Instructional Video
Incorporated Research Institutions for Seismology

Iris: Travel Time Curves: How They Are Created

9th - 10th
An animation which illustrates how the travel time of an earthquake is measured. What alters the velocity of the waves? [1:06]
Instructional Video
American Geosciences Institute

American Geosciences Institute: Big Idea 8: Natural Hazards Affect Humans

3rd - 7th
Watch how natural hazards occur, how they affect our lives and what we can do to prepare for and mitigate their effects. [4:27]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: New Madrid Earthquake: A River Runs Backward

9th - 10th
Watch a river change its course and even flow backward. An animated earthquake shows what happens to the water in a river and possible effects of the surrounding area.
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Seismic Wave Behavior: Critically Refracted Rays Ping Arrivals

9th - 10th
A brief video will illustrate how a ping announces refracted seismic waves. [0:34]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Seismograph: Horizontal

9th - 10th
A brief animation which illustrates how a horizontal seismograph works. A seismograph measures wave activity. [0:19]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Seismograph: Vertical

9th - 10th
This short clip will illustrate how a seismograph measures vertical motion in the Earth. [0:14]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Seismograph: Vertical (Slow Motion)

9th - 10th
A "quick" slow motion clip illustrates how a seismograph measures the vertical motion of S and P waves. [0:13]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Volcano Monitoring: Volcanic Earthquakes

9th - 10th
Find the connection between earthquakes and volcanoes. This clip will illustrate volcanic earthquakes. [1:44]
Instructional Video
National Science Foundation

National Science Foundation: Engineering Innovative Seismic Retrofits That Don't Break the Bank

9th - 10th
Researchers at the state-of-the-art Structural Engineering and Materials Laboratory at the Georgia Institute of Technology are using a full-scale model building to test new ways to protect structures from earthquakes and potentially save...
Instructional Video
US Geological Survey

U.s. Geological Survey: Earthquakes: Divergent Boundary

9th - 10th
Nice, visual animation showing what happens under the Earth's surface at a divergent boundary.
Instructional Video
US Geological Survey

U.s. Geological Survey: Earthquakes: Elastic Rebound

9th - 10th
This captioned animation describes the elastic rebound effect, which happens as a result of an earthquake.
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Types of Seismic Wave Paths Through the Earth

9th - 10th
Video lecture describing speeds and paths of different seismic waves within Earth from an earthquake to a distant seismic station. P & S waves travel through the Earth; Surface waves travel around the perimeter of the Earth. [1:44]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Seismic Waves: P, S, and Surface

9th - 10th
Video lecture on wave motions and speeds of three fundamental kinds of seismic waves: Primary (P = pressure) waves; Secondary (S = shear); and Surface waves. [3:10]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Travel Time Curves: How They Are Created

9th - 10th
See how travel-time curves are created. [2:52]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: 4 Station Seismograph Network; No Cartoon House Bounce

9th - 10th
See what seismograms look like at increasing distances from the epicenter. [0:21]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: 1 Component Seismogram: Building Responds to P, S, Surface Waves

9th - 10th
See how surface waves and P and S-Waves affect Earth's surface. [0:36]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Magnitude Explained: Moment Magnitude vs. Richter Scale

9th - 10th
Scientists have developed far-more sensitive seismometers that, with faster computers, have enabled them to record & interpret a broader spectrum of seismic signals than was possible in the 1930's, when the Richter magnitude was...
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Earthquake: Foreshock Mainshock Aftershock

9th - 10th
Learn how foreshocks and aftershocks are related to the main shocks of earthquakes. [6:32]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Exploring Seismic Waves With Slinkys

9th - 10th
This demonstration shows that seismic waves propagate in all directions in the Earth from the source (not just in the direction of a single slinky). [5:13]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Earthquake Machine: Demonstration of the 2 Block Model

9th - 10th
See how to model differential friction along a fault. [2:30]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Human Wave Demo Modeling P & S Waves in Solids & Liquids

9th - 10th
This demonstration explores two of the four (P and S waves) main ways energy propagates from the hypocenter of an earthquake. [8:27]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Chile (2010) vs Sumatra (2004)

9th - 10th
Learn how Chile's tectonic setting and megathrust earthquake of 2010 is similar to the catastrophic earthquake in Sumatra in 2004 by touching icons on this interactive map.
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Fault: Oblique

9th - 10th
Find out the motion that is halfway between a normal fault and a strike-slip fault. [0:15]
Instructional Video
Incorporated Research Institutions for Seismology

Iris: Asperities on Strike Slip Fault: Spaghetti in Vise as an Analogy

9th - 10th
This demonstration, squeezing uncooked spaghetti noodles in a wood template set in a vise, effectively shows how asperities (stuck patches) on a fault rupture at different times. [1:44]