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Faults
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browse graphicThrough the study of faults and their effects, much can be learned about the size and recurrence intervals of earthquakes. Faults also teach us about crustal movements that have produced mountains and changed continents. Initially a section of Earth’s crust may merely bend under pressure to a new position. Or slow movement known as seismic creep may continue unhindered along a fault plane. However stresses often continue to build until they exceed the strength of the rock in that section of crust. The rock then breaks, and an earthquake occurs, sometimes releasing massive amounts of energy. The ensuing earth displacement is known as a fault. This slide set describes the mechanism and types of faulting. It illustrates a variety of fault expressions in natural and manmade features.

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Non-Digital Form: 35 mm slides; Faults Ordering Instructions: Product may be ordered from online store via: http://ols.nndc.noaa.gov/plolstore/plsql/olstore.prodspecific?prodnum=G01203-SLI-A0001 Custom Order Process: Contact Data Center

Ordering Instructions: Product may be downloaded via: http://www.ngdc.noaa.gov/nndc/struts/results?eq_1=10&t=101634&s=0&d=4&d=44 Custom Order Process: Contact Data Center

Ordering Instructions: Product may be ordered from onlinfe store via: http://ols.nndc.noaa.gov/plolstore/plsql/olstore.prodspecific?prodnum=G01268-CDR-A0001 Custom Order Process: Contact Data Center

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Access Constraints: None Use Constraints: None Distribution Liability: While every effort has been made to ensure that these data are accurate and reliable within the limits of the current state of the art, NOAA cannot assume liability for any damages caused by any errors or omissions in the data, nor as a result of the failure of the data to function on a particular system. NOAA makes no warranty, expressed or implied, nor does the fact of distribution constitute such a warranty.