Economic: Businesses and industries destroyed or disrupted, jobs lost, profit from tourism industry
Social: People killed, homes destroyed, fires, trauma, homelessness
Political: Government buildings and other important areas destroyed or disrupted, conflicts concerning government response, food shortages, insurance etc.
Responses to volcanic hazards
Preparedness: Risk assessment and mapping, community education and awareness, early warning systems, evacuation plans and drills
Monitoring and Prediction: Volcanic monitoring networks, remote sensing, research and scientific analysis
Emergency Response: Activation of emergency response plans, evacuation execution, provision of emergency shelters and supplies, temporary infrastructure
Recovery and Rehabilitation: Damage assessment, restoration of infrastructure, support services, review and refinement of plans
Mitigation: Land use controls, structural engineering, vegetative barriers
Factors considered in risk management
Frequency and magnitude of volcanic activity
Population density of areas near volcanoes
Economic impact of disruptions and damage
Primary effects of volcanic activity
Tephra
Pyroclastic Flows
Lava Flows
Volcanic Gases
Tephra
Material ejected by the volcano, varying in size from volcanic bombs (>64mm) to lapilli (2-64mm) and ash (<2mm)
Pyroclastic Flows
Very hot (>800 degrees Celcuis), gas charged, high velocity flows made up of gas and tephra, can flow at 700kmph, usually relatively close to the ground, wiped out the city of Pompeii in 79AD
Lava Flows
Streams of molten rock that pour or ooze from an erupting vent, erupted during either nonexplosive activity or explosive lava fountain
Volcanic Gases
Carbon dioxide
Carbon monoxide
Hydrogen sulphide
Chlorine
Secondary effects of volcanic activity
Lahars (volcanic mud flows)
Flooding
Volcanic landslide
Acid Rain
Climate Change
Lahars (volcanic mud flows)
Melted snow and ice as a result of the eruption combined with volcanic ash forms mud flows that can move down the course of river valleys at high speed
Volcanic eruption
Melts glaciers and ice caps, causing serious flooding
Volcanic landslide
Large masses of wet or dry rock and soil that fall, slide, or flow very rapidly under the force of gravity
Tsunamis
Sea waves generated by violent volcanic eruptions, such as those formed after Krakatoa in 1883, estimated to have killed 36,000 people
Acid Rain
Sulphur emitted from the volcano mixes with moisture in the atmosphere, causing acid rain
Volcanic eruption
Ejects huge amounts of debris into the atmosphere, reducing global temperatures by blocking out sunlight, resulting in climate change
Volcanic Hazards
Most volcanic activity is associated with plate tectonic processes and is mainly located along plate margins
Locations of volcanic activity
Oceanic Ridge
Subduction Zones
Rift Valleys
Hot Spots
Volcanic eruptions
Vary in both scale, frequency and magnitude
Types of volcanic eruptions
Effusive eruptions - magma rises through the surface and flows out of the volcano as a viscous liquid called lava
Explosive eruptions - magma is torn apart as it rises and reaches the surface in pieces known as pyroclasts
Volcanic Explosivity Index (VEI)
A logarithmic scale from 0-8, quiet eruptions score 1 and increase in number as the volcano becomes more explosive
A magnitude 7 has only been experienced in Tamboro, Indonesia (1815), so are relatively uncommon
Frequency of volcanic eruptions
The number of previous eruptions must be recorded and analysed
Primary effects of volcanic activity
Tephra - Material ejected by the volcano, varying in size from volcanic bombs (>64mm) to lapilli (2-64mm) and ash (<2mm)
Pyroclastic Flows - very hot (>800 degrees Celcuis), gas charged, high velocity flows made up of gas and tephra
Lava Flows - streams of molten rock that pour or ooze from an erupting vent
Lahars (volcanic mud flows): Melted snow and ice as a result of the eruption combined with volcanic ash forms mud flows that can move down the course of river valleys at high speed
Flooding - The heat of the eruption melts glaciers and ice caps, serious flooding can occur
Volcanic landslide - These are large masses of wet or dry rock and soil that fall, slide, or flow very rapidly under the force of gravity
Tsunamis - These are sea waves generated by violent volcanic eruptions
Acid Rain - Sulphur is emitted from the volcano, when this mixes with moisture in the atmosphere and acid rain occurs
Climate Change - The huge amounts of debris that can be ejected into the atmosphere can reduce global temperatures as they can block out sunlight
The frequency of volcanic eruptions depends largely upon their type
Kilauea, on the island of Hawaii
An active shield volcano which has erupted basaltic lava continuously since 1983
Yellowstone caldera
Has erupted three times in the last 2.1 million years, with an interval of between 600 000 and 800 000 years between each
Basaltic lava
Erupted from volcanoes at constructive plate boundaries and magma plumes
Volcanoes at destructive plate boundaries
Tend to erupt more viscous, andesitic or rhyolitic lava
Predicting volcanic eruptions
Vulcanologists need to know a volcano's eruption history and to be currently monitoring it, then interpret the data
It is impossible to predict the exact size, nature and timing of an eruption