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Was (wer) ist fault identification - 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
Animal identification
![[[Great frigatebird]] with a wing tag](https://commons.wikimedia.org/wiki/Special:FilePath/Wing tag Great Frigatebird.JPG?width=200 "[[Great frigatebird]] with a wing tag")
.jpg?width=200 "Mussels being tagged")
PROCESS DONE TO IDENTIFY AND TRACK SPECIFIC ANIMALS
List of animal identification methods; Animal Identification; Animal ID; Animal id; Livestock identification
Animal identification using a means of marking is a process done to identify and track specific animals. It is done for a variety of reasons including verification of ownership, biosecurity control, and tracking for research or agricultural purposes.
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.
