Earthquakes
... 4. Complete the cause-events-effect chart to show how the different types of stress change the shape and volume of the rock. ...
... 4. Complete the cause-events-effect chart to show how the different types of stress change the shape and volume of the rock. ...
Earthquakes - Crafton Hills College
... Locating the Epicenter ¾ Seismograph: instrument designed specifically to detect, measure, and record vibrations in the Earth’s crust. ¾ Seismogram: data recorded on paper (typically) from an earthquake event. ¾ Mapping epicenters has been characteristically done via triangulation. Earthquake Measur ...
... Locating the Epicenter ¾ Seismograph: instrument designed specifically to detect, measure, and record vibrations in the Earth’s crust. ¾ Seismogram: data recorded on paper (typically) from an earthquake event. ¾ Mapping epicenters has been characteristically done via triangulation. Earthquake Measur ...
Earthquake Summary Sheet
... it as “normal” to go down a sliding board b. Reverse fault: rocks collide (convergent boundary) and one side of the fault gets pushed up think of it as the “reverse” of going down a sliding board c. Strike slip fault: rocks are sheared and slide past one another (transform boundary) 8. Richter Sca ...
... it as “normal” to go down a sliding board b. Reverse fault: rocks collide (convergent boundary) and one side of the fault gets pushed up think of it as the “reverse” of going down a sliding board c. Strike slip fault: rocks are sheared and slide past one another (transform boundary) 8. Richter Sca ...
Lab3PreLab
... Assume that m1 m2 sum to a total mass of 0.300 kg. The mass m2 varies over the range 0.010 kg ≤ m 2 ≤ 0.070 kg . Both masses will begin at rest, and then be subject to a force equal to m2 g , where g is the acceleration of gravity, 9.80 m s-2. That force will be applied to the 0.300 kg total mass ...
... Assume that m1 m2 sum to a total mass of 0.300 kg. The mass m2 varies over the range 0.010 kg ≤ m 2 ≤ 0.070 kg . Both masses will begin at rest, and then be subject to a force equal to m2 g , where g is the acceleration of gravity, 9.80 m s-2. That force will be applied to the 0.300 kg total mass ...
Chapter 3 Notes
... depending on your location. Your acceleration toward the Earth is 9.8 m/s2. Weight is a force so we can plug it into Newton’s 2nd law. Fw = m x a Where the a = 9.8 m/s2. ...
... depending on your location. Your acceleration toward the Earth is 9.8 m/s2. Weight is a force so we can plug it into Newton’s 2nd law. Fw = m x a Where the a = 9.8 m/s2. ...
2-Unit4Part2 EarthsInteriors
... – Measures the amount of energy (magnitude) released by an earthquake – Allows for easier comparison of earthquake magnitudes regardless of location – Logarithmic • Measurements range from 1 to over 9 • Meaning a 6 is 10 times more powerful than a 5 ...
... – Measures the amount of energy (magnitude) released by an earthquake – Allows for easier comparison of earthquake magnitudes regardless of location – Logarithmic • Measurements range from 1 to over 9 • Meaning a 6 is 10 times more powerful than a 5 ...
Measuring Earthquakes
... Locating an Epicenter Lab • Purpose: Geologists who study earthquakes are called seismologists. If you were a seismologist, you would receive data from all across the country. Within minutes after an earthquake, seismographs located in Denver, Houston, and Miami would record the times of arrival of ...
... Locating an Epicenter Lab • Purpose: Geologists who study earthquakes are called seismologists. If you were a seismologist, you would receive data from all across the country. Within minutes after an earthquake, seismographs located in Denver, Houston, and Miami would record the times of arrival of ...
abstract
... remarkable. In order to investigate the electromagnetic phenomena associated crustal activity, the precise ULF electromagnetic measurement network has been established. At each station, three magnetic components and two horizontal electric components are observed. There are two arrays with interstat ...
... remarkable. In order to investigate the electromagnetic phenomena associated crustal activity, the precise ULF electromagnetic measurement network has been established. At each station, three magnetic components and two horizontal electric components are observed. There are two arrays with interstat ...
Chapter 5: Earthquakes
... • When an earthquakes seismic waves reach a seismograph, the vibrations are recorded. – P waves arrive first and the fastest – S waves arrive shortly after the P waves – Surface Waves produce the largest disturbances on the seismogram. – An AFTERSHOCK is a smaller earthquake that occurs after a larg ...
... • When an earthquakes seismic waves reach a seismograph, the vibrations are recorded. – P waves arrive first and the fastest – S waves arrive shortly after the P waves – Surface Waves produce the largest disturbances on the seismogram. – An AFTERSHOCK is a smaller earthquake that occurs after a larg ...
Earthquake destruction and seismic waves Page 1 of 3 I. Factors
... c. Damage from building collapse, gas leaks, lack of water, woodpaper construction with charcoal heating in older parts of city ...
... c. Damage from building collapse, gas leaks, lack of water, woodpaper construction with charcoal heating in older parts of city ...
Chapter 4-5 Review Ideas and Concepts You Are Responsible For
... A. Write the equation for Ff that always holds, whether on a horizontal or tilted surface? B. For a mass m on a horizontal surface, Ff = C. For a mass m on a surface inclined at an angle , Ff = D. For a block of mass m and a coefficient of friction , what force must be applied to move the block at ...
... A. Write the equation for Ff that always holds, whether on a horizontal or tilted surface? B. For a mass m on a horizontal surface, Ff = C. For a mass m on a surface inclined at an angle , Ff = D. For a block of mass m and a coefficient of friction , what force must be applied to move the block at ...
2-Unit4Part2EarthsInteriors
... – Simple pendulum • When the ground shakes, the base and frame of the instrument move with it • Inertia keeps the pendulum in place • It will then appear to move; relative to the shaking ground • As it moves, it records the pendulum displacement • The tracing is called a seismogram ...
... – Simple pendulum • When the ground shakes, the base and frame of the instrument move with it • Inertia keeps the pendulum in place • It will then appear to move; relative to the shaking ground • As it moves, it records the pendulum displacement • The tracing is called a seismogram ...
chapter 7 notes - School District of La Crosse
... Magical projectile motion equations Rx= V2sin2θ/g H= -(vsinθ)2/2g T= -2Vsinθ/g ...
... Magical projectile motion equations Rx= V2sin2θ/g H= -(vsinθ)2/2g T= -2Vsinθ/g ...
PowerPoint - Science A 2 Z
... Water/steam geiser Sand, coal or other mineral geiser Land splits, drops, or raises ...
... Water/steam geiser Sand, coal or other mineral geiser Land splits, drops, or raises ...