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Moderate earthquake: M5.2 quake has struck near Visokoi Island in South Georgia and the South Sandwich Islands

Posted by admin on August 20, 2016 0 Comments

Earthquake location -55.2223S, -31.1955WA moderate earthquake with magnitude 5.2 (ml/mb) was detected on Saturday, 298 km WNW of Visokoi Island, South Georgia and the South Sandwich Islands (185 miles). Exact location, longitude -31.1955° West, latitude -55.2223° South, depth = 33.8 km. A tsunami warning has not been issued (Does not indicate if a tsunami actually did or will exist). The earthquake occurred at a depth of 33.8 km (21 miles) below the earth’s surface. Global time and date of event 20/08/16 / 2016-08-20 20:23:11 / August 20, 2016 @ 8:23 pm UTC/GMT. The 5.2-magnitude earthquake was detected at 18:23:11 / 6:23 pm (local time epicenter). All ids that are associated to the event: us10006fh0. Unique identifier: us10006fh0.

In the past 24 hours, there have been nine, in the last 10 days twenty-one, in the past 30 days twenty-one and in the last 365 days twenty-one earthquakes of magnitude 3.0 or greater that was reported nearby. Earthquakes 5.0 to 6.0 may cause light damage to buildings and other structures. Each year there are an estimated 1320 moderate quakes in the world.

Did you feel it?

How did you react? Was there any damage to buildings? Leave a comment or report about shaking, activity and damage at your home, city and country. This data comes from the USGS Earthquake Notification Service. Read more about the earthquake, Seismometer information, Distances, Parameters, Date-Time, Location and details about this quake, that has occurred near: 298 km WNW of Visokoi Island, South Georgia and the South Sandwich Islands.

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More information

Parameter Value Description
Magnitude 5.2 mb The magnitude for the event.
Longitude -31.1955° West Decimal degrees longitude. Negative values for western longitudes.
Latitude -55.2223° South Decimal degrees latitude. Negative values for southern latitudes.
Depth 33.8 km Depth of the event in kilometers.
Place 298km WNW of Visokoi Island, South Georgia and the South Sandwich Islands Textual description of named geographic region near to the event. This may be a city name, or a Flinn-Engdahl Region name.
Time 2016-08-20 20:23:11 Time when the event occurred. UTC/GMT
Updated 2016-08-20 20:41:32 Time when the event was most recently updated. UTC/GMT
Timezone offset -120 Timezone offset from UTC in minutes at the event epicenter.
Felt The total number of felt reports
CDI The maximum reported intensity for the event.
MMI The maximum estimated instrumental intensity for the event.
Alert Level The alert level from the PAGER earthquake impact scale. Green, Yellow, Orange or Red.
Review Status reviewed Indicates whether the event has been reviewed by a human.
Tsunami 0 This flag is set to "1" for large events in oceanic regions and "0" otherwise. The existence or value of this flag does not indicate if a tsunami actually did or will exist.
SIG 416 A number describing how significant the event is. Larger numbers indicate a more significant event.
Network us The ID of a data contributor. Identifies the network considered to be the preferred source of information for this event.
Sources ,us, A comma-separated list of network contributors.
Number of Stations Used The total number of Number of seismic stations which reported P- and S-arrival times for this earthquake.
Horizontal Distance 3.208 Horizontal distance from the epicenter to the nearest station (in degrees).
Root Mean Square 1.24 sec The root-mean-square (RMS) travel time residual, in sec, using all weights.
Azimuthal Gap 54 The largest azimuthal gap between azimuthally adjacent stations (in degrees).
Magnitude Type mb The method or algorithm used to calculate the preferred magnitude for the event.
Event Type earthquake Type of seismic event.
Event ID us10006fh0 Id of event.
Event Code 10006fh0 An identifying code assigned by, and unique from, the corresponding source for the event.
Event IDS ,us10006fh0, A comma-separated list of event ids that are associated to an event.

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