Title: Do Now:
1Do Now
- How are P and S waves affected by the medium
through which they travel? - How is the difference in arrival times for p and
s waves changed by distance from the earthquake
epicenter? (ESRT p 11) - Name the instrument used to record the arrival of
p and s waves.
21. How are P and S waves affected by the medium
through which they travel?
- Waves travel faster through denser material
- As speed changes bending (refraction) will occur
- S waves can not travel through liquid
3 2. How is the difference in arrival times for p
and s waves changed by distance from the
earthquake epicenter? (ESRT p 11)
- As the distance increases the difference in
arrival times increases
43. Name the instrument used to record the arrival
of p and s waves.
5Aim How do seismic waves behave as they travel
through the earths interior ?
- Objective
- Refraction of seismic waves
- Shadow zones
- Read the ESRT page 10
6I. Seismic Wave Behavior
- Refraction of Seismic Waves
- Shadow Zones
-
7A. Refraction of Seismic Waves
8B. P-wave Shadow Zone
- 105o ? 140o from the epicenter
- Location on the earths surface that does not
record p or s waves
9S-wave Shadow zone
10II. Inferred Properties of earths interior
- ESRT page 1O
- State the relationship between the following
variables - a. depth density
- b. depth pressure
- c. depth temperature
11a. As depth increases, the density increases
b. As depth increases, the pressure increases
c. As depth increases, the temperature increases
12Answer the following based on the ESRT page 10
- Describe the outer core. (density, pressure,
temperature, composition and phase of matter) - Provide the temperature and pressure at 3,600 km.
- Name the zone of the earths interior that is
1,000 km below the surface of the earth.
13III. Calculating Time Origin
- Time origin time at which the earthquake
occurred - Calculate the distance from the epicenter for a
station recording seismic waves - Record the arrival time of the p wave
- Calculate the time required to travel the
distance noted above - Subtract this time from the arrival time
- p wave - p wave origin time
- arrival travel time
14Summary
- Give 3 examples of information that is inferred
through the analysis of seismic waves. - An earthquake occurs somewhere in the pacific
ocean. The island of Hawaii receives p wave at
91510 AM, followed closely by S waves at
91730 AM. - Calculate the distance from the earthquake
- Calculate the origin time for this earthquake
- Can you locate the epicenter? If not, why?
- Why should residents of Hawaii be concerned?