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... Diagram of forces acting on one object. 3.3 types of forces Newton’s Second law Reaction forces does not appear since it acts on There are four fundamental forces in the “The acceleration a of an object is directly a different object. nature, but we will discuss the fundamental proportional to the n ...
II. Acceleration
II. Acceleration

... III. FRICTION AND GRAVITY A. ...
How and Where Do Earthquakes Occur? Causes of Earthquakes
How and Where Do Earthquakes Occur? Causes of Earthquakes

... • A fault is the fracture or system of fractures along which movement occurs. • The surface along which the movement takes places is called the fault plane. ...
Describing Motion - Science
Describing Motion - Science

... What about the ladder on top of the truck? The ladder is in motion because the truck is in motion. When the truck stops, the ladder stays in motion. The truck is stopped by the force of the car, but the ladder is not. What force stops the ladder? ...
Document
Document

... • Equivalent to “Fictitious” gravitational force ...
A body acted on by no net force moves with constant velocity
A body acted on by no net force moves with constant velocity

... Reading quizzes (Chs 5,6) ...
Physics - Newton`s Laws
Physics - Newton`s Laws

The Effective Mass of a Ball in the Air
The Effective Mass of a Ball in the Air

... there is no dissipation. A projectile in air has a larger effective mass because when one accelerates the projectile one also has to accelerate the air around it. Such inertial effects are common in physics. An effective mass can be used to account for oscillations with a massive spring3. Similarly, ...
Newton's Laws of Motion
Newton's Laws of Motion

Chapter 7 Hooke`s Force law and Simple Harmonic Oscillations
Chapter 7 Hooke`s Force law and Simple Harmonic Oscillations

Make Up Lab: Newtonian Gravity
Make Up Lab: Newtonian Gravity

sessnn9
sessnn9

Chapter05
Chapter05

... rather than a photograph. The reason is that the only recording of the event that I have found is an extremely fuzzy videotape in which it is nearly impossible to tell what is going on. Individual frames are also very fuzzy. 2. Planetary Motion Before Newton My students always seem to have trouble w ...
NEWTON`S FIRST LAW
NEWTON`S FIRST LAW

... Directions: You can draw your pictures in the blank space below and on the back of this page or on a separate sheet of paper. Colored accurate pictures earn the highest grade! I. Newton’s First Law is the Law of Inertia. Inertia is defined as an objects resistance to a change in its state of motion. ...
Then time can be obtained by using 700=69.8 t.
Then time can be obtained by using 700=69.8 t.

... from the bus, it starts to pull away, moving with a constant acceleration of 0.170 m/s . (a) For how much time and what distance does the student have to run at before she overtakes the bus? (b) When she reaches the bus, how fast is the bus traveling? (c) The equations you used in part (a) to find t ...
Questions – Impulse and Momentum
Questions – Impulse and Momentum

... 2. For how many seconds would a force of 8.00 N have to act on a 2.00 kg mass in order to change its velocity from 2 m/s to 7 m/s? 3. If a certain mass has its velocity changed from 6.00 m/s to 7.50 m/s when a 3.00 N force acts for 4.00 seconds, find the mass of the moving object. 4. What force is n ...
Workshop module 5
Workshop module 5

Dynamics of Uniform Circular Motion
Dynamics of Uniform Circular Motion

... Acceleration (ac) and it is directed towards the center of the circular path.  This object traveling in a circular path also experiences a force that is also directed towards the center of the circular path  This force is known as Centripetal Force ...
Practice Test 2
Practice Test 2

... A spring (k = 600 N/m) is placed in a vertical position with its lower end supported by a horizontal surface. A 2.0-kg block that is initially 0.40 m above the upper end of the spring is dropped from rest onto the spring. What is the kinetic energy of the block at the instant it has fallen 0.50 m (c ...
Oscillatory Motion
Oscillatory Motion

... Note that the acceleration is NOT constant, unlike our earlier kinematic equations.  If the block is released from some position x = A, then the initial acceleration is – kA/m, but as it passes through 0 the acceleration falls to zero.  It only continues past its equilibrium point because it now h ...
Question #1. 1. A tennis ball of mass m = 0.080 kg and speed v = 45
Question #1. 1. A tennis ball of mass m = 0.080 kg and speed v = 45

Earthquakes release energy.
Earthquakes release energy.

Centripetal Force / Gravity (very good practice)
Centripetal Force / Gravity (very good practice)

... have masses of 60.0 kg and are sitting 1.20 m apart. 2. Two tennis balls have a mass of 0.25 kg each and they are placed so that there is a distance of 42 cm between their centers. What is the gravitational force between the two tennis balls? 3. Two objects with the same mass are placed 60. cm apart ...
Document
Document

... How does two particles interact directly with each other through free space? What is the “action at a distance”? The same problem of interaction without actual contact occurs with electric charges and magnets. In 1830s Faraday developed the concept of a “field”, resolving the problem of action at a ...
Chapter 2 - Motion in One Dimension
Chapter 2 - Motion in One Dimension

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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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