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10 Circular Motion
10 Circular Motion

... greater distance in one rotation than a point near the center. • The linear speed is greater on the outer edge of a rotating object than it is closer to the axis. • The speed of something moving along a circular path can be called tangential speed because the direction of motion is always tangent to ...
Centripetal force keeps an object in circular motion.
Centripetal force keeps an object in circular motion.

Seismic and Tectonic Correspondence of Major Earthquake
Seismic and Tectonic Correspondence of Major Earthquake

... activation of old regional faults. Characteristically, they were accompanied by considerable foreshock and aftershock productivity [1], confirming them as shallow earthquakes [26]. The most representative and well-documented one was the 1939 Accra Earthquake of magnitude 6.5, which had epicentral lo ...
Good Vibes: Introduction to Oscillations
Good Vibes: Introduction to Oscillations

SEC - Warrenphysics
SEC - Warrenphysics

... gravitational potential energy from the lowest point to the highest point then be greater, less, or the same? ssm 6P. In Fig. 8-28, a small block of mass m can slide along the frictionless loop-the-loop. The block is released from rest at point P, at height h = 5R above the bottom of the loop. How m ...
An inverted continental Moho and serpentinization of
An inverted continental Moho and serpentinization of

Using Newton`s Laws
Using Newton`s Laws

... Assess  Again, let’s look at special cases. Suppose the rock’s mass is zero; then our expression gives a = g. In this case there’s no rope tension and the climber plummets in free fall. Also, acceleration decreases as the rock’s mass increases, so with an infinitely massive rock, the climber would d ...
Rolling friction on a wheeled laboratory cart
Rolling friction on a wheeled laboratory cart

LCP1 INTUITIVE PHYSICS
LCP1 INTUITIVE PHYSICS

... LCP1 begins with the intuitive understanding of motion, then continues to discuss motion in qualitative terms first, before appealing to the Galileo’s kinematics and Newton’s dynamics in quantitative terms. We will continue discussing these laws in LCP 2 by following the history of the concepts abou ...
Solution - NUS Physics Department
Solution - NUS Physics Department

PSI AP Physics I
PSI AP Physics I

... 2. What is the axis of rotation? Does the axis of rotation of a rotating tire on a car touch the rubber in the tire? 3. Explain why the radian is a more physically natural unit than the degree when working rotation problems. 4. A small bug is on a spinning record near the center of the record. His f ...
PSI AP Physics I
PSI AP Physics I

... 2. What is the axis of rotation? Does the axis of rotation of a rotating tire on a car touch the rubber in the tire? 3. Explain why the radian is a more physically natural unit than the degree when working rotation problems. 4. A small bug is on a spinning record near the center of the record. His f ...
Newton`s Laws of Motion
Newton`s Laws of Motion

PSI AP Physics I
PSI AP Physics I

... 2. What is the axis of rotation? Does the axis of rotation of a rotating tire on a car touch the rubber in the tire? 3. Explain why the radian is a more physically natural unit than the degree when working rotation problems. 4. A small bug is on a spinning record near the center of the record. His f ...
rotating + ω r
rotating + ω r

2-D georesistivity structure in the central part of the northeastern...
2-D georesistivity structure in the central part of the northeastern...

... to the static-shift caused by charge accumulation at boundaries can not be calculated during the GBD procedure, and so needs to be inferred by some other means. In this study, a time-domain em measurement method (Sternberg et al., 1988) was applied to handle MT static-shifts (Jiracek, 1990), utilizi ...
Velocity increase in the uppermost oceanic crust of subducting
Velocity increase in the uppermost oceanic crust of subducting

偏微分方程其旅行波之探討 Traveling Wave
偏微分方程其旅行波之探討 Traveling Wave

2. Acceleration, Force, Momentum, Energy
2. Acceleration, Force, Momentum, Energy

Continental crust under compression: A seismic refraction study of
Continental crust under compression: A seismic refraction study of

May the Force Be With You Topic
May the Force Be With You Topic

Crustal motion in the Southern Andes (26°–36°S): Do the Andes
Crustal motion in the Southern Andes (26°–36°S): Do the Andes

... [4] Less attention has been focused on interpreting and modeling the velocity field in the backarc region of the Andes, largely because horizontal velocities in these regions tend to be 10 mm/yr or less. In one recent study, however, Lamb [2000] found that velocity gradients (from geologic and Norab ...
7thMotionfinal_Oct
7thMotionfinal_Oct

... motion of falling objects, projectile motion, planetary motion and the gravitational effects of objects upon each other. People use simple and complex machines to perform “everyday” tasks, which require a force to move objects. The amount of effort saved when using machines is called mechanical adva ...
Generalized statistical mechanics approaches to earthquakes and
Generalized statistical mechanics approaches to earthquakes and

... distribution, typically present power-law behaviour, enhanced by (multi-) fractal geometries, long-range interactions or large fluctuations between the various possible states; properties that seem to correspond well to the phenomenology of earthquakes. For the statistical mechanics description of s ...
AN ABSTRACT OF THE THESIS OF Date thesis is presented Abstract approved
AN ABSTRACT OF THE THESIS OF Date thesis is presented Abstract approved

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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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