Volcanic Hazards Flashcards
How are volcanoes formed at destructive boundaries?
- Denser O plate is subducted and material melts
- Molten material is less dense and rises in the mantle and erupts at the surface
How are volcanoes formed at constructive boundaries?
- Plate diverge leaving a gap in the crust
- Magma rises due to low pressure and erupts
What are volcanoes at destructive boundaries like?
- Eruption of andesitic lava (high viscosity)
- Eruption of tephra
- Explosive eruptions (gas doesn’t escape as easily from the lava)
What are volcanoes at constructive boundaries like?
- Eruption of basaltic lava (low viscosity)
- Lava flows longs distances
- Effusive eruptions (gas escapes easily from the lava)
What are the primary hazards of a volcanic eruption?
- Tephra
- Pyroclastic flow
- Lava flow
- Volcanic gases
What is tephra?
Large fragments of ash and rock (volcanic bombs) ejected into the atmosphere
What is pyroclastic flow?
Gas and tephra collapses down the slopes of a volcano at up to 700 km/h
What are lava flows?
Lava pours from an erupting vent at constructive boundaries
What are volcanic gases?
Gases such as CO2, CO and SO2 escape during an eruption
What are the secondary hazards of a volcanic eruption?
- Lahars (mudflows)
- Flooding (jokulhlaup)
- Acid rain
What are lahars?
Volcanic material is mobilised by melting ice and snow and moves at up to 60 km/h
What is a jokulhlaup?
Serious flooding when an eruption takes place beneath glaciers and ice caps
What is acid rain?
SO2 combined with atmospheric moisture to produce acidic precipitation
What is the distribution of volcanoes?
- Plate boundaries and hotspots
- The Pacific Ring of Fire (high volcanic and seismic activity)
How can eruptions be defined?
- Explosive (high VEI)
- Effusive (low VEI)