are opening in the Earth'scrust that allowsenergyfrom the interior of the Earth to escape to the surface. The energy in the magma that goes out are in the form of lava, ash, and gas
How volcanoes are formed?
subduction allows water from the subducting plate to be drivenupward, off the subducting plate and into the mantle wedge
2 ways magmaescape
Intrusion
Extrusion
Intrusion
"inside" internalmagmapullsdown the volcano
the creation of sedimentaryrocks
Extrusion
"outside" externalflow of magma
forms igneousrocks
moltenrock
magma
Classifications of Volcano
Active Volcano
Dormant Volcano
Extinct Volcano
Active volcano
eruptsregularly
ex: taal volcano
Dormant Volcano
tendency to erupt in the future
ex: Mount Fuji
Extinct volcano
have noterupted in human history and doesnot have magma
Dormant can be active if heat is sufficient
Potentialhazard of volcano
Volcanichazard
Types of Volcanoes
Stratovolcanoes
Shield Volcano
Calderas
Mid-Ocean Ridges
Stratovolcanoes
-appear as tallsteepmountains
-perfecttriangularshape
Shield Volcano
flatter and domeshaped that produces low viscosity, runny lava, it spreads from the source
Calderas
-large depressions in the ground -has a deep crater
Mid-OceanRidges
-underwaterchains of volcanicmountains
-can be found at the Pacific ocean
Volcanic Hazards
any potentiallydangerous volcanicprocess that puts human lives, livelihood or infrastructure at risk of harm
Potentialvolcano-relatedhazards
Lahar
Ash fall
Pyroclastic flow
Ballistic Projectile
Volcanic Gas
Lava flow
Lahar
-is a mixture of water, pyroclasticmaterials and rockfragmentsflowingdown a volcano or rivervalley
-type of mudflow or debrisflow
Pyroclasticmaterials
cinder, ash, volcanicbomb
Ashfall
-composed of bits and pieces of pulverizedrock, minerals, and volcanic gloss generated from the volcanic eruption
-can cause larger impact and wider casualties. -it lasts up to months
-affects air visibility which means it could cause plane turbulence
Pyroclasticflow
refers to hotdrymasses of fragmented volcanic materials that move along the slope in contact with groundsurface
-hot & dry = faster and wider casualties.
BallisticProjectile
is a rockfragment that is ejected from the volcano during its explosiveeruption. It is like a cannonball that travelsfast in the air
VolcanicGas
-gases givenoff by activevolcanoes, consists of sulfurdiovide and hydrogen sulfide, which are poisonous and hazardous to organisms
-too much inhalation could cause respiratory problems
Signs of an impending volcanic eruption
Occurrence or increase in the frequency of smallearthquakes
Deformation in theground manifested by changes in ground elevation (tilting) and formation of cracks or openings (ground fissuring)
Increase in the amount of volcanicgases and in temperature, which may indicate that the magma has gone closer to the surface
Glow of volcaniccrater due to the presence of magma
Increase in steamemissions coming from volcanic openings, fissures, or hot springs
Thermalchanges within the surroundings of the volcano
Change in the color of nearby vegetation and lakes
Landslides and rockfall not due to heavy rains
Drying up of springs and freshwatersources around the volcano
Parametersused to monitorvolcanoes
GroundDeformation
SeismicActivity
Gases
SensoryObservations
Ground Deformation
any surfacechanges on a volcano (subsidence sinking, tilting, buiging)
Tiltmeter
identifies the change of land area
SeismicActivity
when magmarisesup, it breaks the rocksalong the way
seismograph
measuressmalltremors
Gases
monitortypes and rates of emissions of differentgases
-have foul smell
Sensory Observations
Visual
Auditory
Olfactory
Tactile
visual
-vision
-potential hazards that we can see
Auditory
sense of hearing
ex: explosions, shaking, sounds of animals.
Olfactory
hazardous smell
tactile
touch/feel
-ex: temperature, heat, skin irritations.
Lava flow
is a highly elongated mass of molten rock materials cascading downslope from an erupting vent. The lava flow being extruded has low silica water content
-gives time to escape
2 magma components 1. silica- higher silica, the higher viscosity