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Seismic techniques - Ground Engineering
Seismic techniques - Ground Engineering

Lesson Plans 6th Grade Science
Lesson Plans 6th Grade Science

Friction Lab - Oakland Schools Moodle
Friction Lab - Oakland Schools Moodle

Momentum WS - davis.k12.ut.us
Momentum WS - davis.k12.ut.us

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Unit 3 – Net Force

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what happens when an object changes direction
what happens when an object changes direction

... direction. Do an experiment with a ball such as a basketball or ball that is tightly blown up used on playgrounds. Roll the ball down a hall, an open space in the classroom or outside on a smooth, flat area. If you let it roll, what kind of motion is it – straight line, circular, erratic? How does t ...
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3 Newton`s First Law of Motion—Inertia

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Pendulum Definition Worksheet Name

... different. So it is evident that the length of the pendulum is what is determining its period. If they still have difficulties, have them go back to their pendulums. Tell them to leave the length the same and add weights to see if it affects the period. ...
Tuesday, June 3, 2008
Tuesday, June 3, 2008

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effect of earthquake incidence angle on seismic

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Force and Motion - Rockaway Township School District

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Chapter 5 – Newton`s Laws of Motion
Chapter 5 – Newton`s Laws of Motion

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PHYS 307 LECTURE NOTES, Daniel W. Koon, St. Lawrence Univ.

... Consider a pair of fuzzy dice hanging from a car's rear-view mirror. If the car is at rest, they hang straight down. The tension in the strings cancels the pull of their weight. Without changing those two forces, we begin to accelerate the car. The dice will appear to accelerate toward the rear of t ...
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P Tohoku earthquakes, off the Boso Peninsula, deduced

... Marine-Earth Science and Technology). A seismic survey line with a length of 400 km was located on the landward slope along the JT and was oblique to the Sagami trough (Fig. 1). We deployed 31 short-period type OBSs, equipped with a three-component 4.5 Hz geophone on a leveling mechanism (Shinohara ...
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Massive Pulleys Review

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General Physics II - The University of Alabama

... 11. A plane travels horizontally at a constant speed of 40 m/s, 100 m above the ground. It drops a package out of its hold. How far does the dropped package travel horizontally before hitting the ground? Let the horizontal direction be x, with +x in the direction of the plane’s travel, and the verti ...
Geograph2
Geograph2

... Why would we receive such a surprising result? The reason is that a spring-balance actually measures not the mass of the gold coin but, rather, the force that gravity exerts on it. Force and gravity are two more of those common words that are used by physicists in very specific ways. We shall define ...
Stacey Carpenter
Stacey Carpenter

... push it or pull it – apply a force. What happens when you apply the force? It’s motion changes – it either speeds up, slows down, or changes direction - it’s velocity changes. A change in velocity is acceleration. If it’s a bigger thing - more mass, more inertia - you need a bigger force to get it m ...
Chapter 10
Chapter 10

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Simple Harmonic Motion and Elasticity

... The force by which a spring is compressed or stretched is proportional to the magnitude of the displacement (F  x). ...
Newton`s First Law of Motion
Newton`s First Law of Motion

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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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