| Arch 721, Structural Design for Dynamic Loads,
University of Virginia Copyright © 1996-2006 Kirk Martini. 10-Oct-2007 10:09 |
Table
of Contents |

[Bolt
78, p. 14]
A model of underground shocks associated with the 1994 Northridge earthquake in Los Angeles (from the Southern California Earthquake Center).
[SCEC 1996,
/animation.html]
A structure which straddles a fault rupture will almost surely be destroyed, but that probablity is very low.
The ground shaking induced by fault rupture causes much more widespread damage.
The nature of shaking at a particular site depends on many factors concerning the nature and distance of the origin of the earthquake and the surrounding geology.

[Bolt
78, p. 32]
Waves propogate through the earth's crusts in several forms. P waves and S waves are most prominent.

[Bolt
78, p. 29]
In addition to fault rupture and ground shaking, shaking can also induce tidal waves, called tsunamis. (from the Cornell Theory Center)
[CTC 1996,
/~devine/tsunami.html]
| Next: Measuring Earthquakes |
| Arch 721, Structural Design for Dynamic Loads,
University of Virginia Copyright © 1996-2006 Kirk Martini. 10-Oct-2007 10:09 |
Table
of Contents |