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Earthquake breaking news, Minor World Earthquakes Magnitude -3.9

Minor earthquake: M3.2 quake has struck near Georgetown in Idaho

Posted by admin on September 10, 2025 0 Comments

Earthquake location 42.67S, -111.2847WA minor earthquake with magnitude 3.2 (ml/mb) was detected on Wednesday, 22 kilometers (14 miles) from Georgetown in Idaho. Date and time of earthquake in UTC/GMT: 10/09/25 / 2025-09-10 18:24:24 / September 10, 2025 @ 6:24 pm. Exact location of event, depth 5 km, -111.2847° West, 42.67° North. Id of earthquake: us7000qvaf. Event ids that are associated: us7000qvaf. The epicenter of the earthquake was roughly 5 km (3 miles) below the earth’s surface. The 3.2-magnitude earthquake was detected at 18:24:24 / 6:24 pm (local time epicenter).

Epicenter of the earthquake was 80 km (50 miles) from Preston (c. 5 200 pop). Nearest cities/city/towns to hypocenter/epicentrum was Preston (min 5000 pop). Close country/countries, United States (c. 310 233 000 pop) (That might be effected).

Earthquakes 3.0 to 4.0 are often felt, but only causes minor damage. There are an estimated 130,000 minor quakes in the world each year. In the past 24 hours, there have been one, in the last 10 days one, in the past 30 days one and in the last 365 days six earthquakes of magnitude 3.0 or greater that have been detected in the same area.

Did you feel the quake?

Were you asleep? Was it difficult to stand and/or walk? Leave a comment or report about shaking, activity and damage at your city, home and country. Read more about the earthquake, Location, Distances, Seismometer information, Date-Time, Parameters and details about this quake, reported near: 22 km NNE of Georgetown, Idaho. This information comes from the USGS Earthquake Notification Service.

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More information

Parameter Value Description
Magnitude 3.2 mb The magnitude for the event.
Longitude -111.2847° West Decimal degrees longitude. Negative values for western longitudes.
Latitude 42.67° North Decimal degrees latitude. Negative values for southern latitudes.
Depth 5 km Depth of the event in kilometers.
Place 22 km NNE of Georgetown, Idaho Textual description of named geographic region near to the event. This may be a city name, or a Flinn-Engdahl Region name.
Time 2025-09-10 18:24:24 Time when the event occurred. UTC/GMT
Updated 2025-09-10 19:03:24 Time when the event was most recently updated. UTC/GMT
Timezone offset 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 158 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 44 The total number of Number of seismic stations which reported P- and S-arrival times for this earthquake.
Horizontal Distance 0.665 Horizontal distance from the epicenter to the nearest station (in degrees).
Root Mean Square 0.41 sec The root-mean-square (RMS) travel time residual, in sec, using all weights.
Azimuthal Gap 75 The largest azimuthal gap between azimuthally adjacent stations (in degrees).
Magnitude Type ml The method or algorithm used to calculate the preferred magnitude for the event.
Event Type earthquake Type of seismic event.
Event ID us7000qvaf Id of event.
Event Code 7000qvaf An identifying code assigned by, and unique from, the corresponding source for the event.
Event IDS ,us7000qvaf, A comma-separated list of event ids that are associated to an event.

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