2.3 Notes: Earthquake Damage Can Be Reduced
|
|
- Randolf Hoover
- 6 years ago
- Views:
Transcription
1 2.3 Notes: Earthquake Damage Can Be Reduced Earthquakes can cause severe damage and loss of life Each year, there is about one earthquake with a magnitude of or higher-this is an extremely earthquake. 8.0 earthquakes (or bigger) can destroy all buildings near their epicenters and cause huge loss of. 9.0 Earthquake in Japan in 2011 lasted 6 minutes and killed people. Most deaths from earthquakes are caused by collapsing buildings and, not by the shaking of the ground. Earthquake magnitude The most powerful earthquakes can release more energy than weak earthquakes combined! Earthquake magnitude is described using a number scale from 0-10 (no real maximum possible value). The first number scale was developed in the 1930 s by Charles Richter and. o Describes an earthquake s magnitude based on how fast the ground moves at a seismic. Most scientists today prefer the moment magnitude scale (MMS), which measures the total amount of released by an earthquake. Both the Richter Scale and the MMS increase by 32 times with each whole number increase. o A magnitude 5 earthquake is times stronger than a magnitude 4 earthquake. o A magnitude earthquake is 1000 times stronger than a magnitude 4 earthquake! The MMS is more accurate and also allows scientists to measure the strength of earthquakes that occurred before seismographs were invented by measuring the strengths of rocks and length they moved along a fault. Damage from earthquakes Earthquakes can crack roads, buildings, damns, and any other structures that exist on top of a. Earthquakes can also raise, lower, or tilt the surface. An is a smaller earthquake that follows a more powerful earthquake in the same area. Sometimes aftershocks cause buildings that were weakened by an earthquake to collapse. Fire caused by earthquakes can cause significant damage. In the 1906 San Francisco Earthquake, fire caused more than of the damage. are a common side effect of earthquakes as soil is shaken loose. Liquefaction is a process in which shaking of the ground causes soil to temporarily act like a. Liquefaction can cause structures to down into the soil or flow away with it. Damage from tsunamis A tsunami is a water triggered by an earthquake, volcanic eruption, or landslide. Tsunamis can be taller than a building! A tsunami may be a single wave but can also be several waves that have different heights and arrive apart. In deep water, tsunamis can travel at km/hr (430 mi/hr)! p. 19
2 As tsunamis approach coastlines, they slow down and grow in. In 2004, an earthquake off the coast of Sumatra caused a tsunami. o people died. Scientists work to monitor and predict earthquakes We cannot predict the day or even that an earthquake will occur. Sometimes there are and sometimes there are none at all. Long term predictions can be generated. o Example: An area might have a chance of being hit by an earthquake with magnitude or higher in the next years. Scientists around the world work constantly to try to better predict earthquakes, by observing the following things: o Tilts or changes in the of the ground o Slow movements or stretching in rock o The development of small in the ground Structures can be designed to resist earthquake damage Review For safety during an earthquake, the best place to be is and away from any buildings. Scientists make of areas that have many earthquakes. Planners use these maps to develop for building in these areas. For small buildings (like houses): o Should be firmly fastened to the o Should have walls For large buildings (like skyscrapers): o Base : flexible material between building and foundation o Cross braces: X shaped braces added to a building to help a building keep its. 1. The moment magnitude scale is based on the A. Amount of ground movement at a seismic station B. Amount of building damage caused by an earthquake C. Number of human deaths caused by an earthquake D. Amount of energy released by an earthquake 2. One method of making a building earthquake resistant is to A. Add sand under the foundation C. Make the walls of brick B. Reduce the use of steel D. Use cross braces
3
4 2.3 Notes: Earthquake Damage Can Be Reduced Earthquakes can cause severe damage and loss of life Each year, there is about one earthquake with a magnitude of 8 or higher-this is an extremely powerful earthquake. 8.0 earthquakes (or bigger) can destroy all buildings near their epicenters and cause huge loss of life. 9.0 Earthquake in Japan in 2011 lasted 6 minutes and killed 18,000 people. Most deaths from earthquakes are caused by collapsing buildings and fires, not by the shaking of the ground. Earthquake magnitude The most powerful earthquakes can release more energy than 1 million weak earthquakes combined! Earthquake magnitude is described using a number scale from 0-10 (no real maximum possible value). The first number scale was developed in the 1930 s by Charles Richter and Beno Gutenberg. o Describes an earthquake s magnitude based on how fast the ground moves at a seismic station. Most scientists today prefer the moment magnitude scale (MMS), which measures the total amount of energy released by an earthquake. Both the Richter Scale and the MMS increase by 32 times with each whole number increase. o A magnitude 5 earthquake is 32 times stronger than a magnitude 4 earthquake. o A magnitude 6 earthquake is 1000 times stronger than a magnitude 4 earthquake! The MMS is more accurate and also allows scientists to measure the strength of earthquakes that occurred before seismographs were invented by measuring the strengths of rocks and length they moved along a fault. Damage from earthquakes Earthquakes can crack roads, buildings, damns, and any other structures that exist on top of a fault. Earthquakes can also raise, lower, or tilt the ground surface. An aftershock is a smaller earthquake that follows a more powerful earthquake in the same area. Sometimes aftershocks cause buildings that were weakened by an initial earthquake to collapse. Fire caused by earthquakes can cause significant damage. In the 1906 San Francisco Earthquake, fire caused more than 90% of the damage. Landslides are a common side effect of earthquakes as soil is shaken loose. Liquefaction is a process in which shaking of the ground causes soil to temporarily act like a liquid. Liquefaction can cause structures to sink down into the soil or flow away with it. Damage from tsunamis A tsunami is a water wave triggered by an earthquake, volcanic eruption, or landslide. Tsunamis can be taller than a 20-story building! A tsunami may be a single wave but can also be several waves that have different heights and arrive hours apart. In deep water, tsunamis can travel at 700 km/hr (430 mi/hr)! As tsunamis approach coastlines, they slow down and grow in height. p. 19
5 In 2004, an earthquake off the coast of Sumatra caused a tsunami. o 280,000 people died. Scientists work to monitor and predict earthquakes We cannot predict the day or even year that an earthquake will occur. Sometimes there are signs and sometimes there are none at all. Long term predictions can be generated. o Example: An area might have a 60% chance of being hit by an earthquake with magnitude 7 or higher in the next 25 years. Scientists around the world work constantly to try to better predict earthquakes, by observing the following things: o Tilts or changes in the elevation of the ground o Slow movements or stretching in rock o The development of small cracks in the ground Structures can be designed to resist earthquake damage Review For safety during an earthquake, the best place to be is outside and away from any buildings. Scientists make maps of areas that have many earthquakes. Planners use these maps to develop rules for building in these areas. For small buildings (like houses): o Should be firmly fastened to the foundation o Should have strong walls For large buildings (like skyscrapers): o Base isolators: flexible material between building and foundation o Cross braces: X shaped braces added to a building to help a building keep its shape. 1. The moment magnitude scale is based on the A. Amount of ground movement at a seismic station B. Amount of building damage caused by an earthquake C. Number of human deaths caused by an earthquake D. Amount of energy released by an earthquake 2. One method of making a building earthquake resistant is to A. Add sand under the foundation C. Make the walls of brick B. Reduce the use of steel D. Use cross braces
Forces in Earth s Crust
Name Date Class Earthquakes Section Summary Forces in Earth s Crust Guide for Reading How does stress in the crust change Earth s surface? Where are faults usually found, and why do they form? What land
More informationEarthquakes & Volcanoes
Earthquakes & Volcanoes Geology - the study of solid Earth, the rocks of which it is composed, and the processes by which they change geo = Earth; ology = study of Earth s Layers Plate Tectonics - the
More informationAn entire branch of Earth science, called, is devoted to the study of earthquakes.
Lesson One Essential Question Where do earthquakes take place? What causes earthquakes? What are three different types of faults that occur at plate boundaries? How does energy from earthquakes travels
More informationEarthquake Hazards. Tsunami
Earthquake Hazards Tsunami Review: What is an earthquake? Earthquake is the vibration (shaking) and/or displacement of the ground produced by the sudden release of energy. The point inside the Earth where
More informationAn Earthquake is a rapid vibration or shaking of the Earth s crust created by a release in energy from sudden movement of a part of a plate along a
An Earthquake is a rapid vibration or shaking of the Earth s crust created by a release in energy from sudden movement of a part of a plate along a fault. Energy released radiates in all directions from
More informationEarthquake Hazards. Tsunami
Earthquake Hazards Tsunami Measuring Earthquakes Two measurements that describe the power or strength of an earthquake are: Intensity a measure of the degree of earthquake shaking at a given locale based
More informationEarthquake Hazards. Tsunami
Earthquake Hazards Tsunami Review: What is an earthquake? Earthquake is the vibration (shaking) and/or displacement of the ground produced by the sudden release of energy. The point inside the Earth where
More informationEarthquakes.
Earthquakes http://thismodernworld.com/comic-archive Elastic rebound http://projects.crustal.ucsb.edu/understanding/elastic/rebound.html Elastic rebound Rocks store energy elastically When stored stress
More informationWhat causes an earthquake? Giant snakes, turtles, catfish, and spiders?
What causes an earthquake? Giant snakes, turtles, catfish, and spiders? What causes an earthquake? The movement of Earth s plates creates enormous forces that squeeze or pull the rock in the crust as if
More informationEarthquakes Modified
Plate Tectonics Earthquakes Modified Recall that the earth s crust is broken into large pieces called. These slowly moving plates each other, each other, or from each other. This causes much on the rocks.
More informationEarthquakes and Earth s Interior
- What are Earthquakes? Earthquakes and Earth s Interior - The shaking or trembling caused by the sudden release of energy - Usually associated with faulting or breaking of rocks - Continuing adjustment
More informationName Date Class. radiate in all directions, carrying some of the. of plate boundaries have different usual patterns of.
Chapter Outline Earthquakes CHAPTER 6 Lesson 1: Earthquakes and Plate Boundaries A. What is an earthquake? 1. A(n) is the rupture and sudden movement of rocks along a fault. A fault is a fracture surface
More information11/30/16 EARTHQUAKES ELASTIC LIMIT FAULT FORCE AND PLATES WHAT DO YOU NOTICE?
ELASTIC LIMIT EARTHQUAKES Bend sitck but do not break it. What do you notice? No bend until it breaks. Describe the energy and forces at work. (Kinetic, potential etc) 8 TH GRADE FAULT FORCE AND PLATES
More informationEarthquakes and Seismic Waves Lesson 4 2
Earthquakes and Seismic Waves Lesson 4 2 Apr 15 8:52 PM What are seismic waves? How are earthquakes measured? How is an earthquake located? Apr 15 8:54 PM 1 What are seismic waves An earthquake is the
More informationEarthquake Notes. Earthquakes occur all the time all over the world, both along plate edges and along faults.
Earthquake Notes Name: Date: Where Do Earthquakes Happen? Earthquakes occur all the time all over the world, both along plate edges and along faults. Most earthquakes occur along the edge of the oceanic
More informationHow to Use This Presentation
How to Use This Presentation To View the presentation as a slideshow with effects select View on the menu bar and click on Slide Show. To advance through the presentation, click the right-arrow key or
More informationAIM: What are the features of Earthquakes and where are they located? Do Now: What are some words that are associated with earthquakes?
Notepack # 11 November 8, 201 AIM: What are the features of Earthquakes and where are they located? Do Now: What are some words that are associated with earthquakes? What are Earthquakes? The shaking or
More informationSection Forces Within Earth. 8 th Grade Earth & Space Science - Class Notes
Section 19.1 - Forces Within Earth 8 th Grade Earth & Space Science - Class Notes Stress and Strain Stress - is the total force acting on crustal rocks per unit of area (cause) Strain deformation of materials
More informationEarthquakes and Earth s Chapter. Interior
Earthquakes and Earth s Chapter Interior 8.1 What Is an Earthquake? An earthquake is the vibration of Earth produced by the rapid release of energy Focus and Epicenter Focus is the point within Earth
More informationWhat is an Earthquake?
Earthquakes What is an Earthquake? Earthquake - sometimes violent shaking of ground caused by movement of Earth s tectonic plates; creates seismic waves Often followed by smaller earthquakes (aftershocks);
More informationSection 19.1: Forces Within Earth Section 19.2: Seismic Waves and Earth s Interior Section 19.3: Measuring and Locating.
CH Earthquakes Section 19.1: Forces Within Earth Section 19.2: Seismic Waves and Earth s Interior Section 19.3: Measuring and Locating Earthquakes Section 19.4: Earthquakes and Society Section 19.1 Forces
More informationEarthquakes. Building Earth s Surface, Part 2. Science 330 Summer What is an earthquake?
Earthquakes Building Earth s Surface, Part 2 Science 330 Summer 2005 What is an earthquake? An earthquake is the vibration of Earth produced by the rapid release of energy Energy released radiates in all
More information22.5 Earthquakes. The tsunami triggered by the 2004 Sumatra earthquake caused extensive damage to coastal areas in Southeast Asia.
The tsunami triggered by the 2004 Sumatra earthquake caused extensive damage to coastal areas in Southeast Asia. An earthquake is a movement of Earth s lithosphere that occurs when rocks in the lithosphere
More informationI. What are Earthquakes?
I. What are Earthquakes? A. There is more to earthquakes than just the shaking of the ground. An entire branch of Earth science, called seismology, is devoted to the study of earthquakes. B. Earthquakes
More informationEarthquakes. Chapter Test A. Multiple Choice. Write the letter of the correct answer on the line at the left.
Earthquakes Chapter Test A Multiple Choice Write the letter of the correct answer on the line at the left. 1. Stress that pushes a mass of rock in two opposite directions is called a. shearing. b. tension.
More informationDangerous tsunami threat off U.S. West Coast
Earthquakes Ch. 12 Dangerous tsunami threat off U.S. West Coast Earthquakes What is an Earthquake? It s the shaking and trembling of the Earth s crust due to plate movement. The plates move, rocks along
More informationLAB 9: Earthquakes & Seismic Activity
LAB 9: Earthquakes & Seismic Activity Objectives Identify P, S, and surface waves on a simple seismogram Locate the epicenter of an earthquake using seismograms and travel times curves Describe how the
More informationOnce you have opened the website with the link provided choose a force: Earthquakes
Name: Once you have opened the website with the link provided choose a force: Earthquakes When do earthquakes happen? On the upper left menu, choose number 1. Read What is an Earthquake? Earthquakes happen
More informationPrentice Hall EARTH SCIENCE
Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 8 Earthquakes and Earth s Interior 8.1 What Is an Earthquake? Earthquakes An earthquake is the vibration of Earth produced by the rapid release of energy
More informationEarthquakes and Earthquake Hazards Earth - Chapter 11 Stan Hatfield Southwestern Illinois College
Earthquakes and Earthquake Hazards Earth - Chapter 11 Stan Hatfield Southwestern Illinois College What Is an Earthquake? An earthquake is the vibration of Earth, produced by the rapid release of energy.
More informationSlide 1. Earth Science. Chapter 5 Earthquakes
Slide 1 Earth Science Chapter 5 Earthquakes Slide 2 Forces in Earth's Crust A force that acts on rock to change its shape or volume is stress 3 types of stress acting on rock layers Tension pulls on the
More informationEarthquakes 11/14/2014. Earthquakes Occur at All Boundaries. Earthquakes. Key Aspects of an Earthquake. Epicenter. Focus
Earthquakes Earthquakes Caused by friction and movement between Earth s tectonic plates A release of force Often caused by a catch between two plates As plates slide by, they stick to each other When the
More informationChapter 13 Earthquakes and Earth s Interior
Chapter 13 Earthquakes and Earth s Interior The crust of the Earth is made up of floating tectonic plates- huge continent-sized chunks of solid rock floating on molten rock. Rock masses along the boundaries
More informationScience Starter. Describe in your own words what an Earthquake is and what causes it. Answer The MSL
Science Starter Describe in your own words what an Earthquake is and what causes it. Answer The MSL WHAT IS AN EARTHQUAKE AND HOW DO WE MEASURE THEM? Chapter 8, Section 8.1 & 8.2 Looking Back Deserts Wind-shaped
More informationEarthquakes. Earthquakes and Plate Tectonics. Earthquakes and Plate Tectonics. Chapter 6 Modern Earth Science. Modern Earth Science. Section 6.
Earthquakes Chapter 6 Modern Earth Science Earthquakes and Plate Tectonics Section 6.1 Modern Earth Science Earthquakes and Plate Tectonics Earthquakes are the result of stresses in Earth s s lithosphere.
More informationEarthquakes Chapter 19
Earthquakes Chapter 19 Does not contain complete lecture notes. What is an earthquake An earthquake is the vibration of Earth produced by the rapid release of energy Energy released radiates in all directions
More informationI. Locations of Earthquakes. Announcements. Earthquakes Ch. 5. video Northridge, California earthquake, lecture on Chapter 5 Earthquakes!
51-100-21 Environmental Geology Summer 2006 Tuesday & Thursday 6-9:20 p.m. Dr. Beyer Earthquakes Ch. 5 I. Locations of Earthquakes II. Earthquake Processes III. Effects of Earthquakes IV. Earthquake Risk
More informationon the earthquake's strength. The Richter scale is a rating of an earthquake s magnitude based on the size of the
Earthquakes and Seismic Waves An earthquake is the shaking and trembling that results from the movement of rock beneath Earth's surface. The point beneath Earth s surface where rock under stress breaks
More information4 Deforming the Earth s Crust
CHAPTER 7 4 Deforming the Earth s Crust SECTION Plate Tectonics BEFORE YOU READ After you read this section, you should be able to answer these questions: What happens when rock is placed under stress?
More informationDirected Reading. Section: How and Where Earthquakes Happen WHY EARTHQUAKES HAPPEN. Skills Worksheet. 1. Define earthquake.
Skills Worksheet Directed Reading Section: How and Where Earthquakes Happen 1. Define earthquake. 2. When do earthquakes usually occur? 3. What is a fault? WHY EARTHQUAKES HAPPEN 4. Rocks along both sides
More information20.1 Earthquakes. Chapter 20 EARTHQUAKES AND VOLCANOES. Earthquakes and plate boundaries 500 UNIT 6 EARTH S STRUCTURE
Chapter 20 EARTHQUAKES AND VOLCANOES 20.1 Earthquakes In Chapter 19, you read about the San Andreas Fault, which lies along the California coast (Figure 20.1). This fault passes right through San Francisco
More informationWarm-up #15. How does magma move throughout the mantle? What is another example of this movement in nature?
Warm-up #15 How does magma move throughout the mantle? What is another example of this movement in nature? Earth s Structure Lithosphere = crust & upper mantle; tectonic plates Asthenosphere = lower mantle
More informationWe have previously looked at artificial seismograms such as this one here.
We have previously looked at artificial seismograms such as this one here. S P A realistic Seismic Record Each vertical line = 1 minute Each horizontal line = 15 minutes Seismic station PMM is in Parkfield,
More informationForces in the Earth s crust
EARTHQUAKES Forces in the Earth s crust How does stress in the crust change Earth s surface? Where are faults usually found, and why do they form? What land features result from the forces of plate movement?
More informationRapid Changes on Earth: Earthquakes, Volcanoes, Landslides. Chapter 6 Study Guide
Rapid Changes on Earth: Earthquakes, Volcanoes, Landslides Chapter 6 Study Guide Magma is 1. The point underground where an earthquake starts. 2. Molten rock beneath the Earth s surface. 3. Molten rock
More informationEarthquakes = shaking of Earth because of a rapid release of energy
There are more than 30,000 earthquakes worldwide each year! Earthquakes = shaking of Earth because of a rapid release of energy usually because of movement of tectonic plates Most earthquakes last for
More informationEarthquakes How and Where Earthquakes Occur
Earthquakes How and Where Earthquakes Occur PPT Modified from Troy HS Is there such thing as earthquake weather? Absolutely NOT!!! Geologists believe that there is no connection between weather and earthquakes.
More informationModule 2, Investigation 1: Earthquake Hazards
Module 2, Investigation 1: Earthquake Hazards Introduction Welcome! In the last module, you assumed the role of a volcanologist and learned how volcanoes are described and monitored. You will now assume
More informationPlate Tectonics IDEA THAT EARTH S SURFACE IS BROKEN INTO PLATES THAT MOVE AROUND. Fault = fracture in the crust where the movement has occurred
Warm-up #14 A mountain range found 100 meters above sea level is measured to be 1,000 meters high from its tallest peak. From the top, the first 500 meters are incredibly steep. After this point, the mountain
More informationSeismic Waves. 1. Seismic Deformation
Types of Waves 1. Seismic Deformation Seismic Waves When an earthquake fault ruptures, it causes two types of deformation: static; and dynamic. Static deformation is the permanent displacement of the ground
More informationChapt pt 15 er EARTHQUAKES! BFRB P 215 ages -226
Chapter 15 EARTHQUAKES! BFRB Pages 215-226226 Earthquake causes An earthquake is the shaking of the Earth s crust caused by a release of energy The movement of the Earth s plates causes most earthquakes
More informationThree Fs of earthquakes: forces, faults, and friction. Slow accumulation and rapid release of elastic energy.
Earthquake Machine Stick-slip: Elastic Rebound Theory Jerky motions on faults produce EQs Three Fs of earthquakes: forces, faults, and friction. Slow accumulation and rapid release of elastic energy. Three
More informationUGRC 144 Science and Technology in Our Lives/Geohazards
UGRC 144 Science and Technology in Our Lives/Geohazards Session 3 Understanding Earthquakes and Earthquake Hazards Lecturer: Dr. Patrick Asamoah Sakyi Department of Earth Science, UG Contact Information:
More informationEarthquakes Earth, 9th edition, Chapter 11 Key Concepts What is an earthquake? Earthquake focus and epicenter What is an earthquake?
1 2 3 4 5 6 7 8 9 10 Earthquakes Earth, 9 th edition, Chapter 11 Key Concepts Earthquake basics. "" and locating earthquakes.. Destruction resulting from earthquakes. Predicting earthquakes. Earthquakes
More informationEarthquakes. Earthquake Magnitudes 10/1/2013. Environmental Geology Chapter 8 Earthquakes and Related Phenomena
Environmental Geology Chapter 8 Earthquakes and Related Phenomena Fall 2013 Northridge 1994 Kobe 1995 Mexico City 1985 China 2008 Earthquakes Earthquake Magnitudes Earthquake Magnitudes Richter Magnitude
More informationNatural Disasters Spring, LECTURE #8: Earthquake Disasters: Monitoring & Mitigation. Date: 1 Feb 2018 (lecturer: Dr.
GEOL 0820 Ramsey Natural Disasters Spring, 2018 LECTURE #8: Earthquake Disasters: Monitoring & Mitigation Date: 1 Feb 2018 (lecturer: Dr. Shawn Wright) I. Exam I - Reminder Feb 6 th next class details:
More informationEQ Monitoring and Hazards NOTES.notebook. January 07, P-wave. S-wave. surface waves. distance
Earthquake Monitoring and Hazards Reading a Seismogram General guidelines: P-wave First disruption of trace = Second disruption of trace = surface waves Largest disruption of trace = Not the distance to
More informationPlate Tectonics and Earth s Structure
Plate Tectonics and Earth s Structure Chapter Eight: Plate Tectonics Chapter Nine: Earthquakes Chapter Ten: Volcanoes Chapter Nine: Earthquakes 9.1 What is an Earthquake? 9.2 Seismic Waves 9.3 Measuring
More informationRead & Learn Earthquakes & Faults
Read Earthquakes & Faults Read the provided article. Use the information in the reading to answer the questions on the task cards on your answer sheet. Make sure your answers are in the correct spot on
More informationUnit 9 (packet #2): Volcanoes and Earthquakes
Unit 9 (packet #2): Volcanoes and Earthquakes 13. Earthquakes are one of the most destructive natural forces. I can a. Explain what an earthquake is, where they occur and why they occur. b. Describe the
More informationEarthquakes. Photo credit: USGS
Earthquakes Earthquakes Photo credit: USGS Pancaked Building - 1985 Mexico City Earthquakes don t kill people - buildings do! An earthquake is the motion or trembling of the ground produced by sudden displacement
More informationThe Structure of the Earth
The Structure of the Earth Structure of the Earth The Crust Outer layer of solid rock Quite thin (10km 60 km) Contains the earths plates The Mantle Hot, soft rock (4000 o C) Made up of molten rock (magma)
More informationMoho (Mohorovicic discontinuity) - boundary between crust and mantle
Earth Layers Dynamic Crust Unit Notes Continental crust is thicker than oceanic crust Continental Crust Thicker Less Dense Made of Granite Oceanic Crust Thinner More Dense Made of Basalt Moho (Mohorovicic
More informationUNIT - 7 EARTHQUAKES
UNIT - 7 EARTHQUAKES WHAT IS AN EARTHQUAKE An earthquake is a sudden motion or trembling of the Earth caused by the abrupt release of energy that is stored in rocks. Modern geologists know that most earthquakes
More informationIdentifying the causes and effects of earthquakes
Science 3 Physical Earth and Space Life LESSON 57 Identifying the causes and effects of earthquakes Lesson Preparation Program Materials Child s Booklet E Exploring the Earth s Structure (pp. 12 13) Optional:
More informationEarthquake Investigation
Exploration A Earthquake Investigation 1. Obtain a piece of plastic putty and knead it into a rectangular shape. 2. Push the ends of the putty toward the middle. Draw and describe what it looks like below.
More informationLesson 4: Earthquakes and Moving Plates
Our Changing Earth -> 4: Earthquakes and Moving lates Getting Started Lesson 4: Earthquakes and Moving lates Earthquakes happen quickly, but the pressures that build up to cause them happen over a long
More informationWhat is an earthquake?
Earthquakes Definitions Seismology The study of earthquakes dates back almost 2000 years to the Chinese Fault A crack in the Earth along which movement or sliding occurs What is an earthquake? Focus vs.
More informationEarthquakes. Beyond the Book. FOCUS Book
FOCUS Book Model how liquefaction during an earthquake changes Earth s surface and affects buildings. Put sand in a large plastic container. Mix enough water into the sand to make the ground feel firm.
More informationEarthquakes.
Earthquakes http://quake.usgs.gov/recenteqs/latestfault.htm An earthquake is a sudden motion or shaking of the Earth's crust, caused by the abrupt release of stored energy in the rocks beneath the surface.
More informationChapter 6: Earthquakes
Section 1 (Forces in Earth s Crust) Chapter 6: Earthquakes 8 th Grade Stress a that acts on rock to change its shape or volume Under limited stress, rock layers can bend and stretch, but return to their
More informationPage 1. Name:
Name: 6185-1 - Page 1 1) Which statement correctly compares seismic P-waves with seismic S-waves? A) P-waves travel faster than S-waves and pass through Earth's liquid zones. B) P-waves travel slower than
More informationChapter 4 Earthquakes and Tsunamis
Geology of the Hawaiian Islands Class 21 30 March 2004 100 100 100 96 A B C D F Exam Scores 95 94 94 90 85 83 83 83 Mean 72 67 61 59 59 55 54 41 Mean = 78.5 Median = 83 Any Questions? Chapter 4 Earthquakes
More informationChapter 4 Earthquakes and Tsunamis. Geology of the Hawaiian Islands. Any Questions? Class March Mean = 78.
Geology of the Hawaiian Islands Class 21 30 March 2004 Any Questions? 100 100 100 96 A B C D F Exam Scores 95 94 94 90 85 83 83 83 Mean 72 67 61 59 59 55 54 41 Mean = 78.5 Median = 83 Chapter 4 Earthquakes
More informationEarthquakes An introduction to earthquake monitoring techniques
Earthquakes An introduction to earthquake monitoring techniques TEACHER S COPY Aims To understand what an earthquake is and where they occur To gain an insight into how earthquakes are recorded and how
More informationA physical feature of the Earth s surface
Earth s Landforms A physical feature of the Earth s surface A physical feature of the Earth s surface LANDFORM Highest of Earth s physical features Highest of Earth s physical features MOUNTAIN Low area
More informationInternal Layers of the Earth
Lecture #4 notes Geology 3950, Spring 2006; CR Stern Seismic waves, earthquake magnitudes and location, and internal earth structure (pages 28-95 in the 4 th edition and 28-32 and 50-106 in the 5 th edition)
More informationThe Size of an Earthquake. Intensity of Shaking (Robert Mallet, 1857) Calculation of Earthquake Magnitude (Charles Richter, 1935)
The Size of an Earthquake Intensity of Shaking (Robert Mallet, 1857) Calculation of Earthquake Magnitude (Charles Richter, 1935) In 1857, Robert Mallet produced isoseismal lines based on quantified damage
More informationSIMULATED SEISMOGRAMS
SIMULATED SEISMOGRAMS Great Falls, Montana I I I I I I I I I I I I I I I I I I I I I I I I I 8:03 8:04 8:05 8:06 8:07 P-wave arrival S-wave arrival Little Rock, Arkansas I I I I I I I I I I I I I I I I
More informationA Violent Pulse: Earthquakes. Lecture #2
A Violent Pulse: Earthquakes Lecture #2 Earthquakes Are Always Happening ~ 1,000,000 / yr Most are small o Detected only by instruments Large EQ ~ 20 / yr cause extensive damage ~ 1 catastrophic EQ / year
More informationPrevention Tsunami wall 10m high (breached by the tsunami due to land level falling by 3m)
Plate margin Plates Causes Sendai, Japan Convergent plate margin Pacific and Eurasian Plates Convergent plate margin Sima (Pacific plate) moves towards the sial (Eurasian plate) Sima (Pacific plate) is
More informationEarthquakes. Copyright 2006 InstructorWeb
Earthquakes Earthquakes cause the earth to shake! Earthquakes are caused by a fault line under the earth's crust. You do not have to be right under a fault line to feel an earthquake. You could be miles
More informationTopic 5: The Dynamic Crust (workbook p ) Evidence that Earth s crust has shifted and changed in both the past and the present is shown by:
Topic 5: The Dynamic Crust (workbook p. 65-85) Evidence that Earth s crust has shifted and changed in both the past and the present is shown by: --sedimentary horizontal rock layers (strata) are found
More informationSEISMOLOGY. - The study of earthquakes waves and how they move through the body and around the surface of the earth.
EARTHQUAKES SEISMOLOGY - The study of earthquakes waves and how they move through the body and around the surface of the earth. Seismic Waves - vibrations generated in the earths interior that carry energy
More informationFigure Diagram of earth movements produced by (a) P-waves and (b) S-waves.
Geology 101 Name(s): Lab 10: Earthquakes When the stresses in a rock (which may or may not already be faulted) exceed the tensile strength of the rock, the rock ruptures at a point called the focus or
More informationA. rift valley B. deep trench C. volcanic cone D. uplifted mountain. A. a volcanic island arc B. a large watershed area
DC Practice Test Dynamic Crust PRCTICE TEST Zimm's Earth Science 2013 1. Which feature would most likely be forming at converging continental tectonic plate boundaries?. rift valley. deep trench C.
More informationEarthquakes. Pt Reyes Station 1906
Earthquakes Pt Reyes Station 1906 Earthquakes Ground shaking caused by the sudden release of accumulated strain by an abrupt shift of rock along a fracture in the earth. You Live in Earthquake Country
More informationLecture Outline Wednesday-Monday April 18 23, 2018
Lecture Outline Wednesday-Monday April 18 23, 2018 Questions? Lecture Final Exam Lecture Section 1 Friday May 4, 8:00-10:00am Lecture Section 2 Friday May 4, 3:10-5:10 pm Final Exam is 70% new material
More informationObjectives. Vocabulary
Forces Within Earth Objectives Define stress and strain as they apply to rocks. Distinguish among the three types of faults. Contrast three types of seismic waves. Vocabulary stress strain fault primary
More informationVIDEO The 2011 Japanese Earthquake and Tsunami
VIDEO The 2011 Japanese Earthquake and Tsunami Why was it so large and devastating? Why so short a warning? Why did tsunami precautions fail? What happened elsewhere? The Loma Prieta Earthquake (1989)
More informationSeismic vulnerability in Latinamerica Speaker: Rafael Osiris de León Sciences Academy of Dominican Republic.
Seismic vulnerability in Latinamerica Speaker: Rafael Osiris de León Sciences Academy of Dominican Republic. IANAS GENERAL ASSEMBLY Punta Cana, 16-20 July, 2013 TECTONIC PLATES AND EARTHQUAKES Pacific
More informationCONTENT. A. Changes in the Crust Facts Changes Construction and Destruction. B. Continental Drift What is it? Evidence
Name Earth Science Date Period TOPIC THE DYNAMIC EARTH CONTENT A. Changes in the Crust Facts Changes Construction and Destruction B. Continental Drift What is it? Evidence C. Theory of Plate Tectonics
More informationEarthquake Epicenters
TEACHER RESOURCES Inquiry Lab Earthquake Epicenters DATASHEET Teacher Notes This lab has students use three seismograms to locate the epicenter of an earthquake (covers standard 6.1.g). TIME REQUIRED One
More informationwater erosion lithosphere Describe the process of erosion and deposition. chemical weathering Dissolving limestone is an example of.
At one time, there was one large island off the coast of Mississippi and now it is two separate islands. What caused the island to be split into two? water erosion The crust and the top part of the upper
More informationEarthquakes. Lesson 9
Earthquakes Lesson 9 Scientists believe that convection currents inside the Earth cause tectonic plates, (crustal plates) to separate, collide, or slip past each other. Each type of plate movement creates
More informationImportant Concepts. Earthquake hazards can be categorized as:
Lecture 1 Page 1 Important Concepts Monday, August 17, 2009 1:05 PM Earthquake Engineering is a branch of Civil Engineering that requires expertise in geology, seismology, civil engineering and risk assessment.
More informationModule 7: Plate Tectonics and Earth's Structure Topic 4 Content : Earthquakes Presentation Notes. Earthquakes
Earthquakes 1 Topic 4 Content: Earthquakes Presentation Notes Earthquakes are vibrations within the Earth produced by the rapid release of energy from rocks that break under extreme stress. Earthquakes
More informationChapter 11: Earthquakes. Grade 6 Earth Science Mr. Norton
Chapter 11: Earthquakes Grade 6 Earth Science Mr. Norton Table of Contents Chapter 10: Earthquakes Section 1: Forces Inside Earth Section 2: Features of Earthquakes Section 3: People and Earthquakes Chapter
More informationEarthquakes!! Be sure to fill in your notes sheet as you go through the power point!
Earthquakes!! Be sure to fill in your notes sheet as you go through the power point! Plate Boundary Review Click on the link below to try some plate boundary movement simulations. The link will take you
More informationFigure 2-1. Diagram of earth movements produced by (a) P-waves and (b) S-waves.
Geology 102, Winter 2006 Name(s): Lab 2: Earthquakes When the stresses in a rock (which may or may not already be faulted) exceed the tensile strength of the rock, the rock ruptures at a point called the
More information