3.1.5.3 - Volcanic Hazards Flashcards
How are volcanoes formed at oceanic ridges and what is a key example of this
When the plates move apart magma forces its way up to the surface where it cools and forms a new crust - as the plates move the new crust moves further away
- Eyjafjallajokull
How volcanoes formed on or near subduction zones, why are the volcanoes viscous and explosive and what is an example where lots occur
- the heat generated from the inside of the earth and from the friction between the two plates causes the oceanic plate to melt.
- as its less dense it rises as plutons of magma until reaching the surface and forms volcanoes
- andesitic lava causes viscous and explosive volcanoes
- e.g. ring of fire
How are volcanoes formed at rift valleys and a key example
- when the continental plates move apart areas of the brittle crust drop between forming rift valleys
- this crust is thinner meaning magma can force its way to the surface easily forming volcanoes
- e.g. Mount Nyrigongo
What are hot spots, how do they cause volcanoes and a key example
- = concentration of radioactive elements
- causes plumes of magma to rise and eat into the plate above
- when the magma breaks through, active volcanoes form above the spot
- plates moves along the hot spot forming a chain of islands e.g. Hawaiian islands
Why are volcanoes formed at hot spots cause shield volcanoes and how have the old volcanoes been reduced to seamounts
- basaltic lava flows slowly and forms huge flattish volcanoes = shield volcanoes
- due to marine erosion and subsidence caused by the pressure the volcanoes puts on the crust
Where are three key places that volcanoes are found
- ring of fire (surrounding pacific ocean)
- Rift in Africa
- Hawaiian hot spots
What is used to measure the magnitude of volcanoes and what is used to determine the magnitude
- volcanic explosivity index
- the volume of erupted material
How can volcanologists track the frequency of a volcanoes eruption
- a volcanoes previous history of activity is tracked using deposits associated with the volcano and how old or deep they are
What are 6 ways volcanologists can predict when a volcano is going to erupt or close to erupting
- monitor land swelling - could mean magma is moving to the main chamber
- changes in the groundwater levels - if groundwater levels rise then magma could be forcing its way toward the surface
- chemical composition of groundwater - poisonous gases can seep from the ground, water can get hotter so thermal monitoring is used
- Shock waves caused from magma moving towards the surface
- mass movements like landslides suggests upwelling of magma
- magma movement can be tracked using magnometres
What are 3 ways we can protect from volcanoes
- monitoring allows for prediction which allows for evacuation
- studying the nature and extent of deposits from lahars and lavas which allow to identify places at great risk and therefore influence land use planning
- viscous lava can be diverted through digging trenches or splashing seawater on it to solidify it
What are the 4 primary effects of volcanoes and how do they impact people
- tephra = solid material of varying grain size (vary from volcanic bombs to ash) - climate change, aviation, breathing issues
- pyroclastic flows = very hot, gas charged flows containing a mixture of gas and tephra - can flow up to 700kmph so are a high cause of death as they hard to escape
- Lava flows - destroy buildings and can cause death
- Volcanic gases (e.g. CO2, carbon monoxide and Sulphur dioxide )- can cause climate change and acid rain
6 secondary effects of volcanoes and how do they occur
- Lahars (volcanic mud flows) = when snow or ice melts caused by an eruption and they combine with volcanic ash to form fast flowing mud flows
- Flooding - when an eruption causes glaciers or ice to melt
- Volcanic landslides - the shaking from the eruption causes rocks to move and mass movements to occur
- Tsunami’s - from violent eruptions the ground shakes causing a tsunami to occur
- Acid rain - Sulphur emitted from volcanic eruption combines with the moisture in the air
- Climate change - the emission of CO2 contributes to global warming
Case study
- Where is Mt Nyiragongo located, what is it associated with and when did it erupt
- Democratic republic of congo
- the african rift valley
- January 2002
Case study
- What were the 3 characteristics of the main crater of the volcano
- 250m deep
- 2km wide
- ‘lava lake’
Case study
What encouraged many people to settle down in Goma despite the risk of the volcano
It was a fertile agricultural region because :
- It has an extended growing season
- the volcanic soils are very fertile