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Earthquakes
Earthquakes

PHYS 342: Modern Physics
PHYS 342: Modern Physics

answer key
answer key

... The force of these movements sends shock waves in all directions and shakes the ground. Dropping a stone in a still pond will generate an outward wave similar to the type that results when two plates come into contact. The intensity of these waves depends on how deep the focus is (up to 700 km, or 4 ...
Well-seismic bandwidth and time-lapse seismic characterization: physical considerations
Well-seismic bandwidth and time-lapse seismic characterization: physical considerations

Conceptual Physics- Final Examination Review Practice
Conceptual Physics- Final Examination Review Practice

... _______19. The force of attraction between two particles due to their mass is called gravity. _______20. An example of a lever is a hammer. _______21. Any change is speed or velocity is called acceleration. _______22. An object with more mass would be more difficult to stop. _______23. Energy is mea ...
Seismology A shaky science
Seismology A shaky science

... single number to quantify the amount of seismic energy released by an earthquake. It is a base-10 logarithmic scale obtained by calculating the logarithm of the combined horizontal amplitude of the largest displacement from zero on a seismometer output. Measurements have no limits and can be either ...
1: How far can seismic waves carry energy released from an
1: How far can seismic waves carry energy released from an

Wave Vidmar Solo Pacific Ocean Crossing 2012
Wave Vidmar Solo Pacific Ocean Crossing 2012

... Seaward Kayaks is a small Canadian manufacturer that builds the finest sea kayaks in the world. The Passat G3 that Wave Vidmar will paddle was recently voted ‘Best Double Kayak’ by Sea Kayaker Magazine. The Seaward Passat G3 is used extensively for expeditions and adventure races worldwide, winning ...
Earthquakes T. Perron – 12.001 – March 17, 2010 In our lab on
Earthquakes T. Perron – 12.001 – March 17, 2010 In our lab on

Optimization of DELPHI for Weak Lensing Measurements: A
Optimization of DELPHI for Weak Lensing Measurements: A

...  Object moments recalculated using RRG method  Stellar images used to measure the PSF moments  PSF is removed from the galaxy images (RRG)  Bad galaxies are cut based on: moments, ellipticity, size compared to PSF size, signal-to-noise ratio (RRG)  Shear and shear error are measured from the ga ...
chapter 11
chapter 11

... A 0.85-kg mass attached to a vertical spring of force constant 150 N/m oscillates with a maximum speed of 0.35 m / s. Find the following quantities related to the motion of the mass: (a) the period, (b) the amplitude, (c) the maximum magnitude of the acceleration. ...
Different ways of measuring Earthquakes – Part 3. By energy released
Different ways of measuring Earthquakes – Part 3. By energy released

Conceptual Physics- Final Examination Review Practice
Conceptual Physics- Final Examination Review Practice

... _______19. The force of attraction between two particles due to their mass is called gravity. _______20. An example of a lever is a hammer. _______21. Any change is speed or velocity is called acceleration. _______22. An object with more mass would be more difficult to stop. _______23. Energy is mea ...
McGill University Faculty of Science Department of Earth and
McGill University Faculty of Science Department of Earth and

- The IJST
- The IJST

... resist the lateral loads caused by wind and seismic motion. Lateral loads can develop high stresses, produce sway movement or cause vibration. Therefore, it is very important for the structure to have sufficient strength against vertical loads together with adequate stiffness to resist lateral force ...
12-16-13 Do Now
12-16-13 Do Now

... I can explain the differences between the 3 types of faults. ...
Principles of Geology
Principles of Geology

... Phases of deep-focus earthquakes The major branches of the travel-time curves carry the same descriptions as for shallow-focus events. Waves leaving the focus in an upward direction, and reflected at the surface are described by the letters p, s, as follows: ...
DP Physics 4.1 Oscillations Name: 1. A wave can be described as
DP Physics 4.1 Oscillations Name: 1. A wave can be described as

... entire bulk of the medium move in a parallel and a perpendicular direction (respectively) relative to the direction of energy transport. In a surface wave, it is only the particles at the surface of the medium that undergo the circular motion. The motion of particles tends to decrease as one proceed ...
Earthquakes - GeoBus - University of St Andrews
Earthquakes - GeoBus - University of St Andrews

... people lived in caves carved from soft rock and killing an estimated 830,000 people ...
Earthquakes Seismic Waves Day 2
Earthquakes Seismic Waves Day 2

... To determine the location of an epicenter, scientists determine the difference between the arrival times of the P-wave and S- wave. The farther away an earthquake is, the greater the time between the arrival of the P-wave and the S-wave. By drawing at least three circles using data from 3 different ...
P wave - LSMS Ms. Benson GT
P wave - LSMS Ms. Benson GT

... and only moves through solid rock. This wave moves rock up and down, or side-toside. Because P waves are compression waves, they can move through a liquid. However, S waves cannot move through a liquid. This is because a liquid is not rigid enough to transmit an S wave. S waves travel more slowly th ...
File
File

... • When the displacement of two overlapping waves are in opposite directions their signs are different. • So, when added they produce a smaller wave. This is destructive interference. • When 2 equal and opposite waves overlap, their sum is zero. This is called complete destructive interference. ...
effect of opening on behaviour of shear wall
effect of opening on behaviour of shear wall

... have shown very good performance in past earthquakes. The overwhelming success of buildings with shear walls in resisting strong earthquakes is summarised in the quote: “We cannot afford to build concrete buildings meant to resist severe earthquakes without shear walls”:: Mark Fintel, a noted consul ...
The Wave Equation & Velocity
The Wave Equation & Velocity

Seismic Instrumentation
Seismic Instrumentation

... Understanding the Frequency Domain: Recall that an idealized mass on a spring is a harmonic oscillator: Position x of the mass follows the form x = A cos (t + ) where A is amplitude, t is time,  is the natural frequency of the spring, and  is a phase constant (tells us where the mass was at ...
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Shear wave splitting



Shear wave splitting, also called seismic birefringence, is the phenomenon that occurs when a polarized shear wave enters an anisotropic medium (Fig. 1). The incident shear wave splits into two polarized shear waves (Fig. 2). Shear wave splitting is typically used as a tool for testing the anisotropy of an area of interest. These measurements reflect the degree of anisotropy and lead to a better understanding of the area’s crack density and orientation or crystal alignment.We can think of the anisotropy of a particular area as a black box and the shear wave splitting measurements as a way of looking at what is in the box.
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