Section 6.5: Studying Earthquakes

Slides:



Advertisements
Similar presentations
Measuring Earthquakes
Advertisements

Earthquakes and Earth’s Interior
Earthquakes.
Seismic waves and the shadow zone.  Sudden release of energy in the Earth’s crust and creates seismic waves. Occurs naturally or human induced.
Earthquakes.
Earthquakes Section 2 Section 2: Studying Earthquakes Preview Key Ideas Recording Earthquakes Locating an Earthquake S-P-Time Method: Finding an Epicenter.
Earthquake Measurement
Measuring Earthquakes. Seismograph Or seismometer, is an instrument used to detect and record earthquakes.
Earthquakes.
Studying Earthquakes. Seismology: the study of earthquakes and seismic waves.
LEQ: How are Earthquakes Measured?
Measuring Earthquakes Chapter 5, Section 2 Wednesday, January 27, 2010 Pages
Earthquakes.
Chapter 12 Study Notes Earthquakes. 1 A ____ wave is a seismic wave that travels through the _____ of the earth. –body –interior.
Earthquakes.
Section 12-2 Review Page 304 (1-5)
Ch. 6.2 Recording Earthquakes
Earth Science 8.2 Measuring Earthquakes
8.2 Measuring Earthquakes
Measuring Earthquakes. (1) How are earthquakes studied? – or, seismograph, an instrument that measures ground vibrations seismometer – or, seismograph,
Section 2: Studying Earthquakes
Inside Earth Chapter 2 Earthquakes 2.2 Earthquakes and Seismic Waves.
#18 Measuring Earthquakes. How are earthquakes studied? Seismologists use seismometers, or seismographs, an instrument that measure vibrations in the.
Do Now – In Notebooks 1. What is an earthquake? 2. What kind of stress acts on a normal fault? Does the crust lengthen or shorten? 3. What is the difference.
Seismographs Are instruments located at or near the surface of the Earth that record seismic waves.
Earthquakes HOW IS IT MEASURED?.  Instrument located at or near the earth’s surface to record seismic waves. (Tool) SEISMOGRAPH.
Earthquake Scales Richter vs. Mercalli. What is an earthquake? Earthquakes are the vibration of the earth as a result of a release of energy – Earthquakes.
How do scientists know the structure of the Earth? Rock samples (direct evidence) Seismic waves (indirect evidence) –Vibrations that travel through Earth.
Earthquake Measurement Science Chapter 7, Section 2 Notes Science Chapter 7, Section 2 Notes.
Handout 3 (2-3) green “Recording Earthquakes”
Measuring Earthquakes
Measuring Earthquakes (5-2 Notes). Magnitude = a measure of an earthquake’s strength Based on seismic waves.
Measuring Earthquakes. Seismograph Is an instrument used to detect and record seismic waves.
1. What do seismologists use to determine when an earthquake started? A seismogram 2. How is the intensity of an earthquake determined? By the amount.
Earthquakes. What are earthquakes? Vibration in the ground that result from movement along faults. Fault = a break in Earth’s lithosphere where one block.
CHAPTER 12 EARTHQUAKES MOVEMENTS OF THE EARTH THAT ARE CAUSED BY A SUDDEN RELEASE OF ENERGY WHEN ROCKS MOVE ALONG A FAULT.
Topic: Earthquake Measurement PSSA: A / S8.D.1.1.
Vocabulary 6/28/2016Chapter 19: Earthquakes1 SeismometerSeismographMagnitude Richter Scale Moment Magnitude Scale Modified Mercalli Scale.
Students know how to identify transverse and longitudinal waves in mechanical media such as springs, ropes, and the Earth (seismic waves).
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.
Chapter 12 Earthquakes.
Unit 4 Lesson 6 Measuring Earthquake Waves
Unit 4 Lesson 6 Measuring Earthquake Waves
EARTHQUAKES Part II .
Unit 4 Lesson 6 Measuring Earthquake Waves
Earthquakes.
Earthquake Measurement 7-2
Ch.5, Sec.2 - Earthquake Measurement
Chapter 8 Section 2.
Earthquake Measurement
Chapter 12 Study Notes Earthquakes.
Earthquakes DYNAMIC EARTH.
8.2 – Measuring Earthquakes – Part II
Measuring Earthquakes
DO NOW Pick up notes..
Earthquake Measurement
Using Distances to known Earthquake epicenters, create
Earthquakes Vibration of Earth produced by the rapid release of energy.
Chapter 12-2 Studying Earthquakes.
Key Terms 5.2.
Do we have to take notes? Yes!.
Unit 4 Lesson 6 Measuring Earthquake Waves
Handout 3 (2-3) Recording Earthquakes
Locating Earthquakes Chapter F5
Chapter 12 - Section 2 Measuring Earthquakes
Chapter 12 - Section 2 Measuring Earthquakes
Unit 4 Lesson 6 Measuring Earthquake Waves
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:

Section 6.5: Studying Earthquakes Preview Objectives Studying Earthquakes Recording Earthquakes Locating an Earthquake S-P-Time Method: Finding an Epicenter Earthquake Measurement

Objectives Describe the instrument used to measure and record earthquakes. Summarize the method scientists use to locate an epicenter. Describe the scales used to measure the magnitude and intensity of earthquakes.

Studying Earthquakes The study of earthquakes and seismic waves is called seismology. Seismologists use special sensing equipment to record, locate, and measure earthquakes.

Recording Earthquakes seismograph an instrument that records vibrations in the ground seismogram a tracing of earthquake motion that is recorded by a seismograph Seismographs record three types of ground motion-vertical, east-west, and north-south. Because they are the fastest, P waves are the first seismic waves to be recorded by a seismograph. S waves are the second seismic waves to be recorded, and surface waves are the last to be recorded by a seismograph.

Locating an Earthquake To determine the distance to an epicenter, scientists consult a lag-time graph and analyze the arrival times of the P waves and S waves. The start time of an earthquake can also be determined by this graph. Scientists use computers to perform complex triangulations based on information from several seismograph stations. These calculations help determine the location of an earthquake. Before computers were widely available, scientists used simpler, less precise calculations together with maps to locate earthquakes.

S-P-Time Method: Finding an Epicenter

Earthquake Measurement Magnitude magnitude a measure of the strength of an earthquake Magnitude is determined by measuring the amount of ground motion caused by an earthquake. While the Richter scale was widely used for most of the 20th century, scientists now prefer to use the moment magnitude scale. Moment magnitude is a measure of earthquake strength based on the size of the area of the fault that moves, the average distance that the fault blocks move, and the rigidity of the rocks in the fault zone.

Earthquake Measurement, continued Quick Quiz What is the difference between the Richter scale and the moment magnitude scale? Moment magnitude is more accurate for larger earthquakes than the Richter scale is. Moment magnitude is directly related to rock properties and so is more closely related to the cause of the earthquake than the Richter scale is.

Earthquake Measurement Intensity intensity the amount of damage caused by an earthquake Before the development of magnitude scales, the size of an earthquake was described in terms of the earthquake’s effects. The modified Mercalli scale expresses intensity in Roman numerals from I to XII and provides a description of the effects of each earthquake intensity.