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Resolving vertical tectonics in the San Francisco Bay Area from
Resolving vertical tectonics in the San Francisco Bay Area from

... range-change rates determined with the permanent scatterer interferometric synthetic aperture radar (InSAR) method in the San Francisco Bay Area, we resolve vertical motions in the region at sub-mm/yr precision. The highest displacement rates are due to nontectonic processes, such as active landslid ...
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S - Nuffield Foundation

... They can also be used to find the position, velocity or acceleration of a particle at a specified time. Think about What can you say about the direction of a, at, and at2? What about u and ut? ...
Student pdf - Nuffield Foundation
Student pdf - Nuffield Foundation

PHYS 2053 SEC 0002 Fall 2008
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Physics 20 - Structured Independent Learning
Physics 20 - Structured Independent Learning

... The greater the normal force, the greater the interaction between the atoms and electrons of the object and the surface and, therefore, the greater the frictional force. The second factor is the nature of the interaction between object and the surface. If the surface and object are rough in texture, ...
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Turntables PPT - Physics of Theatre Home
Turntables PPT - Physics of Theatre Home

... td  tnet+tf1+tf2=Ia+tf1+tf2 So, to determine the drive torque, we need to find the moment of inertia, the angular acceleration, and the frictional torques. ...
Year-9- Vectors and Scalars Velocity and Acceleration Scalar
Year-9- Vectors and Scalars Velocity and Acceleration Scalar

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Chapter 1 Units and Problem Solving

... • There is always centripetal acceleration no matter whether the circular motion is uniform or nonuniform. • It is the tangential acceleration that is zero in uniform circular motion. Example 7.4: A wheel is rotating wit a constant angular acceleration of 3.5 rad/s2. If the initial angular velocity ...
grade 9 physics notes
grade 9 physics notes

... When a cannonball is fired from a cannon, the cannon exerts a force on the cannonball and the cannonball exerts an equal and opposite force on the cannon. However, the cannon being more massive, recoils with less speed, but the cannonball moves faster by Newton's second law of motion which states th ...
practice test - Sign in to St. Francis Xavier Catholic School System
practice test - Sign in to St. Francis Xavier Catholic School System

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Newton`s Laws of Motion

Numerical modeling of shear-wave splitting and azimuthal
Numerical modeling of shear-wave splitting and azimuthal

... This report presents the processing and interpretation of seismic modeling data of the earth models for a fractured layer, based on well logs associated with potash mining. The purpose of the work is to study azimuthal seismic anisotropy, shear-wave splitting, and time-lapse seismic signals caused b ...
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... 6. After pushing against a brick wall for a long time, you are feeling extremely tired, but you have not done any work on the wall. Explain. In order for work to be done the force needs to cause the displacement. If there is no displacement no work is done. 7. By what factor does the kinetic energy ...
MOZART: A Seismological Investigation of the East African Rift
MOZART: A Seismological Investigation of the East African Rift

... epicentral area is not clear, because the transition to the Kaapvaal craton is still 250 km away. The 1940 M s 6.2 earthquake, with epicenter ∼200 km south-southwest of the Machaze epicentral area (Fig. 3), may indicate that incipient rifting continues with the same strike until it reaches the Lebom ...
Lab 8: Ballistic Pendulum
Lab 8: Ballistic Pendulum

... This experiment illustrates two different methods for measuring the speed of the steel ball. What are the relative merits of the two methods? If you were trying instead to measure the speed of a bullet coming out of a gun, which method would give the better answer? Why? A .22 caliber long rifle can ...
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lab manual - Moorpark College
lab manual - Moorpark College

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Chapter 3: Forces - trinity

Broadband Seismic Characterization of the Arabian Shield
Broadband Seismic Characterization of the Arabian Shield

THINKING ABOUT MOTION AND FORCE
THINKING ABOUT MOTION AND FORCE

... enter introductory physics courses with similar experiences, and often with similar beliefs. It is nice that we develop with little effort beliefs that are similar to those of the great Aristotle. Now for the bad news. Many of Aristotle’s beliefs differ from the modern ideas of physics. Walls, floor ...
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Chapter 4 Problems

... kg, and the coefficient of kinetic friction between box and floor is 0.300. (a) Find the acceleration of the box. (b) The student now starts moving the box up a 10.0° incline, keeping her 80.0-N force directed at 25.0° above the line of the incline. If the coefficient of friction is unchanged, what ...
Unit IIIB Worksheet 1
Unit IIIB Worksheet 1

...  Add up all your forces together (this is Fnet), and set it equal to ma.  Write down everything symbolically (using letters to represent all the forces) first.  Don’t put in any numbers until the end.  In some problems, you might also have to use your kinematic equations as well. Use Fnet = ma t ...
Physics 151 Week 9 Day 3
Physics 151 Week 9 Day 3

... Caused by electron repulsion between two objects - Friction opposes (in opposite direction of) applied force - Direction of Friction force is Opposite of direction of motion / acceleration - Parallel to motion / Resists force of acceleration Friction Force is a contact force that acts on an object b ...
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Seismometer

Seismometers are instruments that measure motion of the ground, including those of seismic waves generated by earthquakes, volcanic eruptions, and other seismic sources. Records of seismic waves allow seismologists to map the interior of the Earth, and locate and measure the size of these different sources.The word derives from the Greek σεισμός, seismós, a shaking or quake, from the verb σείω, seíō, to shake; and μέτρον, métron, measure and was coined by David Milne-Home in 1841, to describe an instrument designed by Scottish physicist James David Forbes.Seismograph is another Greek term from seismós and γράφω, gráphō, to draw. It is often used to mean seismometer, though it is more applicable to the older instruments in which the measuring and recording of ground motion were combined than to modern systems, in which these functions are separated.Both types provide a continuous record of ground motion; this distinguishes them from seismoscopes, which merely indicate that motion has occurred, perhaps with some simple measure of how large it was.The concerning technical discipline is called seismometry, a branch of seismology.
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