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Motion in two dimensions – projectile motion
Motion in two dimensions – projectile motion

Earthquakes2010
Earthquakes2010

... • Seismograph: instrument to measure earthquakes • Seismologists: scientist that study earthquakes ...
answer key
answer key

... The earth is not a static planet; the large slabs of the earth’s crust (tectonic plates) are in continual slow motion. An earthquake occurs when these plates move. The movement causes rock to be squeezed, bent and stretched. This tremendous pressure eventually forces the rock to break and the plates ...
Newton`s Law Review Problems
Newton`s Law Review Problems

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... A small ring in situated at the centre of a hexagon, and is supported by six strings drawn tight, all in the same plane and radiating from the centre of the ring and each connected to a different angular print of the hexagon. The tensions in four consecutive strings are 12 N, 34 N, 45 N and 30 N res ...
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Force and Motion PP

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Physics Chapter 1-3 Review

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Newton`s Second and Third Laws of Motion

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earthquake notes - Red Hook Central Schools
earthquake notes - Red Hook Central Schools

... The ________ waves are sometimes called primary or push-pull waves. The ________ waves are sometimes called secondary or shear waves. The ________________________ are the biggest waves and travel only along the surface. The ________________________ are responsible for most of the damage an earthquak ...
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Displacement response analysis of base

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The Aristotelian approach

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8th grade Science Study Guide – Earthquakes
8th grade Science Study Guide – Earthquakes

... 8th grade Science Study Guide – Earthquakes  Seismology is the science in which earthquakes are studied.  A seismologist is a scientist that studies earthquakes.  Seismologists use a seismogram to determine when an earthquake started.  The focus is the place within the Earth where an earthquake ...
Earthquake Anatomy and Tectonic Plate Boundaries
Earthquake Anatomy and Tectonic Plate Boundaries

PDF - James M. Tour
PDF - James M. Tour

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Speed up Slow down Change direction 2 m/s 2 Ball rolling down a

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Earthquakes - Fair Lawn Public Schools
Earthquakes - Fair Lawn Public Schools

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Earthquakes - section 12.1

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Chapter 4: Earthquakes
Chapter 4: Earthquakes

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Lab 3 - Geologic Structures, Maps, and Block Diagrams

... • Antiform – “upfold” or “convex folds” – Anticlines - Oldest rocks in the middle young ...
Earthquakes Review
Earthquakes Review

... What is the name of the fault in California where the Pacific plate and North American plate slide past each other? ...
Now
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... because the pull of gravity is less. But your mass remains the same. ...
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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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