The “silent” earthquake that occurs under the Bay of Hook

A slow slippage event, also known as a “silent earthquake”, has been revealed in the Hawk Bay area since early May, causing about 2 cm from the eastern movement in the past two weeks.

This is the equivalent of about six months of intense panel movement to 14 days.

Unlike the usual earthquakes, these slow events occur for weeks or months instead of seconds.

ELISABETTA D'ANASTASI of GNS, said that the slow energy release means that it does not cause people or server.

“Instead, it is the working global satellite system (GNSS) stations that operate constantly (usually referred to as GPS) that follow the movement of the Earth at the level of millimeters on a daily basis, which allows us to see events like this reveals.”

De Anastasio said this type of activity was not unusual.

“When slow sliding events occur, it relieves a lot of pent -up stress on the boundaries of the integration plate. At the same time, it can increase tension on other parts close to the boundaries of the painting, so it is sometimes accompanied by an increase in the smaller earthquakes that the audience may feel.”

More than 100 earthquakes have been registered in the Central Hook Bay area since the beginning of May. (Source: GNS Science)

As a result, more than 100 earthquakes have been located in the Central Hook Bay area since the beginning of May. The biggest event was an earthquake of 3.1 on May 17.

De Anastasio said that slow sliding events were common in the Gulf of Gisporne and Hawk.

“The latest was reported in December last year abroad to the Jesborn region, between the Peninsula of Maq and the Tolga Bay – which lasted for a month.”

She said that the current event was captured between GNSS stations in Cape from the kidnappers and the semi -peninsula of Ma

“Based on our notes on the events of the Bast Hwke's Bay Slow-SLIP, this event is likely to continue in the next few weeks.”

While the slow sliding events did not pose a danger, D'Anastasio said it is a “major part” of an increased understanding on how tectonic panels in the integration area.

“If we can better understand slow events, we can better understand the earthquake capabilities of the integration areas.”

She said it is a “good reminder” of New Zealand's position that extends “the boundaries of a very active tectonic plate.”

“The best thing you can do now is to update yourself on the alert information of the earthquake. Our team will continue to monitor this slow activity, and we will keep your knowledge when the new data comes.”

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