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Earthquakes are recorded by a seismographic network. Each seismic station in the network measures the movement of the ground at that site. The slip of one block of rock over another in an earthquake releases energy that makes the ground vibrate. That vibration pushes the adjoining piece of ground and causes it to vibrate, and thus the energy travels out from the earthquake hypocenter in a wave.
There are many different ways to measure different aspects of an earthquake:
Magnitude is the most common measure of an earthquake's size. It is a measure of the size of the earthquake source and is the same number no matter where you are or what the shaking feels like. The Richter scale is an outdated method for measuring magnitude that is no longer used by the USGS for large, teleseismic earthquakes. The Richter scale measures the largest wiggle (amplitude) on the recording, but other magnitude scales measure different parts of the earthquake. The USGS currently reports earthquake magnitudes using the Moment Magnitude scale, though many other magnitudes are calculated for research and comparison purposes.
Intensity is a measure of the shaking and damage caused by the earthquake; this value changes from location to location
Explanation:
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Answer:
The Monroe Doctrine had originally been intended to keep European nations out of Latin America, but the Roosevelt corollary was used as a justification for U.S. intervention in Latin America.
Involvement in Vietnam was due to the United States policy of containment, which is the attempt to spread the effect of communism. This was because the US believed in something known as the domino effect, which was the notion that if one country fell to communist rule, surrounding countries would follow suit.
B: American law enforcement using torture during interrogations. Its against the constitution therefore unconstitutional.
Answer:
An apple, potato, and onion all taste the same if you eat them with your nose plugged
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