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For presenting the key data of an earthquake in a consistent, standardized format. Template parameters This template prefers block formatting of parameters. Parameter Description Type Status name name no description Unknown suggested title title no description Unknown optional native_name native_name no description Unknown optional native_name_lang native_name_lang no description Unknown ...
In most cases there is an initial report within 10 to 30 minutes of all magnitude 5.0+ earthquakes globally, and magnitude 4.0+ earthquakes within the contiguous U.S. Note that the magnitudes and locations in the initial reports are only first-order approximations, which get revised in the following hours, days, and months.
[[Category:Earthquake templates]] to the <includeonly> section at the bottom of that page. Otherwise, add <noinclude>[[Category:Earthquake templates]]</noinclude> to the end of the template code, making sure it starts on the same line as the code's last character.
There is a greater than 99% probability of one or more magnitude 3.0 earthquakes in the area over the next day, a 74% chance of a magnitude 4.0 or larger, 22% chance of a magnitude 5.0 and larger ...
Aftershocks can be distinguished in part by starting immediately following a main shock, but usually about 1.2 magnitude smaller, and rapidly decaying in magnitude and frequency (see Bath's Law, whereas doublet/multiplet events are usually only a few events of roughly the same magnitude, separated by hours, days, or even weeks.
In most cases there is an initial report within 10 to 30 minutes of all magnitude 5.0+ earthquakes globally, and magnitude 4.0+ earthquakes within the contiguous U.S. Note that the magnitudes and locations in the initial reports are only first-order approximations, which get revised in the following hours, days, and months.
A 2.8 magnitude earthquake shook the Richmond, Virginia area Tuesday afternoon, according to the United States Geological Survey.. The quake struck about six miles northwest of Glen Allen ...
Originally intended for estimating the magnitude of historic earthquakes where seismic data is lacking but tidal data exist, the correlation can be reversed to predict tidal height from earthquake magnitude. [63] (Not to be confused with the height of a tidal wave, or run-up, which is an intensity effect controlled by local topography.) Under ...