fault-finding program - ορισμός. Τι είναι το fault-finding program
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Τι (ποιος) είναι fault-finding program - ορισμός

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.
Medical findings         
COLLECTIVE PHYSICAL AND PSYCHOLOGICAL OCCURRENCES OF PATIENTS SURVEYED BY A MEDICAL DOCTOR
Medical finding
Medical findings will signify the collective physical and psychological occurrences of patients surveyed by a medical doctor. The survey is composed of physical examinations by the doctor's senses and simple medical devices, which build clinical findings.
fact-finding         
WIKIMEDIA DISAMBIGUATION PAGE
Fact finding; Factfinding; Fact-findings; Fact-finding (disambiguation)
A fact-finding mission or visit is one whose purpose is to get information about a particular situation, especially for an official group.
A UN fact-finding mission is on its way to the region.
ADJ: ADJ n

Βικιπαίδεια

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.