Richter and Mercalli Scales

Slides:



Advertisements
Similar presentations
Features of Earthquakes
Advertisements

Measuring Earthquakes
EARTHQUAKES. DEFINITION: EARTHQUAKES DEFINITION: a violent trembling of the earth’s surface.
Seismic waves and the shadow zone.  Sudden release of energy in the Earth’s crust and creates seismic waves. Occurs naturally or human induced.
Section 19.3 – Measuring and Locating Earthquakes
Earthquakes Section 2 Section 2: Studying Earthquakes Preview Key Ideas Recording Earthquakes Locating an Earthquake S-P-Time Method: Finding an Epicenter.
Magnitude verses Intensity!
Earthquake Measurement
Ch – Measuring and Locating Earthquakes Essential Questions
Earthquakes and Seismic Waves
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,
Measuring Earthquakes. Seismograph Or seismometer, is an instrument used to detect and record earthquakes.
Earthquakes.
Earthquakes.
Earthquakes (Chapter 8)
8.2 Measuring Earthquakes
1/23/12 - Bellringer ► How might you measure an earthquake?
Earth Science Notes Measuring Earthquakes. Recall: Seismic Waves show up on a seismograph.
Inside Earth Chapter 2 Earthquakes 2.2 Earthquakes and Seismic Waves.
Earthquake Ground shaking caused by the sudden and rapid movement of one block of rock slipping past another along fractures in Earth’s crust called FAULTS.
Part 3 Seismometers and Seismograms A seismogram is the record produced by a seismometer (or seismograph).
Earthquakes. What is an Earthquake? Earthquake—the vibration of Earth produced by the rapid release of energy – Most often caused by slippage along a.
QUIZ What is Seismology?
Earthquakes and Earth’s Interior Key Points are Green.
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.
 Seismologists use two scales when classifying earthquakes. 2) Modified Mercalli Scale 1) Richter Scale.
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.
2/24/15 To-Do ► Get your 19.3 notes out and have them ready. ► We’re going to investigate possible Mercalli Intensity values for different pictures. We’ll.
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 Standard 3d. Students know why and how earthquakes occur and the scales used to measure their intensity and magnitude.
Earthquakes A sudden shaking of earth as rocks break along a fault or plate boundary A sudden shaking of earth as rocks break along a fault or plate boundary.
Earthquakes. What are earthquakes? Vibration in the ground that result from movement along faults. Fault = a break in Earth’s lithosphere where one block.
EARTH SCIENCE Geology, the Environment and the Universe
Topic: Earthquake Measurement PSSA: A / S8.D.1.1.
Vocabulary 6/28/2016Chapter 19: Earthquakes1 SeismometerSeismographMagnitude Richter Scale Moment Magnitude Scale Modified Mercalli Scale.
Earthquakes Pages C14-17.
Notes 11 Earthquake Magnitude.
What are earthquakes? Stresses in the crust cause rock to move suddenly The sudden movement causes vibrations that travel as waves inside the Earth and.
Earthquakes.
Section 6.5: Studying Earthquakes
Earthquakes Cornell Notes page 121.
Ch.5, Sec.2 - Earthquake Measurement
Chapter 8 Section 2.
Section 3: Measuring and Locating Earthquakes
Earthquake Notes.
“Measuring Earthquakes”
8.2 – Measuring Earthquakes – Part II
Measuring and Predicting Earthquakes
Measuring Earthquakes
Earthquake Measurement
Using Distances to known Earthquake epicenters, create
Earthquakes /
Earthquakes Vibration of Earth produced by the rapid release of energy.
Chapter 12-2 Studying Earthquakes.
Key Terms 5.2.
Measuring and Locating Earthquakes
EARTHQUAKES: WHY? AND HOW?
Section 3: Measuring and Locating Earthquakes
Do we have to take notes? Yes!.
EARTHQUAKES: WHY? AND HOW?
Locating Earthquakes Chapter F5
Chapter 12 - Section 2 Measuring Earthquakes
Chapter 12 - Section 2 Measuring Earthquakes
Earthquake Intensity and Magnitude
Scales used to measure earthquakes
Earthquake Measurement
Chapter 5.2 Earthquakes and seismic waves
Earthquakes Cornell Notes page 121.
Journal #72 Draw a picture of an earthquake (lithosphere) label the focus, epicenter and fault.
Presentation transcript:

Richter and Mercalli Scales An earthquake is the vibration of earth caused by a rapid release of energy. Slippage along pre-existing faults and sudden movement within a subduction zone are commonly the cause of earthquakes. Seismologist use two scales when classifying earthquakes. 1) Modified Mercalli Scale 2) Richter Scale Reference: Pages

Mercalli Scale Measures the Intensity of an earthquake on a twelve (XII) point scale. In 1902 G. Mercalli developed a fairly reliable intensity scale which assesses the damage to various types of structures at a specific location. Note that earthquake intensity is determined by several factors including: 1) Strength of earthquake 2) Distance from epicenter 3) Nature of surface materials 4) Building design

Mercalli Scale The Mercalli scale does not give a true indication of the actual strength of an earthquake because the amount of damage done to different places will largely depend on, the type of materials used and the degree of construction of buildings and structures.

Richter Scale Measures the Magnitude of an earthquake on a ten (10) point scale. In 1935, Charles Richter introduced the concept of earthquake magnitude. Richter magnitude is determined by measuring the largest amplitude (wave height) recorded on the seismogram. Largest recorded earthquake had a Richter magnitude equal to 8.6

Richter Scale Richter magnitude can be expressed in two ways: 1) wave amplitude increases ten fold (10X). 2) energy released increases thirty fold (30X). While it is correct to say that for each increase in 1 in the Richter Magnitude, there is a tenfold (10X) increase in amplitude (height) of the wave; It is incorrect to say that each increase of 1 in Richter Magnitude represents a tenfold (10X) increase in the size of the Earthquake. A better measure of the size of an earthquake is the amount of energy released by the earthquake.

Richter Scale 1) Wave amplitude increases tenfold (10X) with each increase in Richter magnitude. Each increase in 1 in Richter Magnitude represents a 10 fold increase in the wave amplitude (height). Thus, a magnitude 7 earthquake measures 10 times more amplitude than a magnitude 6 earthquake. A magnitude 8 earthquake measures 10 x 10 (or 100 times) more amplitude than a magnitude 6 earthquake. And so on.

Richter Scale 2) Energy released increases thirtyfold (30X) with each increase in Richter magnitude. Each increase in 1 in Richter Magnitude represents a 30 fold increase in the energy released (size). Thus, a magnitude 7 earthquake releases 30 times more energy than a magnitude 6 earthquake. A magnitude 8 earthquake releases 30 x 30 or 900 times more energy than a magnitude 6 earthquake. And so on ….

Richter Scale Wave Amplitude Energy Released 3 4 5 6 7 8 9

Richter and Mercalli Scales

Sample Problem In terms of magnitude, an earthquake measuring 7.2 on the Richter scale has a wave amplitude of how many times greater than an earthquake measuring 4.2 on the Richter scale? Answer: Amplitude 4.2 5.2 6.2 7.2

Sample Problem In terms of magnitude, an earthquake measuring 7.2 on the Richter scale has a wave amplitude of how many times greater than an earthquake measuring 4.2 on the Richter scale? Answer: Energy Released 4.2 5.2 6.2 7.2