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Signs of
Impending
Volcanic
Eruption
Volcanic earthquakes serve as an
early warning sign for an
impending eruption, as well as
well as a marker for the location
of a moving magma and sudden
rise of gases. Earthquakes are
caused by the magma breaking
through rocks or by moving
through rock cracks. On the other
hand, volcanic tremor is a long-
lasting rhythmic signal associated
with magma in motion that can
last for minutes or days.
Steam occurs mostly on active
volcanoes. Presence of steam
signals that magma is lying
relatively close to the surface of
the volcano. Steam is produced
when groundwater and magma or
any ignited fragment of rock
interacts. Meanwhile, ash is one of
the fragments of magma produced
when magma is ejected with great
force. Presence of ashes signals
that the magma is being ejected
violently.
Again, as the magma
rises, the
temperature of the
volcano also
increases. The heat
brought by the rising
magma influences
and causes the
temperature of the
springs, wells, or
lake to increase.
Development of
new thermal areas
and/or reactivation
of old ones signals
the active
movement of
magma within the
volcano as it
interacts with
groundwater or
rocks.
The parameters used to monitor volcanoes are:
1. Ground deformation – any surface changes on a
volcano (subsidence/sinking, tilting, bulging); often use of
tiltmeters as well as satellite imaging which results to less
exposure on the ground or safer for volcanologists. However,
interpretation needs field verification sometimes.
2. Seismic Activity – when magma rises up, it breaks rock
along the way. Thus, earthquakes are generated. Monitoring
of quakes/tremors is done by using a seismometer that
determines which patterns of seismic waves precede an
eruption.
The parameters used to monitor volcanoes are:
3. Gases – monitor types and rate of emission of different
gases; Concentrations of gases are sometimes high enough
to create acid rain that kills vegetation around the volcano;
collection of samples from vents directly with the use of
remote sensing instruments that identify and quantify the
present gases
The parameters used to monitor volcanoes are:
4. Sensory observations (by people living near volcano)
• Visual – intensified presence of steam; drying up of
vegetation, wells/spring/lake; crater glow at the mouth of
the volcano
• Auditory – rumbling sounds are heard.
• Olfactory – observed foul smell (usually rotten egg caused
by sulfur) caused by presence of volcanic gases
• Tactile – ground movement/earthquake is felt
impendingsignsofvolcaniceruption-230219211559-09c649c5.pdf

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impendingsignsofvolcaniceruption-230219211559-09c649c5.pdf

  • 2. Volcanic earthquakes serve as an early warning sign for an impending eruption, as well as well as a marker for the location of a moving magma and sudden rise of gases. Earthquakes are caused by the magma breaking through rocks or by moving through rock cracks. On the other hand, volcanic tremor is a long- lasting rhythmic signal associated with magma in motion that can last for minutes or days.
  • 3. Steam occurs mostly on active volcanoes. Presence of steam signals that magma is lying relatively close to the surface of the volcano. Steam is produced when groundwater and magma or any ignited fragment of rock interacts. Meanwhile, ash is one of the fragments of magma produced when magma is ejected with great force. Presence of ashes signals that the magma is being ejected violently.
  • 4.
  • 5.
  • 6.
  • 7.
  • 8. Again, as the magma rises, the temperature of the volcano also increases. The heat brought by the rising magma influences and causes the temperature of the springs, wells, or lake to increase.
  • 9.
  • 10.
  • 11. Development of new thermal areas and/or reactivation of old ones signals the active movement of magma within the volcano as it interacts with groundwater or rocks.
  • 12. The parameters used to monitor volcanoes are: 1. Ground deformation – any surface changes on a volcano (subsidence/sinking, tilting, bulging); often use of tiltmeters as well as satellite imaging which results to less exposure on the ground or safer for volcanologists. However, interpretation needs field verification sometimes. 2. Seismic Activity – when magma rises up, it breaks rock along the way. Thus, earthquakes are generated. Monitoring of quakes/tremors is done by using a seismometer that determines which patterns of seismic waves precede an eruption.
  • 13. The parameters used to monitor volcanoes are: 3. Gases – monitor types and rate of emission of different gases; Concentrations of gases are sometimes high enough to create acid rain that kills vegetation around the volcano; collection of samples from vents directly with the use of remote sensing instruments that identify and quantify the present gases
  • 14. The parameters used to monitor volcanoes are: 4. Sensory observations (by people living near volcano) • Visual – intensified presence of steam; drying up of vegetation, wells/spring/lake; crater glow at the mouth of the volcano • Auditory – rumbling sounds are heard. • Olfactory – observed foul smell (usually rotten egg caused by sulfur) caused by presence of volcanic gases • Tactile – ground movement/earthquake is felt