eruptions Flashcards
1
Q
effusive
A
- divergent plate margin
- basalt lava - low viscosity, high temperature during eruption and low silica %
- eruptions involve: gas bubbles expanding freely and lava flows
- not explosive
- frequent & can have long durations
- shield volcanoes
2
Q
explosive
A
- convergent plate margin
- acidic lava (rhyolite) with high viscosity and lower temperature during eruption and high silica %
- violent burst of gas, cone shatters
- materials extruded: ash, lava bombs and tephra’s
- infrequent
- stratovolcanoes/ composite volcanoes
3
Q
Plinian eruption
A
- gas rushes up through viscous lava and ash = fragments forced airborne from huge explosion
- produces cloud of gas and volcanic debris km’s thick
- products run down slope
4
Q
Vesuvian Eruptions
A
- powerful blasts of gas and ash clouds
- lava flow and ash falls - covers surrounding areas
- more violent than vulcanic eruption
5
Q
vulcanic eruption
A
- violent gas explosions out plugs sticky/ cooled lava
- fragments build up into cones once viscous lava solidifies
- eruption clears blocked vent and emits volcanic ash
6
Q
Strombolian eruption
A
- frequent gas explosions = runny lava into air and eventually forming a cone
- explosive eruption -> pyroclastic rock dispersed
- produces white cloud of steam
7
Q
Hawaiian eruption
A
- central activity
- runny, basaltic lava and gases escape easily
- minor pyroclastic activity
8
Q
Icelandic lava eruptions
A
- persistent fissure eruptions
- large quantities of basaltic lava build up
- Deccan Plateu and Columbia Plateu
9
Q
difference between volcanic eruption away from plate margins and on plate margins
A
- away from plate boundary the casualty of volcanic activity are hotspots
- where within the magma plume some magma is hotter than its surrounding magma = melting of crust of a moving plate margin
- on plate margin the causality of volcanic activity is plate margins moving agains’t one another causing fissures allowing magma to rise
10
Q
similarities between differing casualties of volcanic activity
A
- formation of volcanoes = plates are moving and the magma/ magma plume stay stationary
- fissures created from plates forces pushing away or towards another plates allowing magma movement