volcanic hazards Flashcards
describe the location of Eyjafjalljokull
It is located in the eastern volcanic zone in the south of Iceland which is situated between a constructive plate boundary between the north american plate and the eurasian plate.
As these plates moved apart the magma rises in the empty chamber
what caused the volcanic ash
- a second eruption occurred in April under an ice cap
- the interaction of magma and water caused rapid cooling which caused a plume of tephra which was over 10km high with spread east
effects of the eyjafjallajokul eruption
- tephra
- flooding due to the melting of the ice cap
- pyroclastic flows
hazards of a volcanic erruption
- tephra- ash ejected into the atmosphere
- nuees ardentes- very hot flows (800 degrees) of gas and tephra
- lava flows
economic impacts of the eyjafjalljokull volcanic eruption
- 100,000 flights were cancelled, causing delays all across the world (£130 million per day)
- Exporters of perishable goods were particularly affected such as Kenya as the fresh stock had to go to waste
- this is particularly damaging as the Kenyan economy is so reliant on the export of fresh goods
Why may the delay of flights be a good thing
- passengers looked for other ways to travel such a boat ride. these companies were better able to benefit
- they used more eco friendly methods of transport
preventing 3 million tonnes of carbon from being released
environmental impact of the eyjafjallajokul eruption
- ash from the volcano deposited iron into the North Atlantic Ocean causing a plankton boom
- this clouds the water and prevents the sunlight from entering the water
- preventing underwater vegetation from growing
- phytoplankton consume their nutrient and a further phytoplankton boom occurs
- without vegetation fish are less able to survive
- less fishing
- which is particularly damaging as the Icelandic economy is so reliant on fishing
social impacts of eyjafjallajokul
a study found that people after the eruption suffered form intense coughing and wheezing and eye and skin iritation
characteristics of basaltic lava
- effusive eruption
- low viscosity
- low silica content
- often flows greater than 10 km
- hotter than 1000 degrees
what type of volcanoes does basaltic lava form
shield volcanoes
what type of volcanoes does Andesitic lava form
composite
formation of composite volcanoes
- at subduction zones at destructive plate boundaries
- steep-sided cones formed from layers of pyroclastic flows. The thick lava cannot travel far down the slope of the volcano before it cools which makes the slopes of the volcano steeper
formation shield volcanoes
- form at constructive plate boundaries
- gently sloping sides as produce fast flowing basic (fluid) lava that can flow for many miles.
- Mount Kilauea is a named example of one
why is there a difference between lavas
the ocean floor contains different sediment. this can alter the silica content in the lave giving it different properties
characteristics of andesitic lava
- explosive erruption
- high viscosity
- high silica content
- flows less than 10km
- around 700 degrees