place on earth's surface where molten rock, gases, and pyroclastic debris erupt through the earth's crust
volcano
can be a mountain, vent , or caldera
volcano
why do volcanoes erupt?
due to decompression and magma is lighter than the solid around it (magma rises)
progress of decompression :
eruption onset
pilinian phase
minor ignimbrite phase
caldera collapse
slopes are gentle (2-10 degrees); shapes resembles a roman shield lying on the ground
shield
made up of successive lava flows
shield
steep slopes (30-40 degrees); made up of pyroclastic materials
cindercones
layered structure of alternating tephra and lava flows
composite / strato-volcano
distribution of volcanoes
pacific ring of fire
hot spots
spreading centers
mauna loa, hawai'i
shield
mauna kea, hawai'i
cindercones
mayon volcano, albay
composite
based on number of things (plume height, volume of ejecta, etc.) that can be observed during an eruption
volcanic explosivity index (vei)
calmest eruption type
hawaiian
characterized by the effusive emission of highly fluid basalt lava flows with low gas content, steady lava fountaining and the production of thin lava
hawaiian
Hawaiian
magma : fluid
effusive activity : then, often extensive flow
ejecta : cow-dung bombs and platter, very little ash
structure : spatter cones and ramparts, very broad, flat lava cones
jagged, rough blocks
aaflows
smooth surfaces
pahoehoe flows
short-lived, explosive outburst of pasty lava ejected a few tens or hundreds of meters into the air
strombolian
no sustained eruption column; episodic explosions with booming blast
strombolian
Strombolian
magma : moderately fluid
explosive activity : weak to violent ejection of pasty fluid
effusive activity : thicker, less extensive flows, flows may be absent
ejecta : spherical to fusiform bombs; cinder; small to large amount of glassy ash
structure : cinder cones
occur as a series of discrete, canon-like explosions that are short-lived, lasting for only minutes to a few hours, often with high-velocity ejections of bombs and blocks
vulcanian
once the volcano "clears its throat", subsequent eruptions can be relatively sustained and quiet
vulcanian
Vulcanian
magma : viscous
explosive activity : moderate to violent ejection of solid hot fragments of new lava
effusive activity : flows commonly absent, thick and stubby if present
ejecta : essential, glassy to lithic, blocks and ash, pumice
explosive activity : like Vulcanian, commonly with glowing avalanches
effusive activity : domes and/or short, very thick flows, flows may be absent
ejecta : same as vulcanian
structure : ash and pumice cones, domes
eruptive columns produce widespread dispersal of tephra which covers large areas with an even thickness of pumice and ash
plinian
Plinian
magma : viscous
explosive activity : ejection of large volumes of ash; caldera collapse
effusive activity : ash flows, small to very luminous, may be absent
ejecta : glassy ash and pumice
structure : widespread pumice lapilli and ash beds, generally no cone-building
generated by the interaction of magma with either groundwater or surface water
surtseyan / phreatomagmatic
much more explosive; as the water is heated, it flashes to steam and expands explosively, thus fragmenting the magma into exceptionally fine-grained ash
surtseyan / phreatomagmatic
erupted with historical times (within last 600 years); accounts documented by man
active volcanoes
erupted within the last 10,000 years based on analyses of materials from young volcanic deposits
active volcanoes
morphologically young-looking but with no historical or analytical records of eruption
potentially-active volcanoes
no recorded eruptions; physical form has been intensively weathered and eroded, bearing deep and long gullies
inactive volcanoes
phivolcs
philippine institute of volcanology and seismology
there are 24 active volcanoes based on eruptive history according to phivolcs
54 known eruptions; yearly volcanic activity; 1814-most destructive (VEI: 4)
mayon volcano (albay)
39 known eruptions (1911); yearly volcanic activity