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Inclined Planes:
Inclined Planes:

... For two surfaces in contact it turns out that the frictional force is independent of the area of contact, independent of the relative speed of the two surfaces and is directly proportional to the normal reaction between the two surfaces. F = µN , where F is the frictional force, N is the normal reac ...
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... we use to measure acceleration? 2)Apply – Dan is standing at his locker C hall. The last bell rings and he knows Mrs. Dion will kick his butt if he is late. Dan quickly runs down C hall toward E hall at 5 m/s in 45 seconds. What is Dan’s acceleration? ...
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dynamic characteristics of alluvial deposits – a case study
dynamic characteristics of alluvial deposits – a case study

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... •A wave is a repeating disturbance or movement that transfers energy through matter or space. •Ocean waves disturb the water and transfer energy through it. ...
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Semester Exam - Shirley Temple dolls
Semester Exam - Shirley Temple dolls

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... to push water backwards. In turn, the water reacts by pushing the fish forwards, propelling the fish through the water. The size of the force on the water equals the size of the force on the fish; the direction of the force on the water (backwards) is opposite the direction of the force on the fish ...
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Geology 111 - A13 - Earthquakes

... Fuca Plate and the North America Plate. There have been two large earthquakes on Vancouver Island in this century, one of magnitude 7.0 in 1918, and one of magnitude 7.3 in 1946. The 1946 quake was significantly larger than the devastating 2010 earthquake in Haiti. Although this earthquake caused da ...
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Examples and problems to the system of particles

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Acceleration Due to Gravity

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... The force remains constant when inclination is kept at that angle leading to constant acceleration - continuous speed up. ...
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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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