14.2 Flashcards

(46 cards)

1
Q

what are the two classifications for volcanoes?

A

shape
type of eruption

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2
Q

lava plateaux/ fissure eruptions

A

shield volcanoes may erupt along lines of fissures rather than a central vent spilling liquid lava in successive layers

form broad plateaux such as the Colombia plateaux - often cut by deep canyons that expose the layers of rock - Grand Canyon

extensive lava flow are basaltic in nature so they can they can flow great distances

flat and featureless

macrofeature

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3
Q

basic/shield volcano

A

3-4 miles wide and 1500-2000m tall

eg Mauna Loa

built up slowly by accreation of thousands of flows of highly fluid basaltic

low silica so spreads over wide areas

cools as thins forming gently dipping sheets

lava erupts form rift vents along fractures that develops on the flanks of the cone

magma has low gas content and is low in silica allowing it to flow over wide distances

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4
Q

acid/ dome volcanoes

A

craggy, steep sloped convex sides covered with rock debris

typically found near large composite volcanoes

made of layers of lava

formed by repeated violent eruptions and slow moving lava flows which gives layered structure

magma is made of higher silica and high gas pressure making magma slow moving and explosive

eg Puy region of central france

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5
Q

ash-cinder cones

A

formed from ash, cinders and volcanic bombs ejected from crater

sides are steep and symmetrical

eg Patricutun, Mexico

may occur as single volcanoes or secondary volcanoes on the sides of stratovolcanoes or shield volcanoes

tephra ejected

lava cools and builds up around the vent forming crater

build up over time

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6
Q

composite volcano/ stratovolcano

A

tall and conical

built up from many layers of hardened lava, tephra, pumice and volcanic ash

steep profiles

periodically explosive and quiet eruptions

lava typically cools before spreading due to high viscocity

layered structure built up of sequential outpourings of eruptive materials

increase in temp causes dome to expand while its outer lava cools, causes newly hardened surface to splinter causing loose debris to fall from its sides

eg Mt Etna

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7
Q

caldera

A

bowl shaped depression formed when volcano collapses into void left by empty magma chamber

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8
Q

crater lake caldera

A

results from stratovolcano collapsing into its magma chamber during a violent eruption

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9
Q

basalstic caldera

A

concentric ring pattern resulting from a series of gradual collapses
often found at summit of shield volcanoes such as the craters at the top of Mauna Loa

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10
Q

resurgent calderas

A

largest volcanic structure
result from catastrophic eruptions that dwarf eruptions recorded by humans
Yellowstone Caldera

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11
Q

lava type explosive volcano

A

rhyolite anderite

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12
Q

lava type effusive volano

A

basalt

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13
Q

lava characteristics explosive

A

acid high % silica
high viscocity
lower temp @ eruption

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14
Q

lava characteristics effusive

A

low % silica
low viscocity
high temp @ eruption

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15
Q

style of eruption explosive

A

violent bursting of bubbles when magma reaches surfacr

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16
Q

style of eruption effusive

A

limited explosive force

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17
Q

materials erupted explosive

A

ash, dust, lava bombs, tephra

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18
Q

materials erupted effusive

A

gas, lava flows

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19
Q

frequency of eruption explosive

A

long periods with no acitivity

20
Q

frequency of eruption effusive

A

more frequent

21
Q

shape of volcano explosive

A

steep sided strato volcanoes
caldera

22
Q

shape of volcano effusive

A

gently sloping sides
shield volcanoes
lava plataux

23
Q

strato volcanoes

A

made up of layers of ash and acid lava
concave symmetrical profiles
complex internal networks of lava flows which form minor igneous features such as sills and dykes

24
Q

caldera

A

volcanic craters
2km in diameter
eruption destroys cone and underlying magma chamber is emptied - sides collapse
eg Krakatoa

25
archipelago
closely grouped cluster of islands Indonesia
26
icelandic lava eruptions
large persistent fissure eruption large quantities of basaltic lava
27
hawaiian eruption
runny basaltic lava travels down sides of volcano in lava flows gases escape
28
strombolian eruption
frequent gas explosions large quantities of pyroclastic rock thrown out
29
vulcanian eruption
blasts out of plugs fo sticky or cooled lava fragments build up into cones of ash and pumice viscous lava large quantities of ash
30
vesuvian eruption
powerful blasts of gas pushing ash clouds high into the sky violent ash covers surrounding areas
31
plinian eruption
gas rushed up through sticky lava ash and fragments clouds of gas and volcanic debris - kilometres thick
32
lava plateaux
magma erupts from multiple fissures vast areas covered by free flowing lava - flood basalts millions of years of denudation create varied relief eg Columbia plateaux covers 130,000km2
33
shield volcanoes
effusive eruptions found at divergent plate boundaries mostly occur at mid ocean ridges successive flows accumulate forming huge volcanoes eg Skjadbreidur, Iceland - example of above ground one
34
eruptions at hot spot
fixed area of volcanic activity where magma from a rising mantle plume reaches the Earth's surface magma rises and forms island arc, and as plates move, island moves further away from hotspot and new island forms above hotspot creates chain of islands eg Hawaiian chain, pacific plate moves NW
35
super volcanoes
volcano that erupts more than 1000km3 of material on a single eruption event exist as giant calderas eg Yellowstone last erupted 70,000 years ago
36
what two factors need to be considered when assessing volcanic acitivity?
magnitude - amount of material erupted intensity- the speed at which material is erupted
37
Volcanic Explosivity Index
combines magnitude and intensity into a single number on a scale 0-8 not good for effusive
38
what factors are taken into consideration when assessing explosivity of the eruption?
volume of erupted material height ejected material reaches time duration
39
lava flows
PRIMARY impacts dependent on type of lava basaltic lava is free flowing and can cover significant distances eg Hawaii 2015, covered 20km acidic lava is thicker and bulldozes everything in its path
40
pycrolastic flows
PRIMARY combination of hot gases (500+ degrees), ash and rock fragments travelling at high speeds 100km/h follow contours of ground inhaling these gases causes instant death eg Pompeii
41
tephra
any material ejected from a volcano into the air ranges in size from very fine- Pele's hair, Pele's tears to ballistic material - lava bombs, Lapilli buries farmland in layers of ash weight of accumulated ash causes buildings to collapse and people with respitory issues are at risk eg, eruption of Eyjafjallajokul 2010 caused cancellation of 100,000 flights
42
toxic gases
PRIMARY eruptions emit CO2, carbon monoxide and sulfur dioxide deadly threat to human and livestock populations can causes acid rain also can cause limnic eruptions eg Lake Nyos killed over 1000 people
43
lahars
SECONDARY mud flow with consistency of concrete snow and ice melt and mix with mud and flow rapidly down cone travel at 50km/h bury and destroy everything in their path eg Nevado de Ruiz, Columbia, 23,000 killed
44
floods
SECONDARY eruptions beneath an ice field or glacier cause rapid melting vast quantities of water accumulate until they find an exit from under the ice aka jokulhlaup
45
tsunami
violent eruptions of island volcanoes can cause massive displacement of ocean water and waves travleling at 600km/h eg Krakotoa, killed 36,000
46