Measuring Earthquakes Chapter

Slides:



Advertisements
Similar presentations
Friday, March 23 nd 1 Attendance 2 Go over Review Sheet Test Pass Back papers.
Advertisements

Earthquakes  Earthquakes:  the shaking and trembling that results from the movement of rock beneath Earth’s surface  See simulation below:  Terashake.
Earthquake Waves Chapter 6-2. Focus and epicenter Actual location of fault Up to 700 km below surface.
Section 1: Earth’s Crust in Motion How Do Stress Forces Affect Rock?
Warm Up – December 17 What kind of stress occurs at a divergent boundary? What type of fault is it? What landform is created? Tension Normal Fault Fault.
EARTHQUAKES, SEISMIC WAVES, & MONITORING SYSTEMS
Inside Earth: Chapter 2- Earthquakes
Lesson 2 – Earthquakes and seismic waves
Ch6 Sec2 Earthquakes and Seismic Waves. Key Concepts How does the energy of an earthquake travel through Earth? What are the scales used to measure the.
Earthquakes Chapter 5. Earthquakes What causes and earthquake? 1._____________________________________ 2.Stress adds _________ to rock and ___________.
Plate Tectonics - Part B - Earthquakes and Seismic Waves -Use your table of contents to find Chapter 14 Section 2 -Flip through the section looking at.
EARTHQUAKES & SEISMIC WAVES CHAPTER 6.2. W HAT IS AN EARTHQUAKE ? The shaking and trembling that results from the movement of rock beneath Earth’s surface.
Inside Earth Chapter 2.2 Pages 64-70
6.2 earthquakes and seismic waves By Kate, Josh, Cam, Mark, and Emily.
Earthquakes and Seismic Waves
Earthquakes.
Measuring Earthquakes Chapter 5, Section 2 Wednesday, January 27, 2010 Pages
Earthquakes.
Earthquakes.
4.2 Notes  An earthquake is the shaking and trembling that results from movement of rock beneath Earth’s surface.
Measuring CH 5 Prentice Hall p CH 5 Prentice Hall p Earthquakes.
Earthquakes.
Chapter 6 Earthquakes.
What causes an earthquake?  Deformation- the change in shape of rock in response to stress  Elastic Rebound- Return of rock to its original undeformed.
Earthquakes and Seismic Waves. Earthquake: Shaking and trembling that results from the movement of rock beneath Earth’s surface. The forces of plate movement.
Earthquakes Chapter 2 book F page 44. Vocabulary for section 1 page 44 book F Stress Tension Compression Shearing Normal fault Reverse fault Strike-slip.
Inside Earth Chapter 2 Earthquakes 2.2 Earthquakes and Seismic Waves.
Section 1: Earth’s Crust in Motion How Do Stress Forces Affect Rock? The movement of earth’s plates creates powerful forces that squeeze or pull the rock.
Aim: What are Earthquakes and their characteristics? I. Earthquakes – any vibrating, shaking, or rapid motion of Earth’s crust. A. Fault – zone of weakness.
6 th Grade EarthScience Project Earth Science- The Science that focuses on the planet Earth and its place in the Universe. Teacher: Ms. DiMatteo.
Earthquake Waves Chapter 6-2. Focus and epicenter Actual location of fault Up to 700 km below surface.
Aim: What are Earthquakes and their characteristics? I. Earthquakes – any vibrating, shaking, or rapid motion of Earth’s crust. A. Fault – zone of weakness.
Earthquakes and Seismic Waves 2-1. What is an Earthquake? Shaking and trembling that results from the movement of rock beneath Earth’s surface Occur when.
EARTHQUAKES, SEISMIC WAVES, & MONITORING SYSTEMS.
 Earthquake = the shaking and trembling that results from movement of rock beneath Earth’s surface  Focus = area beneath Earth’s surface where rock.
Measuring Earthquakes (5-2 Notes). Magnitude = a measure of an earthquake’s strength Based on seismic waves.
Earthquakes.
What are Earthquakes? The shaking or trembling caused by the sudden release of energy Usually associated with faulting or breaking of rocks Continuing.
Measuring Earthquakes. Earthquakes start at the focus Earthquakes produce seismic (sizemic) waves.
Earthquakes and Seismic Waves
Earthquakes Pages C14-17.
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 & Seismic Waves.
Earthquakes.
Earthquakes.
Earthquakes Chapter Notes.
Earthquakes and Seismic Waves
Do Now Which type of boundary creates new lithosphere/oceanic crust?
Earthquakes and Seismic Waves (Part 2)
Earthquake Notes.
6th Grade Earthquakes Mrs. Akin.
Earthquakes Chapter 11.
Earthquakes & Plate Tectonics
Inside Earth, Chapter 2, Section 2
Chapter 5 Earthquakes.
Earthquakes Chapter 19.
Earthquakes Waves and Faults.
Chapter 12-2 Studying Earthquakes.
CH. 14 Vocabulary test study guide
Section 6.2: Earthquakes and seismic waves
The average length of an earthquake is from 30 to 60 seconds.
Key Terms 5.2.
Earthquake Waves Chapter 6-2.
Earthquakes.
Earthquakes.
Earthquakes and Seismic Waves
EARTHQUAKES EARTHQUAKES- THE ROCKING AND ROLLING OF THE LITHOSPHERE
Earthquakes.
Earthquakes.
Chapter 5.2 Earthquakes and seismic waves
Presentation transcript:

Measuring Earthquakes Chapter 5.2-5.3

Where do Earthquakes begin? What is the difference between the focus and epicenter? Earthquakes always begin in rock below the surface, usually within 100 km of Earth’s surface. Focus: The point where rock that is under stress breaks, triggering an earthquake. Epicenter: The point on the surface directly above the focus. Epicenter/focus animation

What are seismic waves? Where are the seismic waves the strongest? Seismic Waves: vibrations that travel in a ripple through Earth, carrying the energy released during an earthquake. .

Three Categories of Seismic Waves P Waves (Primary Waves) - First to arrive at a seismograph - compress and expand ground

Three Categories of Seismic Waves (cont.) 2) S Waves (Secondary Waves) - Vibrate from side to side AND up and down - 2nd to arrive at seismograph Animation of P and S waves Video on P and S Waves

3) Surface Waves. Produce the most severe ground movements. Three Categories of Seismic Waves (cont.)

How do we detect seismic waves? How do we measure earthquakes? Seismograph: a machine that records the ground movements caused by seismic waves as they move through the earth. seismograph animation Magnitude: measurement of earthquake strength based on seismic waves and movement along faults.

3 types of rating scales (continued) Mercalli Scale – Not a precise measurement The same earthquake can have different ratings

2) Richter Scale Rates size of seismic waves with a mechanical seismograph Accurate for small, nearby earthquakes Not accurate for large or distant earthquakes. 3) Moment Magnitude Scale Estimates total energy released by earthquake Used to accurately rate all earthquakes of all sizes, near or far What we currently use Which scale do we use today?

How many seismographs do you need to determine an epicenter Locating the epicenter: You need 3 seismographs to determine an epicenter. Locating an Epicenter Video