Volcanoes Flashcards
Formation of a supervolcano Step2
The magma chamber grows this then forces the ground upwards into DOME this creates fissures hydrothermal features
Formation of a supervolcano Step3
Gas and ash escape through fissures and into cracks in the surface causing a massive super eruption
Formation of a supervolcano Step4
The land collapses into the now empty magma chamber
This creates a depression called a CALDERA
Where is a Composite volcano found
Destructive plate margins (subduction)
What is a Composite volcano like
Cone shaped
Steep sided, layers of ash and lava
Magma viscous/ cools quickly
Example: Montserrat
Where is a Shield volcano found at
Constructive plate margins
What is a shield volcano like
Dome shape with sloping sides
Gentle explosions (less explosively due to type of magma)
Lava is runny and flows distances
Example: Iceland
What is the difference between a volcano and a super volcano
A super volcano is more powerful as it can affect people on a global scale. (volcanic ash in the atmosphere)
Impacts of a supervolcano
- A pyroclastic flow can kill people (flow of magma from volcano)
- People have to move houses new area (falling ash,lava,explosion)
- Volcanic ash will block solar radiation (famine)
- Ash in the atmosphere can cause a volcanic
winter(economies collapse)
5 warning signs of a volcano (yellow stone)
- More frequent eruptions
- Vents spraying out boiling temperatures
- High levels of hydrogen sulphide and carbon dioxide (gases found in magma)
- Ground has steadily/ slowly been uplifting
- Ground temperatures soared to boiling point
Planing for a volcano
- Concrete shelters are built to protect people from volcanic ash
- Channels to divert dangerous flows
Predicting/ monitoring a volcano
- Tilt Meters - detect when volcano swells up as it fills with magma
- Air crafts - measure amount of gas volcano gives off (predict eruption)
- Bore holes- measure water temperature ( temperature increases closer magma is)
Formation of a supervolcano Step 1
The magma chamber is fed with magma from the mantle over weak areas in the earths crust