Question 2)
Speed of P waves
Speed of S waves
Distance of station from earthquake is
Time delay between P and S waves is
, and
Distance of station from earthquake is
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Question 3)
The equipment is at height ,
When the equipment is thrown on to ship, the ship is at a distance of from the dock.
D= Distance traveled by equipment towards the ship (in horizontal direction) + distance traveled by ship towards the dock.
Time taken by ship to move a distance is . In the same time the equipment moves through a distance .
Vertical distance traveled by equipment in time is
Using
Horizontal distance traveled by equipment in time is
Distance covered by ship during this time is
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Question 4)
Train starts with an initial speed and accelerates for with an acceleration
Distance covered during this time
For the next the train travels with constant velocity
Distance covered during the time is
Then train slows down to with an acceleration of in time
Using
Distance covered during this interval is
Total distance covered between the stations is is
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QUESTION 2 Earthquakes produce several types of shock waves, two of which are called S and...
002 10.0 points Earthquakes produce two kinds of seismic waves: he longitudinal primary waves (called P waves) and the transverse secondary waves (called S waves). Both S waves and P waves travel through Earth's crust and mantle, but at different speeds; the P waves are always faster than the S waves, but their exact speeds depend on depth and location. For the pur- pose of this exercise, we assume the P wave's speed to be 8380 m/s while the S...
Earthquakes generate sound waves inside Earth. Unlike a gas, Earth can experience both transverse (S) and longitudinal (P) sound waves. Typically, the speed of S waves is about 4.5 km/s, and that of P waves 8.0 km/s. A seismo- graph records P and S waves from an earthquake. The first P waves arrive 3.0 min before the first S waves. If the waves travel in a straight line, how far away does the earthquake occur?
Question 6 (3 points) An earthquake emits both S-waves and P-waves which travel at different speeds through the earth. An S-wave travels at 5000 m/s and a P-wave travels at 9000 m/s. If S-waves are received at a seismic station one minute after a P-wave arrives, then how far away is the earthquake center? 88.9 km 240 km 480 km 675 km 1200 km
Chapter 17, Problem 005 Earthquakes generate sound waves inside Earth. Unlike a gas, Earth can experience both transverse (S) and longitudinal (P) sound waves. Typically, the speed of S waves is about 4.14 km/s, and that of P waves 7.84 km/s. A seismograph records P and S waves from an earthquake. The first P waves arrive 1.87 min before the first S waves. If the waves travel in a straight line, how far away does the earthquake occur?
When an earthquake occurs, two types of sound waves are generated and travel through the earth. The primary, or P, wave has a speed of about 8.0 km/s and the secondary, or S, wave has a speed of about 4.5 km/s. A seismograph, located some distance away, records the arrival of the P wave and then, 117 s later, records the arrival of the S wave. Assuming that the waves travel in a straight line, how far (in terms of...
2. (1) A pendulum clock makes use of the fact that the period of a pendulum is consistent and can be predicted relatively easy. What should the length of a pendulum be if the desired frequency of oscillation is. 3. (1) Near the shore, Tsunamis travel at a speed of 30 mph and the distance between crests is about 6.5 miles. What is the frequency of such a wave? Give your answer in units of Hz. When one crest hits...
3. Earthquake warning system A typical earthquake produces two types of seismic waves. P ("primary" seismic waves are longitudinal waves that move through the earth's upper crust with speed anywhere from 3 km/s to 5 km/s (the exact speed depends on the local composition of the earth's crust). S ("secondary") waves are transverse waves that move slower than P waves. The S-wave speed is typically about 60% less than the P-wave speed in any given material. The map below shows...
Earthquake Lab: Locating the Epicenter, Determining the Magnitude, and Calculating the Time of Earthquake The goal of this lab is to learn how seismograms are used to locate the epicenter of earthquakes, determine earthquake magnitudes, and to calculate the origin time of earthquakes. A seismogram measures the amount of shaking caused by earthquake waves. The seismogram first records the arrival of P-Waves (Primary), followed by the arrival of the S-Waves (Secondary). The S-P interval is the time difference between the...
EXERCISE 11,4 Locating an Earthquakes Epicenter and Determining When It Occurred (continued) Name Course Section: Date: Arrival times and delays between seismic waves Boston Los Angeles Seattle Selmic wave arrival times Delays between seismic waves S-P Step 3: Estimating Distance from the Epicenter to Each Station Using the Travel-Time Diagram The next figure in this exercise shows how to use seismic wave delay data and the travel time diagram to measure the distance from each station to the epicenter. Start...
ON THIS PAGE. SHOW WORK ON THE OPPOSITE PAGE VERS ON 20) Riding The Waves lculate the missing quantity. Hint: 1 Hz= 1 per second (= 1 sec ) = 3,600 /hour) Earthquake!! : An earthquake in Calexico, CA was felt in San Diego (210km distant) 28 seconds. The quake swayed houses @ twice per second = 2Hz. (1) The wave velocity was (2) The earthquake WAVELENGTH in km was: v= km/sec. 2= B) Thunder: After a lightning flash, you...