that of the earth, with Peridotite
and earth having a difference in density of 2.29 g/cm3 and Basalt and Granite having a 2.82 g/cm3
difference in density. It makes sense that peridotite is the closest in density to the earth, because in this
lab it is meant to simulate the earth's mantle. The reasoning for the difference in density is that the earth
is made up of several different layers, including the mantle, oceanic crust, and continental crust, so it is
clearly going to have a greater density. These three rocks are meant to measure the density of each
individual layer.
With your understanding of the principle of isostasy, if your granite and basalt rock samples were
of equal volume, which of these samples would float highest when resting on the mantle?
Why?
Not only did Granite and Basalt have equal volumes, but they also had equal densities. Based on the
principle of Isostasy, these two rock samples would each float at the same level because how "high" or
"low" they float is based on density.
Which rock sample, granite, or basalt, would float lowest on the mantle? Why?
The Peridotite rock sample would float the "lowest" on the mantle as it has the greatest density of the
three samples.
EXERCISE 3:
Isostatic Adjustment
Table 4
Pine
Oak
Weight (g)
33.52 g
47.96 g
Density (g/cm
3
)
0.486 g/cm3
0.695 g/cm3
Compare the density of the pine and oak wood blocks with the density of water (1 g/cm
3
).
Which
is greater?
Water has a greater density than both the pine and oak wood blocks in this scenario. The Oak wood
block is closer to water as its density is 0.695 g/cm3 whereas the density of pine wood blocks is only
0.486 g/cm3.
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ISOSTASY FORM
Name:
Section:
Would you expect the wood blocks to float in water?
Why?
Yes, I would expect the wood blocks to float in water because they both have a lower density than that
of the liquid that they are in.
Now compare the density of water to the densities of the rock samples you determined in Exercise
2.
Would you expect any of these rocks to float in water?
Why or why not?
I would not expect any of these rock samples to float in water because all three have a greater density
than that of water. The density of Granite is greater than that of water by 1.69 g/cm3, Basalt is greater by
1.91 g/cm3, and Peridotite is greater by 3.21 g/cm3. But, if they were to float, Granite would float the
"highest" because it has the lowest density and Peridotite would float the "lowest" because it has the
greatest density.
Table 5
1 Pine Block
2 Pine Blocks
1 Oak Block
(1)
Thickness of block above
water (cm)
1.1 cm
2.1 cm
0.07 cm
(2)
Thickness of block below
water (cm)
0.08 cm
1.7 cm
1.2 cm
(3)
Total thickness of block
(cm)
1.9 cm
3.8 cm
1.9 cm
(4)
% of block above water
=
(1) / (3) x 100
57.89%
55.26%
3.68%
(5)
Thickness of water
beneath block (cm)
= 10 cm – (2)
9.92 cm
8.3 cm
8.8 cm
(6)
Mass of water under
block (g)
=
(5) x 1 cm x 1cm x 1 g/cm
3
9.92 g
8.3 g
8.8 g
(7)
Mass of wooden block (g)
density x 1 cm x 1 cm x (3)
0.9234 g
1.8468 g
1.3205 g
(8)
Mass of Water + wooden
block (g)
(6) + (7)
10.8434 g
10.1468 g
10.1205 g
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ISOSTASY FORM
Name:
Section:
How do the blocks represent oceanic and continental crust? Why? Give two examples.
By calculating the density of the blocks, and the percentage of the block above and below the water, we
can determine which represents the continental crust and which represents the oceanic crust. Continental
crust is thicker than oceanic but has a lower density, so it will float "higher," whereas oceanic crust is
less thick but has a greater density. We can’t determine which block represents continental crust and
which represents oceanic crust just by looking at the determine total thickness because they are both 1.9
cm, but we can by looking at the percent of the block that is above the water. The pine block was
57.89% above the water and the oak block was 3.68% above, showing that the pine block was floating
"higher". This means that the Pine Block represents the continental crust, and the Oak Block represents
the oceanic crust.
Based on your understanding of isostasy, what layer of the earth does the water represent in this
experiment? Why?
The water in this experiment represents the mantle because the two blocks represent the continental
crust and oceanic crust which both float above the mantle as represented with the blocks and water in
this experiment.
How can isostasy be used to explain the uneven surface of Earth’s crust? How is the Earth’s crust
able to stay balanced on the mantle?
The earth’s mantle is denser than both the continental and oceanic crust. The earth’s crust is not
necessarily balanced on the mantle, but instead, due to isostasy, it is actually floating on top of the
mantle, because the crust is light, and the mantle is dense.
How does the fraction of exposed pine compare for the one pine block case versus the stacked two
pine block case? Is this what you expect? Explain your answer. (Hint: Use Table 5, Row 4)
For the one pine block, the total thickness of the block was 1.9 cm, with 1.1 cm being above the water,
or, 57.89%. For the stacked two pine blocks, the total thickness was 3.8 cm, with 2.1 cm being above the
water, or, 55.26% of it. This is very close to what I expected to happen. Because both cases involve the
same type of wood blocks, I expected them to float in a similar manner due to their density. In both
cases, there was a very similar percentage in the thickness of the block above the water, with the one
pine block case only having a greater percentage out of the water than the other case by 2.63%. It can be
expected that the one block case would have a greater amount above the water, as the mass of one block
is clearly lower than that of two blocks, therefore allowing it to float “higher”. Overall, these two cases
acted very similarly with the only difference being the added block in the two-block case.
Page
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ISOSTASY FORM
Name:
Section:
Compare the 1 pine, 2 pine and 1 oak scenarios.
Are the combined masses of wood and water
similar? Is this what you expected?
Explain your answer. (Hint: Use Table 5, Row 8)
In this scenario, all the combined masses of wood and water are very similar. My recorded combined
mass of wood and water for 1 pine block was 10.8434 g, the combined mass for 2 pine blocks was
10.1468 g, and the combined mass for 1 oak block was 10.1205 g. This is not what I had expected, aa I
thought that the 2 pine blocks would have the greatest combined mass, but they had the second largest
combined mass with the 1 pine block mass being 0.6966 g heavier. However, based on the previous
calculations in table 5, I did expect that the 1 pine block and 2 pine blocks would each individually have
a greater combined mass than the 1 oak block scenario, which was proved true as it had the lowest
combined mass of all 3 scenarios.
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ISOSTASY FORM
Name:
Section:
SUMMARY QUESTION:
What would happen to the continent of Antarctica if all the ice were removed?
To answer this,
assume that the ice did not melt into the ocean, e.g., no large volume of water was added to the
surrounding ocean. Using what you learned in this lab, what happens to the continent?
Where is
sea level on the continent now without the ice compared to with the ice? What is this process
called? (Hint: This is similar to removing the 2
nd
pine block “mountain” used in Exercise 3.)
This process would be called glacial isostatic adjustment. This is when continental crust sinks due to its
weight increasing because of ice growth, sediment deposit, or lava. The weight of the mass on a
continent causes the crust to subside, but when this weight from the ice is removed, the isostatic rebound
takes place and the land would be uplifted, creating a valley that would be relatively flat. This is also
because the sea level will lower due to the “rebound” and the area of land will increase.
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