United Nations expert weighs the earthquake that shook New England

The 3.8 -sized earthquake chanting the Maine coast on Monday morning throughout the New Hampshire Sikwist region and felt southern Boston and parts of the coastal island of Rod Conette. The earthquake center was less than 10 kilometers southeast of York Port, Min.

Sophie Kulson, professor of geophysics in the Department of Earth Sciences in the Department of Earth Sciences, says that it is the unique makeup of the Land mass in New England that allowed antiquities far from the earthquake center.

“Where are we, surrounded by volcanic rocks like granite, which are very dense and very highly sound. So they already allow the shaking of the earthquake waves to spread through longer distances before the energy fades,” says Colleson. “This energy does not dissipate as quickly as possible in other regions because we are on this solid ground.”

Earthquakes of this size are not necessarily common in New England, but they are not completely anomaly. Kulson says we usually test an earthquake of this size every five years or so in the region, noting that New Jersey witnessed a similar one last year. Often there is much smaller that occurs between these cases, but it is usually around the size of 2 or less and is not felt.

Kulson indicated that the last 3.8 earthquake, at least for the strike in Mine's state, occurred in Holly in 2012.

Collson says earthquakes occur along the mistakes, which are the weakening aircraft in advance. And the New England coincides with being home to many. It was created when the Apalashian Mountains were formed several hundreds of millions, although Colorson says they “may not have been very active for a long time.”

When stress or pressure accumulates in those areas, they suffer from rupture with the transformation of rocks, which creates an earthquake.

“The most likely candidate causes this process is a large -scale tectonic process,” says Kulson. “In the Atlantic Ocean, you have a series of hills in the middle of the Atlantic Ocean, where two tecton paintings are already. From stress or pressure near the place we are in New Hampshire.

The United Nations Earth Sciences Department contains an earthquake located in James Hall's cellar, primarily for teaching purposes, which recorded the earthquake activity. This earthquake scale is connected to the Raspberry Shake network, a global seismic control network (such as Waze earthquake, which includes inputs of professional seismologists, amateurs, teachers and students), and the United Nations data was shared with that network.

Colleson says that the site of the earthquake center abroad and not on the ground can provide some learning opportunities, because “it can give us an insight into what is there.”

Although external data was historically difficult to follow, general tectonic trends were not. Do we have to be looking for more frequent earthquakes in the region?

“These paintings were almost at the same rate for tens of millions of years, and we are talking to millimeters annually, so I don't think this is a sign of the presence of things like this becoming more frequent,” says Colleson.

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