GEOSCI 106 Lab 5_ Volcanoes-March
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University of Wisconsin, Madison *
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106
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Date
Dec 6, 2023
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GEOSCI/ENVIR ST 106: Environmental Geology
Lab 5: Volcanoes
Assignment overview:
One of the major
impacts of plate tectonics on human life is in
the form of volcanic activity. Geologists
collect a variety of data about volcanoes to
understand future risks. In this lab, you will
use data from maps and conduct some simple
computations to explore volcanic hazards.
Instructions:
1.
Download the “Pacific NW volcanism.kmz” dataset associated with this lab in Canvas.
2.
If you do not have Google Earth Pro, download and install it. It is freely available here:
https://www.google.com/earth/versions/
. Note that the version of Google Earth in a browser will
not suffice; you will need to use some functions that are only available in Google Earth Pro.
3.
Fill out each red highlighted field (_________) according to each question’s instructions.
Submission:
To submit the assignment on Canvas, use the following steps:
1.
In Google Docs, generate a PDF: File → Download as → PDF Document
2.
In Google Docs, use Share → Get Shareable Link, and copy the link address
3.
In Canvas, upload your PDF to the assignment.
4.
In Canvas, paste the link address to your Google Doc in the assignment comments.
Unit conversions:
In this lab, you will need to convert imperial units to metric on a few occasions. Here
are some unit conversions that you may find helpful.
1 foot = 0.3048 m
1 mile = 5280 feet = 1.609 km
1 km = 1000 m
1 km
3
= 10
9
m
3
1
Volcanic eruptions: Mt. St. Helens (1980)
In Canvas, open the Google Earth file “Pacific NW volcanism.kmz”, and zoom in to Mt. St. Helens. You
should see an image of a rectangular topographic map overlain on the satellite imagery. (If you do not see
this, go to the Places window in Google Earth, click on the “Pacific NW volcanism.kmz” file, and make
sure that the “Mt St. Helens, WA, 1:62,500 quad, 1958” is checked.) This is a topographic map from
1958, which shows the topography of Mt. St. Helens a couple decades before the 1980 eruption. Because
this map is rather old, the elevation data it reports are in units of feet.
By exploring the terrain in Google Earth, you should see that Mt. St. Helens juts up sharply against the
surrounding topography. Here you will use this data to explore the topography of the volcano before it
erupted.
The first step is to orient yourself on the topographic map. If you have not looked at a topo map before,
the following tips may help you interpret what you see:
●
The thin reddish brown lines circling the volcano are contour lines. Each contour line connects
locations with the same elevation.
●
Some of the contour lines are a little thicker than the others. These are labeled with numbers that
indicate the elevation of the contour line in units of feet.
●
The rest of the contour lines are a little thinner and are not labeled. These indicate equally spaced
elevation intervals between the thicker contour lines.
1. Topographic contour lines.
What is the elevation difference between neighboring thin contour lines?
This is known as the map’s contour interval. (Tip: Count the number of lines between two thick contour
lines.) Report this in both feet (as the map shows it) and in meters. (1 point)
40_________ feet
12.192_________ meters
2. Estimating volcano slope.
Using the line tool in Google Earth, draw a line from the
pre-eruption
peak of Mt. St. Helens (i.e., as indicated in the 1958 contour map) to the north, until you reach the
4,400-foot contour line on the map. What is the average slope of the volcano along this line? (Hint:
Slope = elevation change in meters / lateral distance in meters.) (1 point)
_0.356________
3. Estimating pre-eruption volcano volume.
By examining the topographic map, you may notice that
the volcano before the eruption was roughly shaped like a cone. Here you will estimate the volume of the
2
volcano. Using the polygon tool in Google Earth, trace a rough outline of the 4,400-foot elevation
contour on the contour map, which represents the approximate “background” elevation for the region.
This represents the area of the base of the volcano. Then, calculate the total above-ground volume of the
volcano (in cubic km) using the following formula, in which
A
base
has units of km
2
and
h
has units of km.
The area of the polygon will be automatically calculated by Google Earth under the polygon’s
Measurements tab. (3 points)
)/3
V
cone
= (
A
base
×
h
A
base
(km
2
) (area of the volcano’s base) = _38.4________
h
(km) (peak elevation above the background elevation) = _2270________
V
cone
(km
3
) (volume of the volcano) = _29056________
Paste a picture of your polygon representing the area of the base here. (You may want to use “Absolute
elevations” and transparency to help with visualization of this polygon.) (1 point)
_____
____
4. Estimating erupted volcano volume.
(a) If you turn off the 1958 topo map in Google Earth, you will
see how drastically the shape of Mt. St. Helens changed during the eruption. Fill in the following values
to estimate the volume of the “cone” of material that erupted. (3 points)
A
crater
(km
2
) (area of the crater) = _3.79________
h
peak
(km) (elevation of the original peak above the crater rim) = _280________
(Note: for this value, you should choose a rough average of the crater rim elevation, ignoring the
complication the “blow out” made to the topography to the north.
V
erupted
(km
3
) (volume of the volcano that was blown away during the eruption) = _353.73________
(b) What fraction of the pre-eruption volcano volume was blown away during the eruption? (1 point)
3
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_1/100________
(c) Use a density of 2700 kg/m
3
(typical of andesite) to calculate the mass of rock (in kg) that was blown
off the volcano during the eruption. (1 point)
9.55x10^11kg_________
5. Impact of the eruption.
The Seattle metropolitan area is roughly 220 km
2
. If all of the rock erupted
from Mt. St. Helens (as calculated in the previous question) had landed on Seattle, how thick would that
layer be, in meters? (Hint: Dividing the volume of rock by the area over which it fell will give you a
depth. Remember to convert this to meters!) (1 point)
_1607m________
Highway 504, North of Mt. St. Helens, post-eruption. (USGS)
4
6. Shield volcano vs. stratovolcano topography.
Hawaii’s Big Island has the largest volcanoes in the
United States. Unlike Mt. St. Helens and the other stratovolcanoes in the Cascades, these are shield
volcanoes. Shield volcanoes are built from lavas that flow more easily (i.e., they are less viscous) than
the lavas that build stratovolcanoes, and as a result shield volcanoes tend to have gentler, broader slopes
than stratovolcanoes.
The largest volcano on the Big Island is Mauna Loa. In the Google Earth file, click on “Mauna Loa
transect” to navigate to the Big Island. Here, the red line indicates a transect from one side of Mauna Loa
to the other. This is composed of two straight lines, one from Point A to the summit (Point B), and one
from the summit down the other side to Point C, each roughly aligned with the path of steepest descent.
There are twenty placemarks along the transect, indicating the points at which you will need to measure
distances and elevations, which you will need to report in Table 1. The first row represents Point A, and
has already been filled out as an example.
With the Ruler tool, measure the horizontal distance along the transect from Point A to each point on the
transect. Because these must be distances
along
the transect, points on the opposite side of the summit
from Point A (points 12-20) should be measured as the distance from Point A to Point B plus the distance
from Point B to the point in question. Report these distances in the Distance column in Table 1. In the
Elevation column of Table 1, record the elevation of each point. In Google Earth, you can find the
elevation of the terrain under your cursor near the bottom right corner of the Google Earth window, where
the cursor’s latitude, longitude, and elevation are shown. (3 points)
5
Table 1. Mauna Loa transect
Site
Distance along transect (km)
Elevation (m)
1 (Point A)
0
51
2
3718
741
3
7725
1172
4
11258
1487
5
14385
1796
6
17577
2046
7
20740
2411
8
23314
2837
9
26853
3353
10
30066
3861
11 (Point B)
32941
4003
12
35462
3900
13
37365
3445
14
39387
2968
15
41692
2478
16
43517
2028
17
46301
1446
18
48630
1124
19
51524
746
20 (Point C)
54443
498
6
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7. Mt. St. Helens transect.
In the Google Earth file, go to the “Mt. St. Helens transect”. Like the Mauna
Loa transect, this consists of a transect line and 20 placemarks. Fill out Table 2 with the distance of each
point along the transect and its elevation, the same way you filled out Table 1. (3 points)
Table 2. Mt. St. Helens transect
Site
Distance along transect (km)
Elevation (m)
1 (Point A)
0
1067
2
618
1080
3
1393
1110
4
2129
1135
5
2952
1177
6
3880
1341
7
4483
1552
8
5122
1622
9
5885
1762
10
6504
1900
11
7276
2103
12
8031
2407
13
8521
2249
14
9167
1978
15
9815
1762
16
10544
1409
17
11275
1253
18
12117
1158
19
12893
1145
20 (Point B)
13809
1037
7
8. Plot elevation profiles.
(a) Create an x-y plot with the elevation profiles for both the Mauna Loa and
the Mt. St. Helens transects on the same plot, and paste the plot in the designated space below. Make sure
both transects are on the same plot and that the plot has the following elements:
X-axis showing distance from Point A, with an extent of 0 to 65 km
Y-axis showing elevation, with an extent of 0 to 5000 m
Labels on x-axis “Distance (km)” and y-axis “Elevation (m)”
Labels for each profile with the volcano names
You are welcome to use whatever software you like to generate this plot. If you choose to do this in
Google Sheets (which you may find convenient because it is easy to copy a plot from Google Sheets into
this Google Doc), you may find it easiest to follow these steps.
1.
Open a Google Sheet from this Google Doc by going to File > New > Spreadsheet.
2.
Copy the Distance and Elevation data from the Mauna Loa table (Table 1) and paste them into the
first two columns of your Google Sheet. This data should be in rows 1-20 of columns A-B.
3.
Copy the Distance and Elevation data from the Mt. St. Helens table (Table 2), and, starting at the
row below your Mauna Loa data, paste them into columns A and B. This data should be in rows
21-40 of columns A-B.
4.
Move the Mt. St. Helens elevation data one column to the right (i.e., from column B to C). The
spreadsheet should now consist of 40 values in column A, 20 values in rows 1-20 of column B
(and nothing below that in column B), and 20 values in rows 21-40 of column C.
5.
Highlight columns A, B, and C and go to Insert > Chart. At the right side of the Google Sheets,
under Setup, change Chart Type to Line Chart. This will generate an x-y plot with both elevation
profiles.
Paste your completed graph here. (3 points)
8
_
________
(b) Compute the volume of Mauna Loa above sea level using the same equation you used to compute the
volume of Mt. St. Helens above. Although this approach implicitly approximates Mauna Loa as a
geometrically perfect cone -- which it’s not -- it nonetheless provides a rough estimate of its volume,
which will suffice for this exercise. (Side note: a more important influence on this estimate of the volume
of Mauna Loa is that it grew from the seafloor, not sea level, so its total volume is substantially larger
than its volume above sea level.) (2 points)
_75,000km^3________
(c) How many times bigger is Mauna Loa’s above-sea-level volume than Mt. St. Helens’ volume? (1
points)
_2.58________
Bonus question.
A few kilometers north of Mt. St. Helens is Spirit Lake, which was a popular tourist
destination before the eruption. In Google Earth, zoom in (WAY in) on Spirit Lake. What unusual
feature do you see in the lake towards its northern end? Search for information online about this feature,
and, in 2-3 sentences, summarize how this feature was formed, and what its existence today implies about
how long these features can impact lakes. (1 point)
9
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_The eruptions fully impacted the lake. This caused toxic gases to seep up and into the water.
This led to the water being devoid of oxygen.________
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