1. By the time you stop reading this, you will wonder why you were reading this in the first place.

3. Earthquakes and the Earth’s Interior

4. Ag Earth Science – Chapter 8.1
8.1 Vocabulary

5. earthquake
The vibration of the Earth produced by the rapid release of energy.

6. focus
The point within the Earth where the earthquake starts

7. epicenter
The location on the surface directly above the focus

8. fault
Fractures in the Earth where movement has occurred

9. elastic rebound hypothesis
The explanation stating that when rocks are deformed, they break, releasing the stored energy that results in the vibrations of an earthquake.

10. aftershock
A small earthquake that follows the main earthquake

11. foreshock
A small earthquake that often precedes a major earthquake

12. That’s Random

13. Earthquakes
Each year, more than 30,000 earthquakes occur worldwide that are strong enough to be felt.
Most earthquakes are minor tremors, and about 75/year are considered major earthquakes.

14. Earthquakes
Earthquakes – the vibration of the Earth produced by the rapid release of energy 
The point within (inside) the Earth where the earthquake starts is called the FOCUS.
The EPICENTER is the location on the surface directly above the focus.

15. Earthquakes
Earthquakes are usually associated with large fractures in the earth’s crust and mantle called FAULTS.
Faults – fractures in the earth where movement has occurred.

16. Elastic Rebound Hypothesis
The springing back of the rock into its original form is called “elastic rebound” (example – a stretched rubber band).
The explanation says that when rocks are deformed, they first bend and then break, releasing stored energy.
Most earthquakes are produced by the rapid release of elastic energy stored in rock that has been subjected to great forces. When the strength of the rock is exceeded, it suddenly breaks, causing the vibration of the earthquake.

17. Earthquakes
The movements that follow a major earthquake often produce smaller earthquakes called aftershocks.
Small earthquakes called foreshocks often come before a major earthquake.

18. That’s Random

19. Ag Earth Science – Chapter 8.2
8.2 Vocabulary

20. seismograph
An instrument that records earthquake waves

21. seismograph
An instrument that records earthquake waves

22. seismogram
A record made by a seismograph

23. surface wave
A seismic wave that travels along the surface of Earth

24. P wave
Earthquake wave that pushes and pulls rocks in the direction of the wave, also known as a compression wave.

25. moment magnitude
A more precise measure of earthquake magnitude than the Richter scale

26. That’s Random

27. Measuring Earthquakes
The study of earthquake waves, or seismology, dates back almost 2000 years.
Seismographs – instruments that record earthquake waves.
Seismogram – modern seismographs that amplify and electronically record ground motion.

28. Earthquake Waves
The energy from an earthquake spreads outward as waves in all directions from the focus.
Seismograms show that two main types of seismic waves are produced by an earthquake – surface waves and body waves.

29. Earthquake Waves Surface Waves
Seismic waves that travel along Earth’s outer layer.

30. Earthquake Waves Body Waves
Waves that travel through the Earth’s interior
P waves – “push – pull” waves. The push (compress) and pull (expand) rocks in the direction the waves travel.
S waves – shake the particles at right angles to the direction of travel.

31. Earthquake Waves
A seismogram shows all three types of seismic waves – surface waves, P waves, and S waves.

32. Locating an Earthquake
The difference in velocities of P and S waves provides a way to locate the epicenter.

33. Locating an Earthquake
The winning car is always faster than the losing car. The P wave always wins the race, arriving ahead of the S wave.

34. Locating an Earthquake
Travel-time graphs from three or more seismographs can be used to find the exact location of an earthquake epicenter.

35. That’s Random

36. Ag Earth Science – Chapter 8.3
8.3 Vocabulary

37. tsunami
Japanese word for a seismic sea wave

38. liquefaction
soils and other unconsolidated materials saturated with water are turned into a liquid that is not able to support buildings

39. seismic gap
An area along a fault where there has not been any earthquake activity for a long period of time

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41. Seismic Vibrations
These factors include the intensity and duration of the vibrations, the nature of the material on which the structure is built, and the design of the structure.
Liquefaction - soils and other unconsolidated materials saturated with water are turned into a liquid that is not able to support buildings.

42. Tsunamis Tsunami – seismic sea wave
A tsunami triggered by an earthquake occurs where a slab of the ocean floor is displaced vertically along a fault.
A tsunami can also occur when the vibration of a quake sets an underwater landslide into motion.

43. Other Dangers
With many earthquakes, the greatest damage to structures is from landslides and ground subsidence, or the sinking of the ground triggered by vibrations.

44. Predicting Earthquakes
short-range predictions of earthquakes have not been successful.
Long-range forecasts give the probability of a certain magnitude earthquake occurring within years.

45. Predicting Earthquakes
Scientists study historical records and look for seismic gaps (area of fault where no activity has taken place for a long time).
Scientists don’t yet understand enough about how and where earthquakes will occur to make accurate long-term predictions.

46. That’s Random

47. Ag Earth Science – Chapter 8.4
8.4 Vocabulary

48. crust
The thin, rocky outer layer of the Earth

49. mantle
The 2890 km – thick layer of earth located below the crust

50. lithosphere
The rigid outer layer of earth including the crust and upper mantle

51. asthenosphere
A weak plastic layer of the mantle situated below the lithosphere

52. outer core
A layer beneath the mantle about 2260 km thick

53. inner core
The solid innermost layer of the earth, about 1220 km in diameter

54. Moho
It is the boundary separating the crust from the mantle, discernable by an increase in the velocity of seismic waves

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56. Layers Defined by Composition
Earth’s interior consists of three major zones defined by its chemical composition – the crust, mantle, and core.
Crust – the thin, rocky outer layer of Earth, is divided into oceanic and continental crust.
Mantle – 82%+ of the earth’s volume is contained in the mantle – a solid, rocky shell that extends to a depth of 2890 km.
Core – the core is a sphere composed of iron-nickel alloy

57. Layers Defined by Physical Properties
Earth can be divided into layers based on physical properties – the lithosphere, asthenosphere, outer core, and inner core.
Lithosphere – Earth’s outermost layer that is about 100 km in thickness. Consists of the crust and uppermost mantle.
Asthenosphere – lies beneath the lithosphere and is a softer, weaker layer due to it’s high temperature “waxy” texture.
The core is divided into the outer (liquid) core and inner (solid) core.

58. Discovering Earth’s Composition
Early seismic data and drilling technology indicate that the continental crust is mostly made of lighter, granitic rocks.
The crust of the ocean floor has a basaltic composition
Earth’s core is thought to be mainly dense iron and nickel, similar to metallic meteorites. The surrounding mantle is believed to be composed of rocks similar to stony meteorites.

59. That’s Random