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Earthquake Test Review. Next. Which type of stress stretches rock?. Compression. Shearing. Tension. Diversion. This is a break or a crack in the rock. Fault. Fissure. Fracture. Mine. This type of fault is caused by compression. Normal. Reverse. Strike-slip. Oblique strike-slip.
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Which type of stress stretches rock? Compression Shearing Tension Diversion
This is a break or a crack in the rock. Fault Fissure Fracture Mine
This type of fault is caused by compression. Normal Reverse Strike-slip Oblique strike-slip
The type of fault shown below: Normal Reverse Strike-slip Oblique strike-slip
Which type of stress creates the fault below: Tension converging compression shearing
The location where an earthquake begins epicenter fault line focus seismograph
The point directly above the focus. Seismogram Epicenter Stress Fracture
All earthquakes happen at plate boundaries True False
The waves that move out in all directions from the focus on an earthquake. Seismic waves Sonic waves Sound waves Sonar waves
Type of seismic wave that does the most damage. Primary Wave Secondary Wave Surface Wave Sound wave
The first type of wave to arrive at a seismograph station. Primary Wave Surface Wave Secondary Wave Sound wave
This type of wave travels only through solids. Primary Wave Surface Wave Secondary Wave Sound wave
How many seismograph stations are needed to determine the epicenter? One Two Three Four
This measures the amount of energy released by an earthquake. Intensity Strength Depth Magnitude
The magnitude scale used today. Mercalli scale Richter Scale Moment Magnitude Scale Seismograph Scale
Earthquakes can be predicted. True False
Types of Stress Three main types of stress: 5.1 Interactions at Plate Boundaries • Tension: rocks are stretched • Compression: rocks are squeezed • Shear: rocks slide horizontal in opposite directions Return to quiz
Fractures and Faults A fracture is a break or crack in rock. 5.1 Interactions at Plate Boundaries • If rock on side of a fracture has moved relative to the other side it is called a fault. • Three main types of faults • Normal faults • Reverse faults • Strike-slip faults Return to quiz
Reverse Faults Reverse faults result from compression stress and slope at an angle. Hanging wall up relative to footwall. 5.1 Interactions at Plate Boundaries Return to quiz
Normal Faults Normal faults result from tension stress and slope at an angle. Hanging wall down relative to footwall. 5.1 Interactions at Plate Boundaries Return to quiz
Strike-Slip Faults Strike-slip faults result from shearing stress and are often vertical. San Andreas Fault in California. (p.212) 5.1 Interactions at Plate Boundaries Return to quiz
Focus & Epicenter The focus is the location on the fault where an earthquake begins. 6.1 Earthquakes and Plate Boundaries • The closer the focus is to the surface, the stronger the shaking will be. • The point on Earth’s surface directly above the focus is the epicenter. Return to quiz
Focus & Epicenter The focus is the location on the fault where an earthquake begins. 6.1 Earthquakes and Plate Boundaries • The closer the focus is to the surface, the stronger the shaking will be. • The point on Earth’s surface directly above the focus is the epicenter. Return to quiz
Earthquakes Away from Plate Boundaries Not all earthquakes happen at plate boundaries. New Madris Earthquakes of 1911 6.1 Earthquakes and Plate Boundaries • Millions of years ago, a long zone of intense faulting was formed when the crust began to pull apart, but did not break completely. • Today, the crust is being compressed, or squeezedtogether. (p. 246) Return to quiz
Seismic Wave Waves of energy that are produced at the focus of an earthquake. 6.2 Earthquakes and Seismic Waves • Waves move outwardfrom the focus in alldirections. • 3 main types of seismic waves. Return to quiz
3. Surface Waves 6.2 Earthquakes and Seismic Waves Return to quiz
1. Primary Waves (P-waves) 6.2 Earthquakes and Seismic Waves Return to quiz
2. Secondary Waves (S-waves) 6.2 Earthquakes and Seismic Waves Return to quiz
Locating an Epicenter Triangulation is used to locate the epicenter. 6.3 Measuring Earthquakes • This method is based on the speeds of the seismic waves. • At least three seismographs must record the distances. Return to quiz
Measuring Earthquake Size Magnitude measures the amount of energy released by an earthquake. 6.3 Measuring Earthquakes • Determined by the buildup of elastic strain energy in the crust, at place where rupture occurs • Magnitude scale is based on record of height of ground motion and ranges from 0–9. • Richter Magnitude Scale Return to quiz
Moment Magnitude Scale Used today because it is a more accurate scale for measuring earthquake size. 6.3 Measuring Earthquakes • Based on the amount of energy released during an earthquake. Return to quiz
Predicting Earthquakes At this time, geologists cannot predict earthquakes. Geologists can, however, determine the seismic risk by locating active faults and where past earthquakes have occurred. Geologists create seismic risk maps. (p.274) 6.3 Measuring Earthquakes Return to quiz