EQ_Tect_Activity

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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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