fault$27581$ - traduzione in olandese
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fault$27581$ - traduzione in olandese

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

fault      
v. aanmerkingen maken op, vitten op
fault tolerance         
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ABILITY OF A SYSTEM TO CONTINUE FUNCTIONING DESPITE ERRONEOUS INPUTS OR FAULTS WITHIN SOME OF ITS COMPONENTS
Fault-tolerance; Fault Tolerance; Graceful degradation; Failure-oblivious computing; Fault-tolerant; Fault-tolerant system; Fault tolerant systems; Fault tolerant designs; Fault-tolerant designs; Fault-tolerant systems; Graceful failure; Fail gracefully; Fault tolerant system; Fault tolerant design; Fail-safe (computer); Failure oblivious computing; Damage tolerant design; Degrade gracefully; Fault-tolerant computer system; Fail soft; Fail-soft operation; Fault-tolerant computer systems; Failure resistance; Fault-tolerant design; Fault tolerant; Fault-tolerant computing; Degrades gracefully; Failure tolerance; Single fault condition; Single Fault Condition
foutentolerantie, vermogen van een systeem om als gepland werkzaam te zijn ondanks interne of externe veranderingen
strict liability         
RESPONSIBILITY FOR CONSEQUENCES FROM ACTIVITY DESPITE ABSENCE OF FAULT OR CRIMINAL INTENT
Strictly liable; No-fault liability; No fault liability
burgerlijke aansprakelijkheid

Definizione

page 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.