igneous rocks

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Igneous rock
Rocks that have cooled from magma
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Magma
molten rock
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lava
molten rock that cools at the surface
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silicic igneous rocks
Composition rich in silica of more than 30% and is leucocratic (light coloured)
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intermediate igneous rocks
silica content of 66-52% and are mesocratic (grey)
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Mafic igneous rock
silica content of 52-45% and are melanocratic (dark)
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Ultramafic igneous rocks
silica content less than 45%
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felsic minerals
light coloured and silica rich
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mafic minerals
dark coloured, silica poor and rich in iron and magnesium
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Extrusive
igneous rocks that cool at the surface both lava and pyroclasts
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intrusive
igneous rocks that cool below the surface
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hypabyssal
igneous rocks form at relatively shallow depths below the surface
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plutonic
when igneous rocks form deep below the surface
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Divergent plate margin
where two plates are moving apart and magma is rising up between them
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convergent plate margin
where two plates are colliding and magma is formed above a subduction zone or deep in the crust
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hot spot
formed by a fixed mantle plume bringing magma to the surface
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partial melting
occurs where some of the minerals in a rock melt to form a magma
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country rock
any rock into which an igneous rock is intruded
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minor intrusion
cool at hypabyssal depth below the surface and include sills and dykes
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major intrusion
plutonic and cool deep below the surface and include batholiths
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contact
where igneous rock meets the country rock
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chilled margin
where the igneous rock has cooled rapidly so it has fine crystals
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baked margin
country rock where it was heated by the intrusion and altered
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metamorphic aureole
large area around a batholith where the rocks have been metamorphose
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volcano
vent at the surface of the Earth through which magma and other volcanic materials are ejected
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pyroclast
individual fragment ejected during an eruption
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pyroclastic
describes all fragmental materials formed by explosive eruptions
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pyroclastic rocks
formed when the pyroclastic material is compacted into rocks
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pyroclastic flow
hot mixture of pyroclastic material and gas
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isopachyte
line joining points equal thickness of a deposit
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lahars
mudflows of wet ash and volcanic debris that can flow rapidly down a mountainside
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viscosity
measure of a fluid's resistance to flow and controls the stickiness of a magma which depends on silica content
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shield volcano
gentle slopes of less than 10 degrees and a circular vent
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fissure eruptions
where magma reaches the surface along long linear crack
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submarine eruptions
where magma comes from a vent or fissure on sea floor
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low viscosity
where magma is fluid and flows freely
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effusive
fluid non explosive basalt lava
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hawaiian eruption
large amounts of fluid basaltic magma from which gases escape few pyroclasts
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strombolian eruption
explosive with less fluid basalt and andesitic lava, regular eruptions of gas and pyroclasts
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vulcanian eruption
violent eruptions with viscous andesitic lava and large quantities of pyroclastic material
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plinian eruption
extremely explosive with viscous gas filled andesitic and rhyolitic lava and tremendous volumes of pyroclastic material
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active volcano
erupted within recorded history
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extinct volcano
not shown any historic activity and heavily eroded
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dormant volcano
one that has not erupted within recorded history but shows in the rock record
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Other cards in this set

Card 2

Front

molten rock

Back

Magma

Card 3

Front

molten rock that cools at the surface

Back

Preview of the back of card 3

Card 4

Front

Composition rich in silica of more than 30% and is leucocratic (light coloured)

Back

Preview of the back of card 4

Card 5

Front

silica content of 66-52% and are mesocratic (grey)

Back

Preview of the back of card 5
View more cards

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