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Intensity is based on the observed effects of ground shaking on people, buildings, and natural
features. It varies from place to place within the disturbed region depending on the location of
the observer with respect to the earthquake epicenter.
Earthquakes are the result of forces deep within the Earth's interior that continuously affect the
surface of the Earth. The energy from these forces is stored in a variety of ways within the rocks.
When this energy is released suddenly, for example by shearing movements along faults in the
crust of the Earth, an earthquake results. The area of the fault where the sudden rupture takes
place is called the focus or hypocenter of the earthquake. The point on the Earth's surface
directly above the focus is called the epicenter of the earthquake.
Solution
Intensity is based on the observed effects of ground shaking on people, buildings, and natural
features. It varies from place to place within the disturbed region depending on the location of
the observer with respect to the earthquake epicenter.
Earthquakes are the result of forces deep within the Earth's interior that continuously affect the
surface of the Earth. The energy from these forces is stored in a variety of ways within the rocks.
When this energy is released suddenly, for example by shearing movements along faults in the
crust of the Earth, an earthquake results. The area of the fault where the sudden rupture takes
place is called the focus or hypocenter of the earthquake. The point on the Earth's surface
directly above the focus is called the epicenter of the earthquake.

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Intensity is based on the observed effects of ground shaking on peop.pdf

  • 1. Intensity is based on the observed effects of ground shaking on people, buildings, and natural features. It varies from place to place within the disturbed region depending on the location of the observer with respect to the earthquake epicenter. Earthquakes are the result of forces deep within the Earth's interior that continuously affect the surface of the Earth. The energy from these forces is stored in a variety of ways within the rocks. When this energy is released suddenly, for example by shearing movements along faults in the crust of the Earth, an earthquake results. The area of the fault where the sudden rupture takes place is called the focus or hypocenter of the earthquake. The point on the Earth's surface directly above the focus is called the epicenter of the earthquake. Solution Intensity is based on the observed effects of ground shaking on people, buildings, and natural features. It varies from place to place within the disturbed region depending on the location of the observer with respect to the earthquake epicenter. Earthquakes are the result of forces deep within the Earth's interior that continuously affect the surface of the Earth. The energy from these forces is stored in a variety of ways within the rocks. When this energy is released suddenly, for example by shearing movements along faults in the crust of the Earth, an earthquake results. The area of the fault where the sudden rupture takes place is called the focus or hypocenter of the earthquake. The point on the Earth's surface directly above the focus is called the epicenter of the earthquake.