According to experts with the US Geological Survey, the latest swarm began on February 8 in a region roughly eight miles northeast of West Yellowstone, Montana – and, it’s increased dramatically in the days since
© USGS volcanoesAccording to experts with the US Geological Survey, the latest swarm began on February 8 in a region roughly eight miles northeast of West Yellowstone, Montana – and, it’s increased dramatically in the days since
A new swarm of earthquakes has cropped up at the Yellowstone supervolcano, with more than 200 small temblors detected in the last 10 days alone.

According to experts with the US Geological Survey, the latest swarm began on February 8 in a region roughly eight miles northeast of West Yellowstone, Montana - and, it's increased dramatically in the days since.

But for now, scientists say there's no reason to worry.

While the earthquakes are likely caused by a combination of processes beneath the surface, the current activity is said to be 'relatively weak,' and the alert level at the supervolcano remains at 'normal.'

Yellowstone is home to several faults, and has a long history of seismic activity. As natural processes occur beneath the surface and 'stress effects' from past events continue to maintain their hold, the area remains a 'hotbed of seismicity and swarm activity,' according to USGS

On left, a map of Yellowstone earthquakes from 1973 – 2017 is shown, with red circles illustrating all of the quakes. Blue shows quakes that were part of swarms.
On left, a map of Yellowstone earthquakes from 1973 – 2017 is shown, with red circles illustrating all of the quakes. Blue shows quakes that were part of swarms.
The current swarm is shown on the right (red circles), compared to the location of last summer's swarm (gray)
The current swarm is shown on the right (red circles), compared to the location of last summer's swarm (gray)
According to the USGS, the new swarm is occurring in about the same location as the Maple Creek swarm last summer, which brought roughly 2,400 earthquakes in a four-month span.


The University of Utah Seismograph Stations picked up the first quakes just over a week ago, counting more than 200 as of February 18.

But, the experts say there are likely many more that have gone undetected.

'The present swarm started on February 8, with a few events occurring per day,' according to USGS.

'On February 15, seismicity rates and magnitudes increased markedly. As of the night of February 18, the largest earthquake in the swarm is M2.9, and none of the events have been felt. All are occurring about 8 km (5 mi) beneath the surface.'

Yellowstone is home to several faults, and has a long history of seismic activity.

As natural processes occur beneath the surface and 'stress effects' from past events continue to maintain their hold, the area remains a 'hotbed of seismicity and swarm activity,' according to USGS.

'Swarms reflect changes in stress along small faults beneath the surface, and generally are caused by two processes: large-scale tectonic forces, and pressure changes beneath the surface due to accumulation and/or withdrawal of fluids (magma, water, and/or gas),' USGS explains.


'The area of the current swarm is subject to both processes.'

The current activity, however, is likely no cause for worry.

As the experts explain, earthquake swarms are a common phenomenon at Yellowstone, and account for more than 50 percent of seismic activity at the park.

And in the past, they have not been linked to volcanic activity.

'While it may seem worrisome, the current seismicity is relatively weak and actually represents an opportunity to learn more about Yellowstone,' USGS explains.

'It is during periods of change when scientists can develop, test, and refine their models of how the Yellowstone volcanic system works.'

But, the experts also note: 'The earthquakes, too, serve as a reminder of an underappreciated hazard at Yellowstone - that of strong earthquakes, which are the most likely event to cause damage in the region on the timescales of human lives.'
Could an eruption be prevented?

Recent research found a small magma chamber, known as the upper-crustal magma reservoir, beneath the surface
© University of UtahThe traditional picture of a magma chamber needs a re-think
Recent research found a small magma chamber, known as the upper-crustal magma reservoir, beneath the surface

Nasa believes drilling up to six miles (10km) down into the supervolcano beneath Yellowstone National Park to pump in water at high pressure could cool it.

Despite the fact that the mission would cost $3.46 billion (£2.63 billion), Nasa considers it 'the most viable solution.'


Using the heat as a resource also poses an opportunity to pay for plan - it could be used to create a geothermal plant, which generates electric power at extremely competitive prices of around $0.10 (£0.08) per kWh.

But this method of subduing a supervolcano has the potential to backfire and trigger the supervolcanic eruption Nasa is trying to prevent.
This USGS graphic shows how a 'super eruption' of the molten lava under Yellowstone National Park would spread ash across the United States
This USGS graphic shows how a 'super eruption' of the molten lava under Yellowstone National Park would spread ash across the United States
'Drilling into the top of the magma chamber 'would be very risky;' however, carefully drilling from the lower sides could work.

This USGS graphic shows how a 'super eruption' of the molten lava under Yellowstone National Park would spread ash across the United States

Even besides the potential devastating risks, the plan to cool Yellowstone with drilling is not simple.

Doing so would be an excruciatingly slow process that one happen at the rate of one metre a year, meaning it would take tens of thousands of years to cool it completely.

And still, there wouldn't be a guarantee it would be successful for at least hundreds or possibly thousands of years.