Eyjafjallajokull, Iceland - April 2010
Population approx 338,000 (2018)
Capital city - Reykavik (not affected by the earthquake)
Sub-glacial strato-volcano (Eyjafijallajokull is the name of the glacier)
Anomaly - Iceland is on a constructive plate boundary - should be a effusive sheild volcano
Very well monitored volcanic location
15th April 2010 - activity detected since 20th March 2010
Iceland sits on Mid-Atlantic Ridge - constructive plate boundary - divergence of North America and Europe
Seismologists aware of increased activity from March - indicated magma was rising to surface
Magma chamber filled up - pressure increased inside volcano - magma started to rise from March 20th - caused significant lava flows - but then quietened down
More magma was rising in two weeks of less activity on surface - magma from mantle mixed with existing magma in magma chamber
Triggered chemical reactions - more gases created - resulted in explosive eruption
From 12th April lava was flowing from the magma chamber again - by 15th April vents below glacier were full of magma - glacier burst open melting glacier and causing extensive flooding
Hot magma meets freezing ice - creates huge plumes of tephra
Eruption lasted two weeks
Ash clouds up to 30,000 feet into air - tephra dispersed across local area - much of north-east Europe
International air travel was affected - hundreds of thousands of people displaced
Trade affected with cargo flights cancelled - Kenya lost $35 million due to fresh food decaying
Total cost to Europe - $2.8 billion in lost trade and insurance costs from cancelled flights
Caused less demand for air fuel - affected oil industry - stock marked shares in air travel companies fell
Flash floods from jokulhalups damaged fields and crops - 20 farms destroyed - evacuated
200m ice melted - damaged Route 1 - one of countries main roads
Secondary effect - ash covered ice - increased melting - dark surfaces absorb more heat - exacerbating flooding (positive feedback)
Volcano in sparsely populated area - no deaths or injuries - very little damage to property
Airspace closed to mitigate risk of aviation disaster - 100,000 flights cancelled - cost of more than $200 million per day
Iceland’s National Emergency Agency - mitigate risks
Co-ordinated very effective and immediate response
Damaged bridges immediately replaced with temporary structures - minimise impact on communication
No need for emergency aid - no injuries or damage to buildings
Iceland increased surveillance of area - public kept well informed about any changes in activity
Disruption caused chaos in London Heathrow - normally sees 1,200 flights in + out a day
700-800 people evacuated from their homes from area 25km east of capital
Volcano melted a glacier - caused massive flood
First volcano at Eyjafijallajokull glacier since 1823
Iceland’s first since 2004
Briefly forced 6000 from their homes
Millions of people stranded due to grounding thousands of flights
Low pressure system developed over Iceland - push ash towards the Arctic
Population approx 338,000 (2018)
Capital city - Reykavik (not affected by the earthquake)
Sub-glacial strato-volcano (Eyjafijallajokull is the name of the glacier)
Anomaly - Iceland is on a constructive plate boundary - should be a effusive sheild volcano
Very well monitored volcanic location
15th April 2010 - activity detected since 20th March 2010
Iceland sits on Mid-Atlantic Ridge - constructive plate boundary - divergence of North America and Europe
Seismologists aware of increased activity from March - indicated magma was rising to surface
Magma chamber filled up - pressure increased inside volcano - magma started to rise from March 20th - caused significant lava flows - but then quietened down
More magma was rising in two weeks of less activity on surface - magma from mantle mixed with existing magma in magma chamber
Triggered chemical reactions - more gases created - resulted in explosive eruption
From 12th April lava was flowing from the magma chamber again - by 15th April vents below glacier were full of magma - glacier burst open melting glacier and causing extensive flooding
Hot magma meets freezing ice - creates huge plumes of tephra
Eruption lasted two weeks
Ash clouds up to 30,000 feet into air - tephra dispersed across local area - much of north-east Europe
International air travel was affected - hundreds of thousands of people displaced
Trade affected with cargo flights cancelled - Kenya lost $35 million due to fresh food decaying
Total cost to Europe - $2.8 billion in lost trade and insurance costs from cancelled flights
Caused less demand for air fuel - affected oil industry - stock marked shares in air travel companies fell
Flash floods from jokulhalups damaged fields and crops - 20 farms destroyed - evacuated
200m ice melted - damaged Route 1 - one of countries main roads
Secondary effect - ash covered ice - increased melting - dark surfaces absorb more heat - exacerbating flooding (positive feedback)
Volcano in sparsely populated area - no deaths or injuries - very little damage to property
Airspace closed to mitigate risk of aviation disaster - 100,000 flights cancelled - cost of more than $200 million per day
Iceland’s National Emergency Agency - mitigate risks
Co-ordinated very effective and immediate response
Damaged bridges immediately replaced with temporary structures - minimise impact on communication
No need for emergency aid - no injuries or damage to buildings
Iceland increased surveillance of area - public kept well informed about any changes in activity
Disruption caused chaos in London Heathrow - normally sees 1,200 flights in + out a day
700-800 people evacuated from their homes from area 25km east of capital
Volcano melted a glacier - caused massive flood
First volcano at Eyjafijallajokull glacier since 1823
Iceland’s first since 2004
Briefly forced 6000 from their homes
Millions of people stranded due to grounding thousands of flights
Low pressure system developed over Iceland - push ash towards the Arctic