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Microsoft Word - SPH 3U, T2L6, Newton`s Second Law.doc
Microsoft Word - SPH 3U, T2L6, Newton`s Second Law.doc

... We can see that these three variables are connected. As mass increases, acceleration decreases (because of inertia). By how much will it decrease? Is it proportional? YES! As mass increases, acceleration will decrease proportionally (with a constant force): F a OR Fnet  ma m This is N2L! In words; ...
Earthquakes - PH - teacher
Earthquakes - PH - teacher

... • The epicenter is located using the difference in the arrival times between P and S wave recordings, which are related to distance. ...
Chapter 12: Forces and Motion
Chapter 12: Forces and Motion

FOSS Force and Motion Course Glossary
FOSS Force and Motion Course Glossary

Circular and Simple Harmonic Motion Test Review Sheet
Circular and Simple Harmonic Motion Test Review Sheet

Webquest 14
Webquest 14

... 8. What happens when the stress causes the fault to break? __________________________ 9. On the “Spreading the Motion” screen, fill in the blanks: “Tectonic plates are somewhat _______________. The motion between them is not confined entirely to their own boundaries. The motion extends into their __ ...
newton*s law of universal gravitation and it*s application
newton*s law of universal gravitation and it*s application

... The line joining the two bodies (the sun and the revolving object) sweeps equal areas in equal times. The graphic precisely displays Kepler's second law. The area of every triangle formed is exactly the same area. Also notice as the planet or satellite moves closer to the sun, the speed of its orbit ...
Physics 1 - Peda.net
Physics 1 - Peda.net

Name: Practice - 4.3 Newton`s Second Law of Motion: Concept of a
Name: Practice - 4.3 Newton`s Second Law of Motion: Concept of a

Dr. Zeemo has a brief guide to Newton`s Three Laws of Motion.
Dr. Zeemo has a brief guide to Newton`s Three Laws of Motion.

... of motion in the assembly program. These demonstrations make use of common items that students are familar with which also makes them easier to remember. ...
Earthquakes - WordPress.com
Earthquakes - WordPress.com

Physical Science Gravity
Physical Science Gravity

... stronger as the masses increase and rapidly become weaker as the distance between the masses increases, F=G(m1m2/d2) • Evaluate the concept that free-fall acceleration near Earth’s surface is independent of the mass of the falling object • Demonstrate mathematically how free-fall acceleration relate ...
Chapter 11: Earthquakes - Ms. Banjavcic`s Science
Chapter 11: Earthquakes - Ms. Banjavcic`s Science

... structures and the distance from the epicenter. • Ex: only a few people would feel an intensity-I earthquake and it would cause no damage. An intensity-IV earthquake would be felt by everyone indoors during the day but would be felt by a few people outdoors. Pictures might fall off the wall and book ...
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• Worksheet #2

Rising Plumes in Earth`s Mantle: Phantom or Real?
Rising Plumes in Earth`s Mantle: Phantom or Real?

Ch._19
Ch._19

... If two seismic stations receive data from an earthquake, the quake’s location can be computed if P-waves, S-waves, and surface waves have been received. ...
File
File

... and always arrive after P waves. Side to side. (body) • Surface Waves – Cause motion mostly in the upper few KM of earth’s crust. Travel more slowly and are more destructive than body waves. Can move up and down or side to side. ...
Name: ___________________________ Chapter 6 Notes: Earthquakes Stress 
Name: ___________________________ Chapter 6 Notes: Earthquakes Stress 

...  Moment Magnitude Scale: rating that estimates the energy released by an earthquake.  Scientists study seismographs  Seismograph: instrument that records and measures seismic waves  These show the kinds of waves present and how strong they were.  Comparing Magnitude  For each point increased i ...
Physics 310 - Assignment #1 - Due September 12
Physics 310 - Assignment #1 - Due September 12

... (b) For any vector, r with coordinates (u, v, z) in the parabolic coordinate system, express it in terms of the êu , êv and k̂ unit vectors. (c) Express the derivatives dêu /dt and dêv /dt in terms of the unit vectors in the parabolic coordinate system. ...
Earthquakes
Earthquakes

... • Surface waves travel just beneath the Earth's surface. • Body waves travel through the Earth's interior. • There are two types of body waves, P waves and S waves. • S waves have much higher amplitude than P waves, travel more slowly, carry more destructive force, but cannot travel through the Eart ...
Circular
Circular

... With the aid of a vector diagram, find an expression for the change in velocity v as the particle moves from, say, point A to an adjacent point B in time t. Hence, determine the magnitude and direction of its acceleration at point A. (ii) A pendulum bob is attached to a string and made to revolve i ...
Reviewing Motion & Forces
Reviewing Motion & Forces

... • An object in motion will stay in motion, an object at rest will stay at rest, until acted on by an unbalanced force. ...
Earthquakes
Earthquakes

... The energy from the quake is transferred to the water and causes huge waves to form. Waves don’t gain height until they near the ...


... 21. During gym, two teams are playing Tug of War. The pink team on the left side of the rope has three players – one who pulls with 2 N of force and two who pull with 1 N of force. The blue team, on the right side of the rope also has 3 players, two who pull with 2 N of force and one who pulls with ...
Forces and Motion Commotion 2012
Forces and Motion Commotion 2012

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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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