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Waves - compcolts
Waves - compcolts

... • You see or hear a mixture of waves of many different frequencies or amplitudes. • Interference happens when 2 or more waves mix together. Some can be useful and some dangerous. • Ex. radio and TV use the interference of 2 waves to carry music and video. • Ex. water waves can add up to make one gig ...
ch 3 PowerPoint
ch 3 PowerPoint

... waves- shear waves- slower than primary- travel like a vibration through jello- move particles up and down  S waves are the second-fastest seismic waves ...
Finding the epicenter of an earthquake Background Information
Finding the epicenter of an earthquake Background Information

... Background Information: Movement within the earth along a fault or between plates is the cause of shock waves to spread out in all directions. The point at which the movement occurs is called the focus. Above the focus, on the surface of the earth is the epicenter. There are two distinct types of sh ...
Seismic Waves and Earth`s Interior PPT Name
Seismic Waves and Earth`s Interior PPT Name

... The energy of earthquakes moves away from the focus in all directions. While some of the waves occur on the surface, other waves of energy move through the planet at very deep levels. The large earthquake that triggered the tsunami of 2004 sent waves of energy through much of the planet. Many earthq ...
Earthquakes Seismic Waves Day 2
Earthquakes Seismic Waves Day 2

... Earthquake: shaking of Earth’s surface due to movement of rock along a fault. This movement comes from the release of stress occurring within rocks of the tectonic plates. Focus: the location beneath Earth’s surface (~ 100 km depth) where rock that is under stress breaks; earthquake (P- & S-wave) or ...
Unit 3: Earthquakes Intro Slideshow Notes
Unit 3: Earthquakes Intro Slideshow Notes

... • Can travel through solids, liquids and gases (Solids and Fluids) ...
1: How far can seismic waves carry energy released from an
1: How far can seismic waves carry energy released from an

... 1: How far can seismic waves carry energy released from an earthquake? ...
EQ Review
EQ Review

... d. the atmosphere. ______ 26. The composition of Earth’s interior affects a, how long an earthquake will last. b. the speed and direction of seismic waves. c. the location of an earthquake’s focus. d. the epicenter of an earthquake. ______ 27. What are the fastest body waves? a. P waves b. T waves c ...
File
File

... Body waves travel through the interior of the earth. The two types of body waves are P-waves and S-waves Surface waves – these travel through the rock that we are standing on – the crust ...
Chapter 10
Chapter 10

... is zero in a liquid. (This point will become important later). Note that S-waves travel slower than P-waves, so they will reach a seismograph after the P-wave. ...
Influence of the block-hierarchical structure of rocks on the
Influence of the block-hierarchical structure of rocks on the

... Recently the geomechanics and geophysics researchers tend to describing deformation of a rock mass as a block structure with a complex hierarchy. Under this conception, a rock mass is a structure of nested blocks different in scales [1]. By analyzing dimensions of blocks, starting from scales of cry ...
Earthquakes PowerPoint
Earthquakes PowerPoint

... travel through solids, liquids, or gases compressional wave, material movement is in the same direction as wave movement S or secondary waves slower than P waves travel through solids only shear waves - move material perpendicular to wave movement ...
Study Guide - Thomas C. Cario Middle School
Study Guide - Thomas C. Cario Middle School

... Explain (in more than one complete sentence) how seismic waves provide the indirect evidence for our understanding of the Earth’s layers. Since we cannot see the layers of the Earth, we must rely on indirect evidence. The fact that a shadow zone occurs when sensing earthquakes, tells us that there i ...
Waves Fact Sheet Anything that causes water to move can produce
Waves Fact Sheet Anything that causes water to move can produce

... motion, only the energy of the wave is passed forward, not the water. When waves near shore, they change because the water molecules can no longer complete their downward orbital motion. As the depth of the water decreases, the bottom of the wave begins to feel drag and the energy movement in the wa ...
CHAPTER 2 – Seismic waves
CHAPTER 2 – Seismic waves

... WTC_LDEO_KIM.pdf) ...
Key Concept Review (Answers to in-text “Concept Checks”) Chapter
Key Concept Review (Answers to in-text “Concept Checks”) Chapter

... expression of the relative heaviness of a substance. 4. Density is usually expressed in grams per cubic centimeter (g/cm3). 5. No one has yet sampled below Earth’s outermost layer, the crust. 6. Seismic waves form in two types: surface waves and body waves. Surface waves can sometimes be seen as an ...
File
File

...  The Earth moves during an earthquake – moving the machine as well.  The hanging weight DOES NOT MOVE!!  Attached to the weight is a pen.  As the paper moves back and forth with the machine, the pen marks the paper, recording the strength of the seismic http://www.youtube.com/watch?v=83G waves. ...
Vibrations and Waves
Vibrations and Waves

... The body of a 1275 kg car is Supported on a frame by four springs Each of which has a constant of 2 X 104 . 2 people riding in the car Have a combined mass of 153 kg. Find the period of Vibration of the car when it is Driven over a pothole on the road? T = 0.84s ...
Earthquake Notes
Earthquake Notes

... Scientists use the principle that the ______________________________________________ of a seismic wave depends on the material it travels through. How does scientist know or study the Earth’s Core? Because of the behavior of these different waves, scientists have indirect evidence for the solid inne ...
Supplementary Figure 1
Supplementary Figure 1

... displaced, there arises a force in the z direction from each of the two pairs of tensile forces T Δx and T Δy acting on the four edges of the square element. If we consider strips of the membrane of width Δx extending in the y direction then the net force for this strip is: ...
Seismographs - Keeping Track of Earthquakes
Seismographs - Keeping Track of Earthquakes

... Another method of locating an earthquake is to use the P-wave arrival-time minus origin-time (P O) interval instead of distance. This method is more common because the time can be taken directly from surface focus travel-time tables assuming an origin of 00 hours. This method, however, requires that ...
No Slide Title
No Slide Title

... Note the subtle velocity anomaly beneath the channel reflections. ...
Student Number - Department of Mechanical Engineering
Student Number - Department of Mechanical Engineering

... 2. Three children are throwing snowballs at each other. Child A throws a snowball with a horizontal velocity V0. If the snowball just passes over the head of child B and hits child C, determine (a) the value of V0, (b) the distance d. (25 points) ...
Waves
Waves

... • Because of light refraction, a person bow fishing would not aim directly at the fish. Where should they aim? ...
Structure of the Earth Study Guide with Answers
Structure of the Earth Study Guide with Answers

... SURFACE WAVES 23) How fast do body waves move through the Earth? 11 KM/SEC 24) What are the layers of the Earth from inside out? INNER CORE, OUTER CORE, MANTLE, CRUST 25) What layer of the Earth is the densest layer? INNER CORE 26) What is the difference between continental and oceanic crust? CONTIN ...
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Surface wave inversion



Inversion is the set of methods used to infer properties through physical measurements. Surface wave inversion is the method by which elastic properties, density, and thickness of layers in the subsurface are attained through analysis of surface wavedispersion. The entire inversion process requires the gathering of seismic data, the creation of dispersion curves, and finally the inference of subsurface properties.
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