Volcanism - Ash Columns Flashcards
What are ash columns
Resultant from explosive solo liv eruptions at destructive margins/ continental hotspot locations when the top of a conduit is breached
4 stages of ash Column formation
1) Rising magma reduces pressure at shallow depths, gas bubbles exsolve driving the magma up
2) bubbles grow, forcing material upwards to get more space, travelling at super sonic velocities to explode at fragmentation surface
3) column entrails ambient air heated by rock fragments, ash rises to equal buoyancy height in convective thrust region
4) plume spreads horizontally by winds, blocks and bombs fall - right angle to wind s
VEI
Logarithmic measurement
Ash could height depends on VEI which is dependent on magma types and gas
Tephra fall out and ejected form conduit walls
Can view 3D fly by
Air problems from ash columns
Ash fragments melt inside planes, corrode and clog up engines
- N America to Asia particularly at risk
Example of air problems from ash columns
Indonesia, 1982
From New Zealand lost power in engines and dropped 7.5km
Front panels corroded only 1 left
NO DEATHS
Ground problems from ash columns
Blocks and bombs
Close to source can fall on people
Isopachs predictions and show radial manner
Ground problems from ash columns example
Tamboura, 1815
VEI 7
61,000 deaths from starvation and disease through crop death and contamination
Deposit problems from ash columns
Tephra property destruction underweight
Breathing ash = respiratory problems
Ash = blinds animals, contaminated water and crops
Can mobilise to form lahars and abrasion of machinery
Deposited problems from ash columns example
Pinatubo, 1991
VEI 6
Typhoon eruption, ash mixed with water = slurry, concrete roof collapsed
Zobin, 2005
Volcan de Colima, Mexico
Most active volcano in Mexico
Done building and destruction, culminating in explosive events
Reached more than 200-220km across
Velocities 50km
Cloud 3860m
Forecasting Ash columns
Denlinger, 2010
SEVIRI - enhances infrared images detect Ash
World meteorological organisation examine dispersion and transport = modelling sensitivity and column
Maximum likelihood estimates - include parameters: height, rate, time, altitude, spatial complexity
Icelandic eruption predict and create estimates by SEVIRI and maximum likelihood estimates
2010
Denlinger
Denlinger
2010
1978
Wilson
Wilson
1978