IRIS Earthquake Science
Hawai`i—Origin of Earthquakes & What causes them (Educational)
updated
Residents of California, Oregon and Washington now have an earthquake early warning tool—the ShakeAlert© system, operated by the United States Geological Survey.
To download a copy of the mp4, see EarthScope / SAGE InClass: https://www.iris.edu/hq/inclass/animation/earthquake_early_warning_system_for_the_pacific_northwest
Presented on: November 10, 2022
Presented on: October 27, 2022
Presented on: September 29, 2022
What if you had only 30 seconds to introduce yourself to someone working at your dream company? How would you get them interested enough to keep talking to you so you could learn about potential job opportunities?
Elevator speeches, or elevator pitches, are a form of networking in which you describe yourself and your work in about 30 seconds. Importantly, they include a “hook” – some interesting and relevant information that grabs your audience’s attention to engage them in the conversation. They’re called “elevator speeches” because they should be about the length of time it takes to ride an elevator to another floor. They make the perfect opportunity to open a short conversation with a potential employer.
This resource has been developed as part of the SAGE facility operated by IRIS via support
from the National Science Foundation.
For more animations on tectonic settings worldwide: www.iris.edu/earthquake
Written & directed by Dr. Robert F. Butler, University of Portland
Narrated by Asenath Kwagalakwe, VA Tech, and Dr. Wendy Bohon, IRIS.
Animation & graphics by Jenda Johnson, Earth Sciences Animated
Edited by Dr. Beth Pratt-Sitaula, UNAVCO and Dr. Sarah Stamps, Virginia Tech
Photographs from: Sarah Stamps; UNAVCO; Public domain sources
Maps from GeoMappApp and the U.S. Geological Survey
Earthquake locations from IRIS Earthquake Browser (www.iris/ieb)
Microplate rotations: Sarah Stamps et al, 2020, Redefining East African Rift System kinematics; in Geology
Rifting stages modified from Biggs et al., 2021, Volcanic activity and hazard in the East African Rift Zone; in Nature Communications
Video footage of Agadir is from the Associated Press (copyright)
Music from Youssoupha Sidibe, Sacred Sound (freemusicarchive.org) and Nnankasaa, Awatsimnba, and Wogala, Elgon Troup (freemusicarchive.org)
Dr. Derek Schutt, Colorado State University (Derek.Schutt@colostate.edu)
Dr. Tolulope Olugboji, University of Rochester (tolulope.olugboji@rochester.edu)
Dr. Margarete Jadamec, University at Buffalo (mjadamec@buffalo.edu)
Presented on May 26, 2022
Kīlauea volcano in Hawai‘i is one of the most active volcanoes in the world. The U.S.G.S./HVO operates an extensive seismic network to monitor and investigate hazards from active volcanoes and earthquakes on the Island of Hawai‘i. Seismic investigations have considerable potential for addressing key issues regarding the evolution of volcanic and tectonic activity in Hawai‘i. Specifically, what is the relationship between crustal stress changes and past and future seismic and volcanic events? To what extent are stress changes explained by known events and how predictive are they of future events? In 2018, Kīlauea experienced its largest Lower East Rift Zone eruption and caldera collapse in the past 200 years. This activity provided an unprecedented opportunity for seismologists to investigate the interactions between seismic and magmatic processes and for the general community to learn how seismologists use earthquake data to monitor volcanoes. In this talk, I will present the seismic activity in Kīlauea based on the 33 years of HVO records and focus on the changes in earthquake distribution, seismic wave speeds, and stress field before and after the 2018 eruption. I will also review the geological setting and volcanic activity of Kīlauea volcano along with other volcanoes on the Big Island.
IRIS Recent Earthquake Teachable Moments (www.iris.edu/retm) capture that unplanned opportunity to bring knowledge, insight, and critical thinking to the classroom following a newsworthy earthquake. Each IRIS Teachable Moment: —Is a 5-15 slide PowerPoint presentation that — contains interpreted USGS regional tectonic maps and summaries, computer animations, seismograms, AP photos, and other event-specific information — Generated within hours of the event! — Prepared by seismologists and educators! — A classroom-ready product that can be customized! — Is pushed to you through notifications when new products are ready!
Stanford University/Incorporated Research Institutions for Seismology/U.S. Geological Survey collaboration.
In 2018, Kīlauea Volcano experienced its largest caldera collapse in more than 200 years profoundly changing the landscape. We use a highly simplified cross section of a magma reservoir and the overlying caldera to look at the subterranean architecture of Kilauea, and to show how the massive outpouring of lava in 2018 caused the summit of the volcano to collapse.
Presented on: April 14, 2022
Nicolas Arcos, NOAA NCEI
Lindsey Wright, CIRES - University of Colorado at Boulder, NOAA NCEI
Presented on: March 10, 2022
Natural Hazards Databases at NCEI
ngdc.noaa.gov/hazel/view/about
Natural Hazards Map Viewer
ncei.noaa.gov/maps/hazards
Tsunami Events Time-Lapse Animation
ncei.noaa.gov/maps/tsunami-events
Tsunami Events Time-Lapse Animation Teacher Guide and Tsunami Worksheet
ncei.noaa.gov/news/ncei-supports-natural-hazards-education
NCEI Tsunami Information and Data
ngdc.noaa.gov/hazard/tsu.shtml
Presented on: February 11, 2022
0:01 Tell Us About Yourself
0:39 What was your career path?
1:23 What are some geoscience topics you find interesting?
3:37 What skills, training, and certifications do you need for your work?
4:56 What are opportunities for growth in your position/field?
7:33 How do you find a mentor?
8:50 How do you balance your work and personal life?
10:46 What advice would you give to students interested in geology?
Timestamps:
0:00 Tell Us About Yourself
1:06 What does your work day look like?
2:26 What topics related to geophysics interest you most?
2:53 What were the steps you took in your academic career that led you to your current position?
4:00 What barriers did you encounter in this aspect of your life?
4:44 How financially obtainable do you think a degree in geoscience is?
5:58 What skills were applicable in your career?
6:52 What is your workplace atmosphere like?
7:34 What advice would you give to students pursuing a career in geoscience?
CHAPTERS:
0:00 Intro on mantle convection
0:27 Young hot vs Old cold plates
1:10 Spreading ridges
3:44 Gravity force that pushes
4:15 Force that pulls subducting slab
6:05 Push & pull in action on Pacific Plate
6:20 Thermal convection system
6:52 Convection system in 3D
This January 2022 updated version of our animation addresses convection at the end.
Lithospheric plates are part of a planetary scale thermal convection system. The energy source for plate tectonics is Earth’s internal heat while the forces moving the plates are the “ridge push” and “slab pull” gravity forces.
It was once thought that mantle convection could drive plate motions. Early textbooks showed mantle convection cells, like in a beaker of hot liquid on a Bunson burner, pushing plates along from below. Current dynamic models have plates moving as part of a gravity-driven convection system that pushes young hot plates away from spreading ridges and pulls old cold plates down into subduction zones.
Narrated by Roger Groom, Mount Taber Middle School
Animation & graphics by Jenda Johnson, Earth Sciences Animated
Directed by Robert Butler, Geophysicist, University of Portland, OR
Scientific review by Michael Wysession, Washington University in St. Louis
Technical advisor Glenn Kroeger, Trinity University
Dr. Bunsen Honey Dew II: transformative and fair use of Dr. Bunsen Honeydew© used for educational non-commercial purposes only.
Map of sea-floor ages, math of world bathymetry, and bathymetric profile of the E. Pacific Rise from the National Oceanic & Atmospheric Administration
Cross section of tectonics modified from USGS This Dynamic Earth
Landslide animation: NASA's Goddard Space Flight Center
Made possible by support from the National Science Foundation
0:01 – Introduction
1:27 – What do you study?
2:23 – How financially obtainable do you think a career in geoscience is?
3:35 – What skills, training, or certifications do you need for your work?
4:03 – Do you feel financially stable in your career?
5:34 – What are the opportunities for growth within seismology and geophysics?
6:32 – What barriers have you faced In your academic and career path?
8:14 – When have you felt uncomfortable as a geoscientist?
9:27 - What advice would you give to a student interested in pursuing geoscience?
10:05 – What roles have mentors have mentors had in your life?
Derek Schutt was a first-generation college student and is currently an Associate Professor in Seismology at Colorado State University. In Derek’s interview, he discusses his path in academia, current research, advice for students, and more.
TIME CODES:
0:00 How did you become interested in geoscience?
2:30 What does your workweek look like?
3:04 What research topic do you find interesting?
4:11 What do you think are some barriers within your field of work?
5:40 What opportunities are available for people who want to pursue Geophysics?
6:40 What advice do you have for students interested in geoscience?
University of Illinois Chicago in collaboration with the Incorporated Research Institutions for Seismology
The PIS wish to thank the NSF for their award, EAGER: EAR-2042011 EArly-concept Grants for Exploratory Research (EAGER)
Presented on: November 11, 2021
IF/THEN (supported by AAAS, American Association for the Advancement of Science) partners with Incorporated Research Institutions for Seismology (IRIS) and Earth Sciences Animated.
IF/THEN (supported by AAAS, American Association for the Advancement of Science) partners with Incorporated Research Institutions for Seismology (IRIS) and Earth Sciences Animated.
This animation looks at a basic physical comparison of the Earth with our closest neighbor, Mars. In 2018, InSight put an IRIS seismograph on Mars. Why would we do that? The purpose is to study that planet's deep interior by monitoring any earthquakes that are generated and using the information to determine a general picture of what lies below the surface. It quickly answered the question, "does Mars have earthquakes?" It does. Is it a layered planet like Earth? How thick are the layers?
Animation narrated by Michael Hubenthal, IRIS education specialist
Animated by Jenda Johnson, Earth Sciences Animated
Funded by the National Science Foundation.
Reviewed by William A. Gutsch, Jr., Astronomer, Saint Peters University
IF/THEN (supported by AAAS, American Association for the Advancement of Science) partners with Incorporated Research Institutions for Seismology (IRIS) and Earth Sciences Animated.
IF/THEN (supported by AAAS, American Association for the Advancement of Science) partners with Incorporated Research Institutions for Seismology (IRIS) and Earth Sciences Animated.
IF/THEN (supported by AAAS, American Association for the Advancement of Science) partners with Incorporated Research Institutions for Seismology (IRIS) and Earth Sciences Animated.
Colorado State University in collaboration with the Incorporated Research Institutions for Seismology
The PIs wish to thank the NSF for their award, EAGER: EAR-2041967 EArly-concept Grants for Exploratory Research (EAGER)
Colorado State University in collaboration with the Incorporated Research Institutions for Seismology
The PIs wish to thank the NSF for their award, EAGER: EAR-2041967 EArly-concept Grants for Exploratory Research (EAGER)
Colorado State University in collaboration with the Incorporated Research Institutions for Seismology
The PIs wish to thank the NSF for their award, EAGER: EAR-2041967 EArly-concept Grants for Exploratory Research (EAGER)
Colorado State University in collaboration with the Incorporated Research Institutions for Seismology The PIs wish to thank the NSF for their award, EAGER: EAR-2041967 EArly-concept Grants for Exploratory Research (EAGER)
This animation is a composite of TWO separate IRIS animations:
2010 Haiti Earthquake—10-yrs later: www.iris.edu/hq/inclass/animation/650
and
Hispaniola Tectonics & Earthquakes: www.iris.edu/hq/inclass/animation/714
IF/THEN (supported by AAAS, American Association for the Advancement of Science) partners with Incorporated Research Institutions for Seismology (IRIS) and Earth Sciences Animated.
Copyright: Song in dance video by Quimbara.
Download mp4 @ EarthScope / SAGE InClass:
https://www.iris.edu/hq/inclass/animation/781
IF/THEN (supported by AAAS, American Association for the Advancement of Science) partners with Incorporated Research Institutions for Seismology (IRIS) and Earth Sciences Animated.
Narrated by Dr. Wendy Bohon, IRIS
Written by Dr. Gabriel Lotto, University of Washington and Dr. Danielle Sumy, IRIS
Animated by Jenda Johnson, Earth Sciences Animated
To download a copy of the mp4, see EarthScope / SAGE InClass: https://www.iris.edu/hq/inclass/animation/earthquake_alert_times_in_the_pacific_northwest
https://www.iris.edu/hq/inclass/animation/635
Normal fault—the block above the inclined fault moves down relative to the block below the fault. This fault motion is caused by extensional forces and results in extension. [Other names: normal-slip fault, tensional fault or gravity fault] Examples include Basin & Range faults. Reverse fault—the block above the inclined fault moves up relative to the block below the fault. This fault motion is caused by compressional forces and results in shortening. A reverse fault is called a thrust fault if the dip of the fault plane is small. [Other names: reverse-slip fault or compressional fault.] Examples include the Rocky Mountains and the Himalayan Mountains. Strike-slip fault—movement of blocks along a fault is horizontal and the fault plane is nearly vertical. If the block on the far side of the fault moves to the left, as shown in this animation, the fault is called left-lateral (Figure 2). If it moves to the right, the fault is called right-lateral. The fault motion of a strike-slip fault is caused by shearing forces. [Other names: trans current fault, lateral fault, tear fault or wrench fault.] Examples include the San Andreas Fault, California; Anatolian Fault, Turkey.
0:00 Intro
0:26 What IS stress?
1:03 Type of stress
1:50 Elastic deformation
3:20 Ductile deformation
4:04 Brittle deformation
5:52 Extensional stress
6:18 Compressional stress
6:59 Shear stress
8:01 Conclusion
This animation describes stress in Earth's outer layer and how it leads to faults and plate boundaries.
Earth’s thin, brittle outer shell of rock is under a constant state of stress. Stress impacts the formation of small local faults, and broader tectonic plate boundaries.
How the rock responds, depends on the type of stress and the conditions the rock is being subjected to when it encounters stress. It is this change in Earth’s crust that generates different types of faults and plate boundaries.
IF/THEN (supported by AAAS, American Association for the Advancement of Science) partners with Incorporated Research Institutions for Seismology (IRIS) and Earth Sciences Animated.
Additional photo credits to Dr. Danny Hilman Natawidjaja and Dwi Indriyati.
Si te encuentras en un edificio durante un terremoto, la forma en que está construido y tu ubicación en el edificio pueden tener un efecto en el temblor que sientes. Esto significa que puedes experimentar un terremoto de manera diferente a alguien que se encuentra a solo unos edificios de distancia. El tipo de construcción también tiene un gran efecto sobre si un edificio sufre daños en un terremoto.