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Was (wer) ist systained fault - definition
SMALL STEP OR OFFSET ON THE GROUND SURFACE WHERE ONE SIDE OF A FAULT HAS MOVED VERTICALLY WITH RESPECT TO THE OTHER
Fault Scarp; Fault escarpment
Electrical fault
ABNORMAL ELECTRIC CURRENT
Asymmetric fault; Symmetric fault; Transient fault; Persistent fault; Fault current; Electrical faults; Prospective fault current; Earth fault; Restricted earth fault; Fault (electric); Ground Fault; Ground fault; SLGF; Single line to ground fault; Line to line fault; Double line to ground fault; DLGF; Double line-to-ground fault; Line-to-line fault; Bolted fault; Line-to-ground fault; Single line-to-ground fault; Fault (power engineering); Through fault; Incipient fault; Internal fault
In an electric power system, a fault or fault current is any abnormal electric current. For example, a short circuit is a fault in which a live wire touches a neutral or ground wire.
Humboldt Fault
CLASS C IN KANSAS
Humboldt fault; Humboldt Fault Zone
The Humboldt Fault or Humboldt Fault Zone, is a normal fault or series of faults, that extends from Nebraska southwestwardly through most of Kansas.from the Kansas Geological Survey (at the University of Kansas) site, oil geology page, accessed on December 16, 2006
page fault
WHEN A RUNNING PROGRAM ACCESSES A MEMORY PAGE THAT IS NOT CURRENTLY MAPPED BY THE MMU INTO THE VIRTUAL ADDRESS SPACE OF A PROCESS
Invalid page fault; Pagefault; Hard fault
<memory management> In a paged virtual memory system, an
access to a page (block) of memory that is not currently
mapped to physical memory. When a page fault occurs the
operating system either fetches the page in from {secondary
storage} (usually disk) if the access was legitimate or
otherwise reports the access as illegal.
(1995-11-11)
Wikipedia
Fault scarp
A fault scarp is a small step or offset on the ground surface where one side of a fault has moved vertically with respect to the other. It is the topographic expression of faulting attributed to the displacement of the land surface by movement along faults. They are exhibited either by differential movement and subsequent erosion along an old inactive geologic fault (a sort of old rupture), or by a movement on a recent active fault.
