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Glossary - Meteorological Centre, Shimla
Glossary - Meteorological Centre, Shimla

... A type of surface wave having a retrograde elliptical motion of the particle, as the wave travels through the Earth's surface. These are the slowest, but often the largest and most destructive, of the wave types caused by an earthquake. They are usually felt as a rolling or rocking motion and move t ...
P-waves
P-waves

Seismic Intensity Estimation of Tall Buildings in Earthquake Early
Seismic Intensity Estimation of Tall Buildings in Earthquake Early

File
File

...  State the 2 key factors that the amount of gravitational force depends upon.  Describe how gravitational force changes, as it relates to the mass of and distance between 2 objects.  Explain why gravity is a long range force effecting the motion of the Earth.  Explain the symbol g, including its ...
What "Seis" Shake?
What "Seis" Shake?

... These scientists use seismographs, which are instruments that record and measure seismic waves and vibrations. When these waves travel through the earth or along the earth's surface, the seismograph records a "zigzag" line called a seismogram. The lines on the seismogram show the changing intensity ...
CP Review Sheet Newton`s Laws
CP Review Sheet Newton`s Laws

... 1. An apple that has a mass of 0.10 kg has the same mass wherever it is. The amount of matter that makes up the apple (depends on, does not depend on) the location of the apple. It has the same resistance to acceleration wherever it is – its inertia everywhere is (the same, different). The weight of ...
Chapter 4 question 5 - leo physics website
Chapter 4 question 5 - leo physics website

SAMPLE TEST 1: PHYSICS 103
SAMPLE TEST 1: PHYSICS 103

... C. directed away from the earth D. in the same direction as its velocity E. It depends on where it is ...
Earthquake`s Seismic Waves
Earthquake`s Seismic Waves

Basin and Crustal Structure Model in Kinki Area and Long
Basin and Crustal Structure Model in Kinki Area and Long

Freefall and Newton`s 2nd Law ppt
Freefall and Newton`s 2nd Law ppt

... – In a vacuum, maximum distance is at an angle of 45o – With air resistance (real world), angle is less • Baseball will go furthest hit at an angle of around 40o, a soccer ball at about 33o ...
HW #5
HW #5

... (due Friday, September 27, 2013 at the beginning of class) For these problems, please use the Newton’s Laws Problem Solving Scheme! 1. A 65 kg person stands on a bathroom scale in an elevator moving downward. If the scale reads 720 N, what are the magnitude and direction of the elevator's accelerati ...
Forces & Motion ()
Forces & Motion ()

... Particles & centre of mass A particle is an object which has mass (and forces can act upon it) but it has no extension. i.e. it is located at a point in space. If objects are rigid, we can ‘model them as particles’ since one can decompose motion into displacement of the centre of mass + rotation of ...
Damped Harmonic Motion
Damped Harmonic Motion

... proportionality b for the retarding force. (Actually, this would be the model for a mass on a spring oscillating in a viscous fluid.) Newton's Second Law for this would be ...
Physics 02-01 Newton`s Laws Lab
Physics 02-01 Newton`s Laws Lab

... Forces are vectors. Look back in previous lessons and explain how to add vectors. You are riding in a car when it turns to the left abruptly. Why do you feel like you are being fore to the right? Which statement is correct? (a) Net force causes motion. (b) Net force causes change in motion. Explain ...
PowerPoint - University of Toronto Physics
PowerPoint - University of Toronto Physics

Let`s Pause for Two Questions from the Audience
Let`s Pause for Two Questions from the Audience

... m represents the mass of an object, which is a numerical measure of its inertia. a represents the acceleration of the object. ...
Name: Date: ______ Period: ____
Name: Date: ______ Period: ____

... 5. What is air resistance? 6. Why does air resistance affect some objects more than others? 7. What is terminal velocity? 8. What is free fall? 9. When does free fall take place? 10. How are orbiting objects in free fall? 11. What 2 motions combine to cause orbiting? 12. How does gravity play a role ...
part 1
part 1

... Inertia is the reason an object at rest stays at rest or an object moving in a straight line continues to move with the same velocity along that line unless an external force causes it to do otherwise. If you have two objects with different masses, the one with more mass is said to have more inertia ...
SHM1simpleHarm
SHM1simpleHarm

... 6. A block of mass 608 grams is fastened to a spring whose spring constant is 65 N/m. The block is pulled a distance of 11 cm from its equilibrium position and then released. a. What force does the spring exert on the block just before the block is released? b. What are the angular frequency, freque ...
Seismic Waves - Fort Thomas Independent Schools
Seismic Waves - Fort Thomas Independent Schools

M7 - Work-Energy Thrm
M7 - Work-Energy Thrm

PowerPoint Presentation - Newton’s Laws of Motion
PowerPoint Presentation - Newton’s Laws of Motion

... If the object was sitting still, it will remain stationary. If it was moving at a constant velocity, it will keep moving. It takes force to change the motion of an object. ...
Surface Waves
Surface Waves

... • Produces motion in the upper crust – Motion can be up and down – Motion can be around – Motion can be back and forth ...
27. Generalized Newton`s second law
27. Generalized Newton`s second law

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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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