edge-triggered - définition. Qu'est-ce que edge-triggered
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Qu'est-ce (qui) est edge-triggered - définition

Trigger earthquake; Triggered earthquake; Remotely triggered earthquake

Time-triggered architecture         
COMPUTER SYSTEM WITH PRE-DETERMINED TASK SCHEDULE
Draft:Time-Triggered system; Draft:Time-triggered system; TT system; TT embedded system; Time-triggered embedded system; Time-Triggered system; Time triggered system; Time-triggered system
Time-triggered architecture (abbreviated as TTA), also known as a time-triggered system, is a computer system that executes one or more sets of tasks according to a pre-determined and set task schedule.Pont, M.
Edge device         
ENTRY POINT INTO A COMPUTER NETWORK
Edge switch; Edge path adapter; Edge concentrator
An edge device is a device that provides an entry point into enterprise or service provider core networks. Examples include routers, routing switches, integrated access devices (IADs), multiplexers, and a variety of metropolitan area network (MAN) and wide area network (WAN) access devices.
Selwyn Edge         
  • Mills]] second from left
  • Gladiator]]
  • alt=Man sitting in open-top vehicle
  • Breaking the 24-hour distance record
BRITISH BUSINESSMAN AND RACING DRIVER (1868-1940)
Selwyn Francis Edge; S. F. Edge
Selwyn Francis Edge (1868–1940) was a British businessman, racing driver, cyclist and record-breaker. He is principally associated with selling and racing De Dion-Bouton, Gladiator; Clemént-Panhard, Napier and AC cars.

Wikipédia

Remotely triggered earthquakes

Remotely triggered earthquakes are a result of the effects of large earthquakes at considerable distance, outside of the immediate aftershock zone. The farther one gets from the initiating earthquake in both space and time, the more difficult it is to establish an association.

The physics of triggering an earthquake are complex. Most earthquake-generating zones are in a state of being close to failure. If such a zone were to be left completely alone, it would generate significant earthquakes spontaneously. Remote earthquakes, however, are in a position to disturb this critical state, either by shifting the stresses statically, or by dynamic change caused by passing seismic waves.

The first type of triggering may be due to static changes in the critical state. For example, after the magnitude 7.3 Landers earthquake struck California in 1992, it is said that "the earthquake map of California lit up like a Christmas tree". This event reinforced the idea of remotely triggered earthquakes, and pushed the hypothesis into the scientific mainstream. Following the very large 2004 Indian Ocean earthquake, it was established that remote earthquakes had been triggered as far away as Alaska.

There is scientific evidence for a "long reach", mainly in the form of discrete element modelling used in the mining industry. If rock is modeled as discrete elements in a critical state, a single disturbance can influence a wide area. A smaller-scale example is when a small excavation in a valley triggers a landslide and brings down a whole mountainside.