Topic 4B Flashcards

1
Q

extrusive

A

fast cooling (small minerals)

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2
Q

intrusive

A

long cooling (large minerals)

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3
Q

glassy characteristics

A

glassy, cools quickly, extrusive

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4
Q

aphanitic

A

small crystals, cools quickly at lower temp, extrusive

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5
Q

phaneritic

A

large crystals, cools slowly at high temp, intrusive

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6
Q

porphyrite

A

two crystal sizes, intrusive

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7
Q

pyroclastic

A

fragments of crystals

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8
Q

vesicular

A

holes, pores

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9
Q

Felsic Minerals in general

A

light in color
light in weight (Fe,Mg poor)
Found in intermediate and felsic rocks

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10
Q

mafic minerals in general

A

dark in color
heavier(Fe,Mg rich)
found in mafic and ultramafic rocks

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11
Q

Felsic Rocks

A

Rhyolite (extrusive)
Granite (Intrusive)

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12
Q

Intermediate rocks

A

Andesite ( extrusive)
Diorite (intrusive)

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13
Q

Mafic rocks

A

basalt (extrusive)
gabbro (intrusive)

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14
Q

Ultramafic rocks

A

Rare (extrusive)
Peridotite (intrusive)

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15
Q

intermediate magma can form through

A

crystal settling in a mafic magma
partial melting of mafic rock
mixing mafic magma with felsic magma
assimilating felsic rocks into mafic magma

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16
Q

felsic magma can be formed through

A

crystal settling in an intermediate magma
partial melting

17
Q

What is a volcano

A

any landform (earth or ocean) that releases lava, gas or ashes or has done so in the past

Mostly occur at divergent or convergent boundaries

18
Q

Mafic Magma characteristics

A

thin and flows easily
low silica content
low viscosity
low gas

forms Aa and
Pahoehoe lavas

19
Q

Felsic Magma characteristics

A

thick
tends to erupt catastrophically
high silica content
more viscous
high gas

20
Q

Pyroclastic debris in ascending mass

A

ash,lapilli, volcanic bombs, volcanic block, welded tuff, pumice

21
Q

what are the 3 most abundant gases released in an eruption

A

H20
CO2
SO2

22
Q

central vent volcanoes characteristics

A

central vent
summit crater
has 4 types
shield volcanoes
cinder cones
stratavolcanoes
rhyolite caldera complexes

23
Q

Large scale volcanic terrains

A

no central vent
network of source material
extend over large areas

24
Q

Shield volcanoes characteristics

A

low viscosity creates broad, gentle slops
low silica, low gas, magma comes from mantle

25
Q

Stratovolcanoes characteristics

A

Alternating layers of mafic to intermediate lava flows with layers of intermediate to felsic explosively pyroclastic fragments (explosions due to gas buildup)

26
Q

Rhyolite caldera complexes characteristics

A

High silica, high gas magmas
massive explosions ( most explosive)
withdrawal of magma from magma chamber causes collapse

27
Q

Large scale volcanic terrains characteristics

A

mid-ocean ridges develop divergent boundaries (spreading centres)
basaltic flow creates a global network

28
Q

tectonic environment- divergent boundary

A

mafic lava flows (efussive)
mid ocean ridge

29
Q

tectonic environment- oceanic hot spot

A

mafic lava flows
shield volcanoes

30
Q

tectonic environment- continental hot spot

A

felsic to mafic lava flows
shield volcanoes (rare)
stratavolcanoes (common)
rhyolite caldera complexes

31
Q

tectonic environment- oceanic/continental subduction zones

A

felsic to mafic lava flows
volcanoes form volcanic arc
stratavolcanoes or rhyolite caldera complexes

32
Q

tectonic environment- oceanic/oceanic subduction zones

A

Intermediate to mafic lava flows
volcanoes form and island arc
shield volcanoes or stratavolcanoes