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In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust adjusts to the effects of the main shock. Large earthquakes can have hundreds to thousands of instrumentally detectable aftershocks, which steadily decrease in magnitude and frequency according ...
Aftershocks in the 3-4.8 magnitude range can be expected on average, according to the USGS, but some aftershock sequences are more energetic than others. What we know about NY, ...
Macroshock: Current across intact skin and through the body. Current from arm to arm, or between an arm and a foot, is likely to traverse the heart, therefore it is much more dangerous than current between a leg and the ground. This type of shock by definition must pass into the body through the skin.
"Aftershocks will continue in the days and weeks ahead, and they will decrease with time." ... But they are possible in any large body of water." ... said it was “a pretty dangerous situation
After large earthquakes, there is an expectation that aftershocks could occur in the hours and days that follow, but aftershocks from some of the strongest earthquakes in recorded United States ...
Electrical burn on hand. An electrical burn is a burn that results from electricity passing through the body causing rapid injury. Approximately 1000 deaths per year due to electrical injuries are reported in the United States, with a mortality rate of 3-5%.
Some 50 aftershocks have been felt as of Friday afternoon. For premium support please call: 800-290-4726 more ways to reach us
The passage of current from one part of the body to another, especially from arm to arm and therefore through the heart. By this definition, the magnitude of the current itself (in amperes) is the most important factor. In general, the greater the current, the more dangerous a shock is and the more likely it is to be lethal.