Volcanic Activity Monitoring and Prediction Notes
The Science of Prediction
Monitoring Volcanic Activity
- Signs of Volcanic Activity: Scientists monitor five key indicators:
- Eruption History: Historical data on past eruptions helps predict future activity.
- Volcanic Gases: Changes in gas composition can signal imminent eruptions.
- Heat and Hydrothermal Activity: Elevated temperatures may indicate moving magma.
- Earthquakes: Increased seismic activity is often a precursor to eruptions.
- Ground Deformation: Changes in the shape of the volcano can indicate magma movement.
- Observation Tools: Various instruments are used for monitoring volcanoes, often set up to operate autonomously due to the danger of eruptions.
- Transmission of Data: Tools typically transmit data via radio signals to a field office or a Volcano Observatory.
- U.S. Volcano Observatories: Includes five main locations operated by USGS and other organizations:
- Alaska Volcano Observatory (AVO)
- Hawaiian Volcano Observatory (HVO)
- Cascades Volcano Observatory (CVO), Washington
- Long Valley Observatory (LVO), California
- Yellowstone Volcano Observatory (YVO), Montana
Examples of Eruptions
- Mt. St. Helens: Erupted on May 18, 1980, where extensive monitoring helped save lives. This includes:
- April 1980 monitoring that led to preparedness for the eruption.
- Historical data supports the notion: “The Past is the Key to the Present.”
Types of Eruptions
- Ash, Gas, and Steam Eruptions:
- Caused by the release of trapped gases and steam.
- Often detected by surface earthquakes and changes in gas levels.
- Lava Flows:
- Occur when magma leaks from the volcano.
- Detected through shallow earthquakes and gas measurements.
- Pyroclastic Flows:
- Superheated gases that flow down the volcano, often following landslides.
- 1980 eruption of Mt. St. Helens caused significant ecological damage.
- Hydrothermal Explosions:
- When steam escapes, potentially creating craters without magma.
Volcanic Gases
- Role of Gases: Provide energy for eruptions; dissolved gases escape as magma rises or erupts.
- Types of Gases Measured:
- Carbon dioxide (CO2)
- Sulfur dioxide (SO2)
- Hydrogen sulfide (H2S)
- Detection:
- Spectrometers, sampling and laboratory analyses.
- Observing effects on vegetation and wildlife as indicators of gas emissions.
Hydrothermal Activity
- Process: Water infiltrates the ground, heated by magma, and can result in hot springs or geysers.
- Indications of Magma Presence: Thermal features like soil temperatures or surface alterations monitored through various methods:
- Aerial observations
- FLIR thermal imaging
- Direct temperature measurements
Seismic Activity
- Earthquake Generation:
- Caused by moving magma that reduces density, leading to pressure release.
- Measurement:
- Seismometers detect ground vibrations; patterns indicate magma movement.
- Volcanic tremors provide information on magma’s behavior.
- Historic Patterns:
- Before the 1980 eruption, numerous magnitude >3.5 earthquakes were recorded daily.
- Shape Changes: Volcanoes may inflate (bulge) or deflate (sink) due to gas or magma presence.
- Measurement Methods:
- Tiltmeters track angle changes in the volcano.
- GPS measurements determine shifts over time.
- Case Study: Between March and May 1980, Mt. St. Helens exhibited significant bulging, leading to its catastrophic eruption.
Volcanic Alert Levels
- Normal: Typical background activity.
- Advisory: Elevated unrest; monitored closely.
- Watch: Increased potential for eruptions, some minor activity may be occurring.
- Warning: Hazardous eruption in progress or imminent, requiring immediate attention.