EQ_Tect_Activity
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Subject
Geology
Date
Dec 6, 2023
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Lab Activity: Earthquakes, Volcanoes and Plate Tectonics
In this exercise we will be investigating websites where you can explore recent earthquakes and
volcanoes, and we will be evaluating these events in their plate tectonic setting.
I encourage you to
explore these websites more in depth where you will find a wealth of information. We will also be
exploring more around the Hawaiian Islands, and how the ages of these islands provided a key piece of
evidence for Plate Tectonics.
For this exercise you will need 4 KMZ files: EQ_Tect_Activity.kmz,, plate_boundaries.kmz, Alaska
Volcanoes.kmz, and USGS_Earthquakes_6mo_20231012.kml.
I recommend the following settings for
Google Earth to make this assignment easier to complete.
Web Version (
https://earth.google.com
).
Google Earth Pro
•
Clear out all previous KMZ layers EXCEPT plate_boundaries.kmz
Set
View to “Clean”
•
click on “Layers”, select “Clean”
.
This
will make it easier to view the various
layers in this file
Turn off Borders and labels.
•
In the “Layers” panel on the sidebar
unclick
“Borders and Labels”
Part 1.
USGS Earthquake Information
Go to the USGS Earthquake Hazards Website (
https://www.usgs.gov/programs/earthquake-hazards
).
To
get information on recent earthquakes, click on “Latest Earthquakes” (see
Figure 1).
Figure 1.
USGS Latest Earthquakes Mapping Tool
Questions:
1A.
In the selection panel (at right
–
figure 1), select
“1 Day, All Magnitudes U.S.” option.
Make
sure the “Only list Eq…shown on map” option is TURNED OFF.
What was the most recent
earthquake and what was its magnitude?
1B.
In the selection panel, select “30 Days, Significant Worldwide”. S
ort the data by magnitude
–
largest first.
Where was the largest magnitude earthquake in the past 30 days in the world and
what was its magnitude?
Click on the largest magnitude earthquake on the left panel and select the link to the Earthquake
Overview page (See figure 2).
Questions:
1C.
(no question here…)
On the Overview Page (figure 2)
–
scroll down and click on “Download
Event KML” (save this to your computer and remember where!).
The “Nearby Seismicity” link brings up a map with all the earthquakes
in the past month within ~250 km.
1D.
How many earthquakes have there been in the vicinity of this earthquake, and what is the range of
magnitudes?
Go to Google Earth (Google Earth Pro, or Web Version).
Open the “plate
-
boundaries.kmz” and the KML
file that you downloaded in step 3 above into Google Earth.
1E.
Is this earthquake near (~within 250 km) of a plate boundary?__________.
If so, what type of
plate boundary is it?__________________.
What plates are coming together at this boundary?
(see figure 3 for plate boundary legend and Table 1 for list of plate boundaries).
Figure 2.
Navigating Earthquake
Overview Page
Nevada/0.8
46km SE of Madang, Papua New Guinea/ 6.9
35 earthquakes/ 4.0-6.9
yes
Convergent plate boundary
Pacific Plate/ Australian-Indian Plate
Table 1: Plate Abbreviations used on the USGS Plate Boundary KMZ:
Plate
Abbreviation
Pacific
PA
North American
NA
Eurasian
EU
African
NU
Antarctic
AN
Australian-Indian
AU
South American
SA
Nazca
NZ
Indian
IN
Philippine
PH
Sunda
SU
Arabian
AR
Caribbean
CA
Cocos
CO
Scotia
ST
Juan de Fuca
JF
Go back to the original earthquake map page (figure 1).
Select “7 Days All Magnitudes US”, “7 Days
Magnitude 2.5+”, and “7 Days Magnitude 4.5+” and
answer the following questions:
1F.
How many total (detectable) earthquakes have occurred worldwide in the past 7 days?
1G.
How many earthquakes of magnitude 2.5 or higher have occurred worldwide in the past 7 days?
1H.
How many earthquakes of magnitude 4.5 or higher have occurred worldwide in the past 7 days?
1I.
What percentage of total earthquakes have had a magnitude of 2.5 or higher? (2 significant digits)
100 ∗
(𝑇𝑜??? ????ℎ????𝑒? > 2.5)
(𝑇𝑜??? ?𝑒?𝑒?????𝑒 ????ℎ????𝑒?)
=
1J.
What percentage of total earthquakes have had a magnitude of 4.5 or higher? (use equation
above but substitute earthquakes > 4.5 in numerator.
2 significant digits).
1K.
What conclusion can you draw about the relationship between the frequency and strength of
earthquakes?
1L.
Bring up your original query (with the “1 Day, All Magnitudes U.S.” option).
How many
earthquakes have occurred since you answered question 1A?_______.
From this information,
what general statement can you make about the occurrence of earthquakes worldwide?
Figure 3.
Legend for Plate
Boundaries on KMZ file
1898 earthquakes have occured
259 earthquakes
91 earthquakes
4.79%
13.65%
The Gutenberg-Richter rule, which states that an earthquake's frequency falls as its magnitude increases, is commonly used to describe
the link between an earthquake's intensity and frequency. Smaller earthquakes happen more often, while larger, more powerful ones
happen far less frequently.
1
Earthquakes happen all across the world on a constant basis. Earthquakes are common occurrences,
with several small to moderate earthquakes taking place every day all around the world. Even though
they are less frequent, larger, more severe earthquakes still occasionally occur.
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Part 2:
Earthquakes and Plate Tectonics
For this exercise you will need to open the EQ_Tect.kmz, plate-boundaries.kmz,
and USGS_Earthquakes_6mo_20231012.kml files.
The earthquake file includes
all earthquakes > 4.5 worldwide for a 6 month period (from 4/12
–
10/12/2023)
downloaded from the USGS Earthquake site explored in Part 1 of this exercise.
Open the folder “Part
2 Poin
ts” in the “
EQ_Tect.kmz
”.
For each of the locations
in this folder, answer the questions below.
Peru
2A.
What type of convergent plate boundary is this (Continent/Continent,
Ocean/Continent,)?
2B.
What is the range of depths of earthquakes (see figure 4)?
Is there a
pattern to the depth of earthquakes relative to the plate boundary?
Explain
Iceland
–
and surrounding Ocean.
2C.
What type of plate boundary is this (convergent/divergent/transform)?
2D.
What is the range of depths of earthquakes?
Is there a pattern to the
depth of earthquakes relative to the plate boundary?
Explain.
Tonga Trench
2E.
What type of convergent plate boundary is this (Continent/Continent, Ocean/Continent,)?
(ignore
the
divergent
plate boundary here. Sometimes there is a small amount of sea floor spreading
behind an island arc structure).
2F.
What is the range of depths of earthquakes?
Is there a pattern to the depth of earthquakes relative
to the plate boundary?
Turkey
2G.
What type of plate boundary is this (convergent/divergent/transform)?
2H.
What is the range of depths of earthquakes?
Is there a pattern to the depth of earthquakes relative
to the plate boundary?
Part 3.
Volcanoes and Plate Tectonics
Go to the Smithsonian Global Volcanism Program website (
https://volcano.si.edu/
).
On the “New
Activity/Highlights” panel on the right side of the page, select “Current Eruptions”.
3A.
What is the “Review Date” for this list of eruptions?
3B.
How many “Current Eruptions were bei
ng tracked as of this review date?
3C.
What is the largest “Volcanic Explosivity Index” (VEI) for the volcanic activity on this list?
3D.
How would a volcano with the maximum VEI on this list
compare to other “Large” volcanoes
in
history?(see figure 4 below)
Figure 4.
Depth and
Magnitude of
earthquakes in USGS
Earthquake KMZ
Nazca Plate/South American Plate - Ocean/Continent
Earthquake depths vary from shallow to intermediate, mainly between 70 and 300 kilometers,
which reflects the behavior of subduction zones. Overriding continental plates have deeper
earthquakes, whereas subducting oceanic plates experience intermediate-depth earthquakes.
Divergent
0-33 km / Because of diverging plate boundaries, shallow earthquakes mostly occur in the top
crust of Iceland, with shallow to mid-crustal areas seeing the greatest amount of seismic activity.
Ocean/Continent convergent plate boundary
0-33 km to 500-800 km
This region's earthquake depth pattern is indicative of subduction zones, with complicated stress
and deformation inside the subduction zone influencing shallow, intermediate, and deep earthquakes.
Transform plate boundary
0-33 km / Because of complex plate interactions and regional geology, earthquake depths
in strike-slip fault zones can vary, usually including shallow and moderate-depth quakes.
46 volcanoes were in continuing eruption
4
11 October 2023
A VEI 4 volcano is considered a "moderate" eruption, with significant local and regional impacts but not as
powerful as larger events.
Go
back to the list of “Current Eruptions” and click on the
“Volcano” link for one of the highest “VEI” volcanoes (the
volcano link is the
Orange
name on the left side of the table
that will take you to the website for this volcano).
Click on the “General Information” tab on this page.
3E.
What is the name, volcanic type(s), rock types, and
tectonic setting for this volcano?
Download the “Google Earth Placemark with Features” for
this Volcano (the link for this is just below the picture at the
top of the Volcano page).
Open this in Google Earth, along
with the “plate boundaries.kmz” file.
3F.
Is this volcano associated with a tectonic plate
boundary (within 250 km)?
If so, what type?
3G.
Do there appear to be nearby earthquakes that
might be associated with this volcano?
Select Volcanoes
The following questions use the
“Select Volcanoes.kmz”
as well as the
“plate boundaries.kmz”
and
USGS_Earthquakes_6mo_20231012.kml files used in Part 2 of this assignment.
“Select Volcanoes” is a selection of Holocene volcanoes from Smithsonian site (Holocene:
<3 Ma to
present).
In the “Select Volcanoes” file there are
6 folders with different regions volcanoes.
Double
Click on these folders to view these sets of volcanoes.
Answer the following questions for each of the
sets of volcanoes (figure 6.37 in your textbook and the video:
https://goo.gl/PSN9hc
may help answer
some of these questions.)
•
type of tectonic boundary (convergent, divergent, transform)
•
the names of the plates colliding (see table 1 and figure 3 above)
•
the types of crust (oceanic-continental) that are involved (may be more than 1).
•
Bonus: indicate
what “type” of volcano (shield, composite, lava dome) is most common in these
sets (see figure 6.13 in your textbook.
https://goo.gl/awPZir
).
3H.
South America:
3I.
Iceland
3J.
Africa Rift Valley (central)
3K.
Africa Rift Valley (eastern) - No Answers need here.
This was a divergent plate boundary in the
recent past, but it has stopped.
However, you can still see some tectonic activity in this region.
3L.
Alaska
3M.
Azores
Figure 3.
Volcanic Explosivity Index (VEI)
Compare.
Note that VEI 0 -1 events occur
daily where VEI 7 events occur every 100
years or more (source: USGS).
A VEI 8
event may occur every ~50,000 years.
Semeru/ Stratovolcano, Pyroclastic cone, Fissure vent/ Andesite, Basaltic Andesite,
Basalt, Picro-Basalt/ Subduction zone, continental crust
yes/ convergent plate boundary
no
convergent/ Nazca-South American/Oceanic, Continental/ Composite, Shield
Divergent, Transform/ Eurasian-North American/ Oceanic, Continental/ Shield
Divergent/ African-Arabian/ Continental/ Shield
Convergent/ Pacific-North American/ Oceanic, Continental/ Composite
Divergent/ Eurasian-North American/ Oceanic/ Shield
Part 4:
Emperor-Hawaiian Islands and Seamounts
Seamounts and volcanic islands can record the history of plate (as in plate tectonic) motion over time.
A
description of how these islands, seamounts, and guyots formed can be found in Chapter 4 of your
textbook under “Mantle Plumes and Hotspots” (see figure 4.26).
A video resource that also discusses
how these form can be found here:
https://youtu.be/AhSaE0omw9o?si=X8euziJ0wc2I0hoQ
.
Open the folder
“Part
4
: Emperor Hawaiian Seamounts” in the “
EQ_Tect
.kmz” folder.
This folder
contains google earth placemarks of several of the islands and seamounts that make up this chain along
with the age when they were formed.
4A.
Look at the ages of these seamounts and the pattern they form on the ocean floor, noting the
“bend” about 3500 km northwest of Hawaii.
A
pproximately how long has the Pacific Plate (in
this region) been moving in its current direction?
4B.
What direction was the Pacific Plate Moving BEFORE it settled into its current direction?
4C.
Calculate the rate (cm/year) that the Pacific Plate is moving from the distances between islands and
their ages
(you will need to use the “Ruler” tool we used in the seafloor lab for this).
Steps to calculate this:
•
Select 2 islands on the southern string of the Emperor-Hawaiian Seamount chain (i.e. before the
bend), that are at least 1000 km apart (use
the “Ruler” tool
to determine this).
•
Record the distance in
centimeters
between the 2 islands you have selected (switch the units to
“Centimeters” in your ruler to do this
).
•
Record the difference in ages between these islands in Ma (To read ages:
1.32 Ma +/- 0.04
means 1.32 million years with 0.04 million years uncertainty).
•
Use the equation below to calculate the rate that the Pacific Plate is moving.
𝑅??𝑒
??
𝑦?
=
𝐷𝑖?????? ???𝑤??? 𝑖?????? (??)
𝐷𝑖???????? 𝑖? 𝐴??? (𝑀?)
∗
1 𝑀?
1,000,000 𝑦????
=
Part 5:
Age of Seafloor and Plate Tectonics
The oldest Ocean crust is around 220 million years, while the oldest rocks that have been found in
continental crust date to 4.4 billion years ago.
With your knowledge of Plate Tectonics from this lab,
what do you think explains why oceanic crust is so young compared to the oldest parts of continental
crust? (1 paragraph max)
50 million years
The shifting direction of the plate was more linear along the Emperor seamounts before it settled into its present position.
141,906,413 cm
51°28'47"N 167°35'59"E// 38°49'59"N 171°15'00"E
81 Ma // 55.4 +- 0.9Ma
141906413/25.6*1/1000000=5.5432
Because plate tectonics is dynamic, there is an age difference between oceanic and continental crust. The oldest oceanic crust
is thought to be 220 million years old, and it is continuously created along mid-ocean ridges by seafloor spreading. The history of
continental crust, on the other hand, is more complicated due to geological processes such mountain-building sequences, subduction,
and recycling of crust through continental collision. As a result, rocks from the continent that are over 4 billion years old have been
preserved. Oceanic crust is continuously recycled through subduction zones, whereas continental crust is floating, allowing it to survive
and build over time.
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