Daily Routine Sit in your appropriate seat quietly

Slides:



Advertisements
Similar presentations
Seismic waves and the shadow zone.  Sudden release of energy in the Earth’s crust and creates seismic waves. Occurs naturally or human induced.
Advertisements

Earthquakes Section 2 Section 2: Studying Earthquakes Preview Key Ideas Recording Earthquakes Locating an Earthquake S-P-Time Method: Finding an Epicenter.
Seismology: ●What is Seismology? ●What are Seismic Waves?: Types of Seismic waves ●Where do Earthquakes Happen? ●Why do Earthquakes Happen? ●How is the.
Studying Earthquakes. Seismology: the study of earthquakes and seismic waves.
Ch. 6.2 Recording Earthquakes
8.2 Measuring Earthquakes
Section 2: Studying Earthquakes
Inside Earth Chapter 2 Earthquakes 2.2 Earthquakes and Seismic Waves.
Earthquake Measurement 10/23/14
Seismographs Are instruments located at or near the surface of the Earth that record seismic waves.
Earthquakes.
Measuring Earthquakes
Measuring Earthquakes (5-2 Notes). Magnitude = a measure of an earthquake’s strength Based on seismic waves.
Earthquakes. Causes of Earthquakes An earthquake is a shaking of Earth’s crust caused by a release of energy Mostly caused by the strain that builds.
Locating Earthquakes. Seismic wave behavior ► P waves arrive first, then S waves, then L and R ► Average speeds for all these waves is known.
8.2 Measuring Earthquakes  A) Seismographs - instruments that record earthquake waves.  B) Seismograms electronically recorded ground motion made by.
Earthquakes and Earthquake Waves
 Energy travels as seismic waves which are vibrations caused by earthquakes.  All earthquakes start beneath the earth’s surface.
Epicenters Infer an earthquake’s epicenter from seismographic data.
Objectives How does the energy of an earthquake travel through Earth? What are the scales used to measure the strength of an earthquake? How do.
Earthquakes. Causes of Earthquakes An earthquake is a shaking of Earth’s crust caused by a release of energy Mostly caused by the strain that builds.
EARTHQUAKES Part II .
Notes 11 Earthquake Magnitude.
Section 6.5: Studying Earthquakes
Earthquake Measurement 7-2
Ch.5, Sec.2 - Earthquake Measurement
Earthquake Measurement
Daily Routine Sit in your appropriate seat quietly
Daily Routine Sit in your appropriate seat quietly
Daily Routine Sit in your appropriate seat quietly
Daily Routine Sit in your appropriate seat quietly
8.2 – Measuring Earthquakes – Part II
Measuring Earthquakes
Daily Routine Sit in your appropriate seat quietly
DO NOW Pick up notes..
Daily Routine Sit in your appropriate seat quietly
Daily Routine Sit in your appropriate seat quietly
Daily Routine Sit in your appropriate seat quietly
Earthquake Measurement
Using Distances to known Earthquake epicenters, create
Daily Routine Sit in your appropriate seat quietly
Daily Routine Sit in your appropriate seat quietly
Daily Routine Sit in your appropriate seat quietly
Seismic Waves 3d - Students know why and how earthquakes occur and the scales used to measure their intensity and magnitude.
Chapter 12-2 Studying Earthquakes.
Daily Routine Sit in your appropriate seat quietly
Daily Routine Sit in your appropriate seat quietly
Daily Routine Sit in your appropriate seat quietly
Earthquakes.
Daily Routine Sit in your appropriate seat quietly
Daily Routine Sit in your appropriate seat quietly
8.2 Measuring Earthquakes
Daily Routine Sit in your appropriate seat quietly
Key Terms 5.2.
Do Now Describe the last earthquake you can remember. (location, strength, time of day, how it felt, etc.) Where do earthquakes occur? Why do earthquakes.
Do First Which type of lava does not trap gases?
So why are seismograms so important?
Thank you for not chewing gum or anything else 
Daily Routine Sit in your appropriate seat quietly
Daily Routine Sit in your appropriate seat quietly
Earth Shakes, Rattles, and Rolls
Chapter 12 - Section 2 Measuring Earthquakes
Thank you for not chewing gum or anything else 
Chapter 12 - Section 2 Measuring Earthquakes
Daily Routine Sit in your appropriate seat quietly
Daily Routine Sit in your appropriate seat quietly
Daily Routine Sit in your appropriate seat quietly
Earthquake Measurement
Chapter 5.2 Earthquakes and seismic waves
Journal #72 Draw a picture of an earthquake (lithosphere) label the focus, epicenter and fault.
Presentation transcript:

Daily Routine Sit in your appropriate seat quietly Have all necessary materials out All back packs on the floor All cell phones on silent and away in backpacks All IPods off and headphones out of your ears Hats off No food or drink except for water

Bellwork What are seismic waves? Describe the three types of seismic waves. What are the three types of faults?

Earth Science Announcements Volcano Project: Due Today Midterm 10/9 or 10/10

How to find the epicenter How does earthquakes affect our lives?

Richter Moment of Magnitude Scale Developed by Charles Richter in 1935 Mathematical calculation for the intensity of an earthquake Calculated using the amplitude of the waves on a seismogram Measures surface waves energy from the epicenter Increases by a factor of 10 (log) Represented by whole numbers and decimals

Richter Moment of Magnitude Scale

What is the usefulness of a seismogram? Determine amplitude of waves from an earthquake Calculate magnitude of an earthquake Calculate where the epicenter of an earthquake is

Distance To Earthquake Epicenter S-P Time Delay = Distance to Epicenter Scientists use the seismograph to locate the epicenter of an earthquake Remember, the P-wave is faster and arrives first at a seismic station Every Seismograph records a time delay between the P and S and waves The farther from the earthquake epicenter, the greater the time delay This time delay between the P and S wave is used to find the distance to the earthquake epicenter P-Wave Arrival Time S-Wave Arrival Time Surface-Waves Surface-Waves P-Waves P-Waves S-Waves S-Waves

Distance To Epicenter Distance to Epicenter ---------- = S - waves --------- = P - waves P-Waves S-Waves Seismic Station Epicenter

S-Wave Time - P-Wave Time Distance

Let’s practice

Math work S Wave comes in at: 25:00 minutes

Let’s practice

Math work S Wave comes in at: P wave comes in at: 25:00 minutes

Let’s practice

Math work S Wave comes in at: P wave comes in at: Do the math: 25:00 minutes 20:00 minutes 25-20:00 = 5:00 minutes

S-P Time Delay = Distance to Epicenter P-Wave S-Wave Seismic Station A Epicenter The time delay between the S and P wave gives us the Distance to the epicenter In other words, S-P Time Delay = Distance to Epicenter

Triangulation P-Wave S-Wave Seismic Station A Epicenter Epicenter Station B P-Wave Seismic Station C

Daily Routine Sit in your appropriate seat quietly Have all necessary materials out All back packs on the floor All cell phones on silent and away in backpacks All IPods off and headphones out of your ears Hats off No food or drink except for water

Bellwork What do you use to determine how far the epicenter is located from a seismic station? Why can’t one seismic station determine where the epicenter of an earthquake is located? How many stations do you need to make a better locate the epicenter?

Earth Science Announcements Volcano Project: Due Today Midterm 10/9 or 10/10

How to find the epicenter How does earthquakes affect our lives?