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Teacher Answer Key - California Academy of Sciences
Teacher Answer Key - California Academy of Sciences

... How are these fossils evidence of plate movement? Explain your reasoning. Answers will vary. Since mesosaurs are reptiles that couldn’t swim across an entire ocean, they must have lived when the two continents were one. South America and Africa then split due to plate movement, so we find different, ...
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Earthquakes! - Westerville City Schools

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8th grade Science Study Guide – Earthquakes

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What Causes EARTHQUAKES?

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Earthquakes PowerPoint
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Characteristics of Earthquakes Located In the Magadi Area, Kenya

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... To determine the location of an epicenter, scientists determine the difference between the arrival times of the P-wave and S- wave. The farther away an earthquake is, the greater the time between the arrival of the P-wave and the S-wave. By drawing at least three circles using data from different se ...
4.1 KEY CONCEPT SUMMARY Earthquakes occur along faults.
4.1 KEY CONCEPT SUMMARY Earthquakes occur along faults.

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Chapter 5: Earthquakes

... a specific point. The focus of an earthquake is the point at which a rock beings to move, causing an earthquake. • An earthquake is the shaking and trembling that results form movement of rock beneath Earth’s surface. – Some can be unnoticed, some can cause the earth to break open, shift mountains a ...
Earthquakes
Earthquakes

... 1. What are the two factors that geologists take into account when they determine earthquake risk? 2. The risk of earthquakes is highest in the United States along the ___________ coast. 3. What kinds of damage are caused by the severe shaking of an earthquake? ...
Chapter 6 Review – Earthquakes
Chapter 6 Review – Earthquakes

... If the statement is true, write true. If it is false, change the underlined word or words to make the statement true. 1. Liquefaction forces squeeze or pull the rock in Earth’s crust. 2. Rock uplifted by normal faults creates fault-block mountains. 3. An earthquake’s epicenter is located deep underg ...
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Earthquake



An earthquake (also known as a quake, tremor or temblor) is the perceptible shaking of the surface of the Earth, which can be violent enough to destroy major buildings and kill thousands of people. The severity of the shaking can range from barely felt to violent enough to toss people around. Earthquakes have destroyed whole cities. They result from the sudden release of energy in the Earth's crust that creates seismic waves. The seismicity, seismism or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time.Earthquakes are measured using observations from seismometers. The moment magnitude is the most common scale on which earthquakes larger than approximately 5 are reported for the entire globe. The more numerous earthquakes smaller than magnitude 5 reported by national seismological observatories are measured mostly on the local magnitude scale, also referred to as the Richter magnitude scale. These two scales are numerically similar over their range of validity. Magnitude 3 or lower earthquakes are mostly almost imperceptible or weak and magnitude 7 and over potentially cause serious damage over larger areas, depending on their depth. The largest earthquakes in historic times have been of magnitude slightly over 9, although there is no limit to the possible magnitude. The most recent large earthquake of magnitude 9.0 or larger was a 9.0 magnitude earthquake in Japan in 2011 (as of March 2014), and it was the largest Japanese earthquake since records began. Intensity of shaking is measured on the modified Mercalli scale. The shallower an earthquake, the more damage to structures it causes, all else being equal.At the Earth's surface, earthquakes manifest themselves by shaking and sometimes displacement of the ground. When the epicenter of a large earthquake is located offshore, the seabed may be displaced sufficiently to cause a tsunami. Earthquakes can also trigger landslides, and occasionally volcanic activity.In its most general sense, the word earthquake is used to describe any seismic event — whether natural or caused by humans — that generates seismic waves. Earthquakes are caused mostly by rupture of geological faults, but also by other events such as volcanic activity, landslides, mine blasts, and nuclear tests. An earthquake's point of initial rupture is called its focus or hypocenter. The epicenter is the point at ground level directly above the hypocenter.
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