PREDICTING VOLCANIC ERUPTIONS

Scientists have no trouble figuring out where volcanoes are, but predicting a volcanic eruption is not as easy. There are many different methods and tools scientists use to try to predict when a volcano will erupt.

history * seismometer * tiltmeter * gas emissions * satellites * acoustic flow monitoring * links

HISTORY

 

The first thing scientists do is determine a volcano's eruption history. A volcano is classified as active, dormant or extinct based upon when it has last erupted.

  • Active volcanoes are in the process of erupting or show signs of eruption in the very near future.
  • Dormant volcanoes are "sleeping." This means they are not erupting at this time, but they have erupted in recorded history.
  • An extinct volcano has not erupted in recorded history and probably will never erupt again.
back to the top

SEISMOMETER

Next, scientists consider seismic (earthquake) activity as it is registered on a seismometer. A volcano will usually register some small earthquakes as the magma pushes its way up through cracks and vents in rocks as it makes its way to the surface of the volcano. As a volcano gets closer to erupting, the presure builds up in the earth under the volcano and the earthquake activity becomes more and more frequent.

back to the top

TILTMETER

Close-up view of a tiltmeter being installed

Scientists also have an instrument that they attach to the side of volcanoes. It is called a tiltmeter. A tiltmeter will detect small changes in the slope of a volcano because as a volcano is about to erupt, the earth may bulge or swell up a bit.

back to the top

GAS EMISSIONS

Mageik Volcano, Alaska

Another thing scientists look for is the amount and types of gasses that are emitted from a volcano. When a volcano is close to erupting, the gasses become more pronounced. There is a slight problem with depending upon only gas emissions to predict eruptions, however. Sometimes lava will leak up through the top of a volcano and harden quickly. This will trap gasses inside of a volcano. Therefore, no gasses may be seen just before an eruption. This type of data collection may be very dangerous for scientists because they have to go to the top of the volcano and the gasses are very poisonous.

back to the top

SATELLITES

Mt. Etna, Italy

Scientists also use satellites to try to predict eruptions. Satellites can record infrared radiation where more heat or less heat shows up as different colors on a screen. If a volcano is seeming to become hotter, then an eruption may be coming soon.

 

back to the top

ACOUSTIC FLOW MONITORING

Acoustic Flow Monitor

A more recent monitoring techique used by scientists is the Acoustic Flow Monitor (AFM). With this type of instrument, scientists use a seismometer to record sound waves within a volcano. It has been determined that as pressure builds up within the earth, sound waves can be recorded-and that the waves coming from inside of a volcano just before an eruption look like regularly formed sound waves more than eratic and jagged earthquake waves.

back to the top

LINKS

back to the top

Links

Creation of Volcanoes

Types of Volcanoes

Volcanic Eruptions

Effects of Volcanoes

Predicting Eruptions

 

site created by Maria-Kristina Smith, November 2002