Igneous Rock Classification Flashcards
2.5-2.10
Three main igneous textures
crystalline
fragmental
glassy
define aphanitic
fine grained crystals grow quickly under conditions of rapid cooling, typically in extrusive settings
1 stage of cooling
define phaneritic
coarse grained crystals grow larger by cooling slowly typically intrusive
1 stage of cooling
defined porphyritic
both small and large crystals (called phenocrysts)
initial slow cooling followed by rapid cooling (usually after eruption)
2 stages of cooling
texture of rhyolite andesite and basalt
aphanitic
texture of granite diorite and gabbro
phaneritic
mafic melts have a high proportion of
magnesium and iron relative to silica
mafic rocks are usually ___ colored
dark
mafic rocks have ____ specific gravity than felsic
higher
Basalt and diorite M/F
Felsic color
lighter
felsic specific gravity
lower than mafic
rhyolit and granite M/F
felsic
Grain size has to do with
history not composition
peridotite M/F A/P I/S/M
ultramafic phaneritic igneous
andesite M/F A/P I/S/M
intermediate anphanitic igneous
komatite / picrite M/F A/P I/S/M
ultramafic anphanitic igneous
granite M/F A/P I/S/M
felsic phaneritic igneous
freezing temp is proportional to __ density __ silica content ____how mafic it is
+ - +
what is pumice
felsic rock full of vesicles
it floats
glassy igneous rock
what is scoria
vesicular and glassy mafic rock
glassy igneous
what is obsidian
glassy felsic rock, no vesicles
glassy igneous
what the 3 main glassy igneous rocks
pumice
scoria
obsidian
what are the pyroclastic igneous rocks
tuff: fused volcanic ash
volcanic breccia : angular fragments that have fused together
a volcano is
a mountain constructed by the eruption of molten rock from earths interior
volcanoes are a direct consequence of
plate tectonics and mantle convections
Products of volcanic eruptions
lava flows
volcanic gases
pyroclastic debris
lava flows are
molten rock that moves over the ground
volcanic gases are
expelled vapor’s and aerosols
pyroclastic debris are
fragments blown out of a volcano
in violent eruptions
gas escape is difficult
in mellow eruptions
gas escape is easy
mellow eruptions have _ viscosity
low
violent eruptions have _ viscotisy
high
basaltic lava has
low viscosity and can travel long distances
andesitic lava is
too viscous to flow far and tends to break up as it flows
felsic lava is
so viscous that it may pile up in a dome shaped mass
basaltic lava flows are
very hot, mafic, low viscosity
basalt flows are often
thin and fluid
go long distances