Topic 4B Flashcards

(32 cards)

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

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
Stratovolcanoes characteristics
Alternating layers of mafic to intermediate lava flows with layers of intermediate to felsic explosively pyroclastic fragments (explosions due to gas buildup)
26
Rhyolite caldera complexes characteristics
High silica, high gas magmas massive explosions ( most explosive) withdrawal of magma from magma chamber causes collapse
27
Large scale volcanic terrains characteristics
mid-ocean ridges develop divergent boundaries (spreading centres) basaltic flow creates a global network
28
tectonic environment- divergent boundary
mafic lava flows (efussive) mid ocean ridge
29
tectonic environment- oceanic hot spot
mafic lava flows shield volcanoes
30
tectonic environment- continental hot spot
felsic to mafic lava flows shield volcanoes (rare) stratavolcanoes (common) rhyolite caldera complexes
31
tectonic environment- oceanic/continental subduction zones
felsic to mafic lava flows volcanoes form volcanic arc stratavolcanoes or rhyolite caldera complexes
32
tectonic environment- oceanic/oceanic subduction zones
Intermediate to mafic lava flows volcanoes form and island arc shield volcanoes or stratavolcanoes