natural hazards Flashcards
constructive plate boundaries
1) pressure release of plates moving apart causing the crust to melt
2) magma rises through the gap, forming a ridge
3) the ridge builds up as more magma rises through the gap, and is pushed down by gravity, pushing the plates further apart
4) over time, ridges can rise above sea level and form shield volcanoes
destructive plate boundaries
1) denser oceanic plate subducts under continental plate
2) friction between rough edges and the mantel builds up, which when released causes earthquakes
3)water from the crust and heat from the mantel causes the crust to melt, creating magma
4) magma rises and erupts out of the crust, and cools many times, eventually forming composite volcanoes
conservative plate boundaries
1) as plates move past each other, friction builds up, causing them to become stuck and building up pressure
2) eventually a crack forms and releases pressure in the form of an earthquake
3) there is no gap in between them, so magma cannot rise and form volcanoes
composite volcanoes features
- alternate layers of lava and ash
- tall, steep sided cone
- narrower base (lava doesn’t travel as far)
- andesitic lava - more viscous
- explosive eruptions
shield volcanoes features
- made from magma
- low, gentle sloping relief and wide base
- basaltic lava - more runny and travels further
- effusive eruptions (more gentle and frequent)
hotspots features
- formed by a plume of superheated rock rising through the mantel
- not formed at plate boundaries
- causes base of the lithosphere to melt, forming magma that rises through cracks in the crust
- ocean hotspots have basaltic lava, continental hotpots have andesitic lava
- mantle plumes fixed in place, so as plate moves, hotspot location moves away from volcano
pyroclastic flows
- mixture of hot steam, rock, ash and dust
- faster than a car, usually up to 20m
- death and severe injuries
lahars
- water + ash =mudflow
- high speeds and travels far
- often happens consecutively and with little warning
tephra
- ash and volcanic bombs
- tiny sharp fragments and big boulders (both cause injuries)
- from volcanin vents
volcanic gases
- particulates = cancer and global dimming
- sulphur dioxide = poisonous and acid rain
- carbon dioxide = global warming
earthquakes
- focus = where earthquake is released
- epicenter = point on the curst directly above the focus
- focal depth = distance between focus and epicenter
- seismic waves = released from focus, causing earthquakes
primary effects of volcanic eruptions
- homes/buildings damaged
- gas and electricity lines and sewage systems damaged
- deaths and injuries
- acid rain
secondary effects of volcanic eruptions
- farmer go bankrupt
- water supply will be contaminated by sewage, which means the spread of diseases
- homeless people
- insurance costs go up
- economy/trade suffers
- psychological trauma from deaths
management of volcanic eruptions
- monitoring and prediction = signs of eruptions (tremors, gases, changes in temperature, etc.)
- planning = evacuation strategies, education (drills, first aid), emergency shelters
- protection = evacuation, lava diversion channels, artificial lahar barriers
primary effects of earthquakes
- ground shaking
- damage to infrastructure
- deaths and injuries
- possible landslides