Search the courses, subjects, tracks, games and features, or jump straight to a page.
Learn it your way
A short class with Sarah and her students. The other ways are under More.
Sign up free to listen. Transcripts are free to read.
Today, we're going to recap the classification of seismic waves. Can anyone tell me how seismic waves are generally classified?
I think they are classified into body waves and surface waves.
Exactly! Body waves travel through the interior of the Earth. Can anyone name them?
P-waves and S-waves!
Correct! And what about surface waves?
Rayleigh waves and Love waves.
Great job! Let's remember this by using the mnemonic 'Bows Slip Right'—Body waves, Surface waves, S-waves, and Rayleigh waves.
To summarize, seismic waves can be divided into two main categories: body waves and surface waves. Body waves include P-waves and S-waves, while surface waves include Rayleigh and Love waves.
Now, let's discuss S-waves and Rayleigh waves specifically. What can you tell me about S-waves?
S-waves are transverse waves that move the ground perpendicular to their direction of travel.
Exactly! And do S-waves travel through fluids?
No, they do not.
Right! And how about Rayleigh waves?
Rayleigh waves move in an elliptical motion and cause vertical and horizontal ground shaking.
Perfect! So we can remember that S-waves cause side-to-side motion while Rayleigh waves move like ocean waves. Let's summarize: S-waves cause transverse displacement and do not travel through fluids, while Rayleigh waves cause elliptical motion at the surface.
Seismic waves that travel through the Earth's interior, including P-waves and S-waves.
Seismic waves that travel along the Earth's surface, including Rayleigh and Love waves.
Secondary or shear waves that move perpendicular to wave propagation and do not pass through fluids.
Surface waves that exhibit retrograde elliptical motion.
Waves go deep and waves go wide, Body waves and surface glide.
Once in a land where the ground shook, S-waves were playing with the dirt, and Rayleigh waves danced gracefully like ocean waves on a beach.
Remember 'B-S-R' for Body waves, Shear waves, and Rayleigh waves.
B.S.R. = Body waves, Shear waves, Rayleigh waves.
Term
What are Body Waves?
Click to flip
Term
What are S-waves?
Click to flip
Term
What are Rayleigh Waves?
Click to flip
Seismic waves that travel through the interior of the Earth, including P-waves and S-waves.
Primary or Compressional Waves that are the fastest seismic waves, compressing and expanding the ground.
Secondary or Shear Waves that cause perpendicular motion to the wave's direction and cannot propagate through fluids.
Seismic waves that travel along the Earth's surface, including Rayleigh waves and Love waves.
Surface waves that cause retrograde elliptical motion, affecting both vertical and horizontal ground displacement.
A type of surface wave that causes horizontal shearing of the ground.
This section summarizes the classification of seismic waves into body waves and surface waves, specifically focusing on Shear waves (S-waves) and Rayleigh waves.
Seismic waves are classified into body waves, which travel through the Earth's interior (P-waves and S-waves), and surface waves, which travel along the Earth's surface (Rayleigh and Love waves). Understanding this classification is crucial for grasping the properties of S-waves and Rayleigh waves and their implications for earthquake engineering.
In earthquake engineering, accurate classification of seismic waves is essential for analyzing ground motion and designing earthquake-resistant structures. Seismic waves can be categorized as:
Body Waves: These waves travel through the interior of the Earth. They include:
Surface Waves: These waves travel along the Earth's surface and include:
This chapter emphasizes S-waves and Rayleigh waves, outlining their characteristics and effects on structures, which are vital for earthquake hazard assessment and construction design.