volcanology unit 12 study guides

Key Eruptions Covered

• Mount St. Helens, USA (1980) catastrophic eruption that reshaped the surrounding landscape
• Nevado del Ruiz, Colombia (1985) devastating lahars caused by melting of summit glaciers
• Mount Pinatubo, Philippines (1991) second-largest volcanic eruption of the 20th century
• Eyjafjallajökull, Iceland (2010) disrupted air travel across Europe due to volcanic ash
• Mount Ontake, Japan (2014) sudden phreatic eruption caught hikers by surprise
• Kilauea, Hawaii (2018) Lower East Rift Zone eruption and summit caldera collapse

Geological Context

• Tectonic setting plays a crucial role in determining the type and frequency of volcanic eruptions
  • Convergent plate boundaries (subduction zones) are associated with explosive volcanism (Mount St. Helens, Mount Pinatubo)
  • Divergent plate boundaries (mid-ocean ridges, rift valleys) are characterized by effusive volcanism (Kilauea)
• Magma composition influences the style of eruption and the associated hazards
  • Silica-rich magmas (rhyolitic, dacitic) tend to be more viscous and prone to explosive eruptions
  • Mafic magmas (basaltic) are less viscous and often result in effusive eruptions with lava flows
• Volcanic edifice structure and stability can affect the course of an eruption
• Presence of glaciers or snow cover can lead to secondary hazards such as lahars (Nevado del Ruiz)
• Hydrothermal systems beneath volcanoes can contribute to phreatic eruptions (Mount Ontake)

Pre-Eruption Signs

• Increased seismicity indicates magma movement and potential unrest
  • Volcano-tectonic earthquakes result from rock fracturing due to magma intrusion
  • Long-period earthquakes are associated with fluid movement within the volcanic system
• Ground deformation caused by magma accumulation or pressure changes
  • Inflation of the volcanic edifice detected through GPS measurements or satellite interferometry
• Changes in gas emissions (sulfur dioxide, carbon dioxide) can signal magma ascent
• Thermal anomalies detected by satellite imagery suggest increased heat flow
• Alterations in hydrothermal activity, such as changes in hot spring temperature or composition
• Precursory phreatic explosions may occur as magma interacts with groundwater

Eruption Dynamics

• Explosive eruptions are driven by the rapid expansion of dissolved gases in the magma
  • Fragmentation of magma generates ash, pumice, and pyroclastic density currents (Mount St. Helens, Mount Pinatubo)
• Effusive eruptions involve the outpouring of lava with lower gas content
  • Lava flows can be basaltic (Kilauea) or more viscous, such as andesitic or dacitic flows
• Phreatomagmatic eruptions occur when magma interacts with water, resulting in explosive fragmentation (Eyjafjallajökull)
• Pyroclastic density currents are ground-hugging mixtures of hot ash, gas, and rock fragments that can travel at high speeds
• Lava domes form when viscous magma accumulates and piles up near the vent (Mount St. Helens)
• Volcanic ash can be transported long distances by prevailing winds, posing hazards to aviation and public health

Impact on Surrounding Areas

• Pyroclastic density currents can cause widespread destruction and loss of life in nearby communities (Mount St. Helens)
• Lahars (volcanic mudflows) can inundate valleys and cause catastrophic damage downstream (Nevado del Ruiz)
  • Lahars can be triggered by melting of glaciers or heavy rainfall on unconsolidated volcanic deposits
• Ash fall can disrupt transportation, damage infrastructure, and affect agriculture and livestock
• Volcanic gases (sulfur dioxide, hydrogen fluoride) can lead to air pollution and acid rain, impacting ecosystems and human health
• Lava flows can destroy property and infrastructure in their path (Kilauea)
• Volcanic ash and aerosols can cause short-term climate cooling by blocking solar radiation (Mount Pinatubo)

Human Response and Evacuation

• Timely evacuations are critical in saving lives during volcanic crises
  • Establishing and communicating evacuation zones based on hazard assessments
  • Providing shelters and resources for displaced populations
• Monitoring and early warning systems help detect signs of unrest and impending eruptions
  • Seismic networks, GPS stations, gas measurements, and satellite observations
• Effective communication between scientists, authorities, and the public is essential for risk reduction
• Challenges in evacuation efforts include public perception of risk, logistical constraints, and socioeconomic factors
• Long-term relocation and resettlement may be necessary for communities in high-risk areas (Montserrat)

Scientific Observations and Lessons Learned

• Each eruption provides valuable data and insights into volcanic processes and hazards
  • Studying deposit characteristics helps reconstruct eruption dynamics and improve hazard models
• Multidisciplinary approaches combining geophysical, geochemical, and remote sensing techniques enhance understanding
• Importance of real-time monitoring and data analysis for timely decision-making during crises
• Collaboration between volcanologists, emergency managers, and local authorities is crucial for effective risk management
• Incorporating local knowledge and cultural perspectives in risk communication and evacuation planning
• Continuously refining and updating hazard maps and emergency response plans based on new scientific findings

Long-Term Consequences

• Landscape changes due to ash deposition, lava flows, and pyroclastic density currents
  • Destruction of ecosystems and subsequent ecological succession (Mount St. Helens)
• Economic impacts on tourism, agriculture, and infrastructure in affected regions
• Chronic health issues related to prolonged exposure to volcanic ash and gases
• Social and psychological effects on communities displaced by eruptions
• Opportunities for geothermal energy development in volcanic areas
• Enhanced public awareness and education about volcanic hazards and preparedness
• Strengthening of international cooperation and knowledge sharing in volcanology research and risk management