Understanding S Waves and Seismograms

Understanding S Waves and Seismograms

Assessment

Interactive Video

Physics

9th - 10th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video tutorial explains the behavior and variations of S-type seismic body waves, including SS and SSS waves, and their interactions with the Earth's core-mantle boundary. It discusses the concept of seismic shadow zones and the diffraction of S waves, leading to Sdiff paths. The tutorial highlights the complexity of interpreting seismograms from large earthquakes and provides resources for further learning about shadow zones and p-waves.

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9 questions

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1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What type of waves are S-type seismic body waves?

Surface waves

Longitudinal waves

Compressional waves

Shearing waves

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the maximum angle from the epicenter that S waves can reach a seismograph station?

103 degrees

180 degrees

90 degrees

120 degrees

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is the term used for the area beyond 103 degrees from the epicenter where S waves do not reach?

Seismic diffraction zone

Seismic blackout zone

Seismic reflection zone

Seismic shadow zone

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How does an SS wave differ from a regular S wave?

It bounces off the Earth's surface

It travels through the core

It is slower than an S wave

It travels in a straight line

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is an SSS wave?

An S wave that is slower than an SS wave

An S wave that travels in a straight line

An S wave that reflects twice off the surface

An S wave that travels through the core

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How can S waves reach seismometers in the shadow zone?

By traveling through the core

By diffracting at the mantle-core boundary

By reflecting off the surface

By traveling in a straight line

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What are Sdiff waves characterized by?

Low speed and straight path

High speed and direct path

Small amplitude and gradual onset

High amplitude and sharp onset

8.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What makes interpreting seismograms from large earthquakes challenging?

The lack of wave arrivals

The simplicity of wave patterns

The uniformity of wave arrivals

The complex interwoven pattern of wave arrivals

9.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What additional resource is suggested for learning about shadow zones and p-waves?

The website mentioned in the video

A scientific journal

A documentary

A textbook