CRITERIA FOR EARTHQUAKE RESISTANT CODE BOOK

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An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in size from those that are so weak that they cannot be felt to those violent enough to propel objects (and people) into the air, and wreak destruction across entire cities. The seismicity, or seismic activity, of an area is the frequency, type, and size of earthquakes experienced over a period of time. The word tremor is also used for non-earthquake seismic rumbling.

At the Earth's surface, earthquakes manifest themselves by shaking and displacing or disrupting 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.

1893 (MDCCCXCIII) was a common year starting on Sunday of the Gregorian calendar and a common year starting on Friday of the Julian calendar, the 1893rd year of the Common Era (CE) and Anno Domini (AD) designations, the 893rd year of the 2nd millennium, the 93rd year of the 19th century, and the 4th year of the 1890s decade. As of the start of 1893, the Gregorian calendar was 12 days ahead of the Julian calendar, which remained in localized use until 1923.

THE CODE BOOK EARTHQUAKE RESISTANT DESIGN OF STRUCTURES 

1893 PART -1  : 2002 


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