REVIEW DECK Flashcards
crystalline structure
atoms in a mineral must occupy fixed positions in a grid called a lattice
mineral def
nat occurring
solid
inorganic
defineable chem comp
orderly arrangement or molecules in a lattice
crystal growth
growth occurs as atoms attach to the outer surface
in an open cavity crystal faces grow perfectly
early crystals act as seeds for further growth
three types of crystals (based on face visibility
anhedral
euhedral
subhedral
mineral identitification characteristics
color
streak
luster
hardness
spec grav
cry habit
cleavage
reaction to acid
special prop
7 classes + 5 subgroups of #7
sulfides
oxides
sulfates
carbonates
halides
native metals
silica
- independant tetra
-single chain
-double chain
-sheet silicates
-framework silicates
clay minerals are a type of
sheet silicates
two types of clays
koalinite and smectite
does koalinite swell
no
does smectite swell
yes
what kind of clay swells and why
smectite
TOT structure allows water to enter
how small is clay
<4 microns
salt use
tatsty
5 ways minerals form
precipitation in water
solidification from a melt
solid state diffusion
biomineralization
precipitation from gas
solid state diffusion def
atom by atom transfer without ever melting
rock def
a coherent naturally occurring solid aggregate of minerals or less commonly a body of glass
two main types of rocks
clastic
crystal
bedrock vs clast def
bedrock attached to ground
clast not
physical characteristics that identify rocks
layering
grain size
texture
equantnness
three textures + secret fourth
crystalline
fragmental
glassy
foliated
not sedimentary to sedimentary
erosion transportation deposition
sedimentary to sedimentary
erosion transportation
redeposition
meta to ignous
melting
meta to meta
burial heating and remetamorphism
sed to meta
burial and heating
igenous to igneous
heating and remelting
sed to igneous
heating and melting
crust to rock
input of new melt into the crust from the mantle
rock to crust
subduction
three main types of rocks by orginin
igneous
sedimentary
metamorphic
two igenous realms
extrusive
intrusive
what is a melt
molten rock
lava vs magma
lava extrusive
magma intrusive
the crust and athenosphere are mostly
solid rock
melts occur in
localized areas
3 reasons for melting
decompression
flux (volatiles
heat transfer
how decompression melts
temp constant pressure goes down
melts the rock
how introduction of volatiles melts
subduction introduces volatiles
(water) changes the melting point
felsic %
67-76
intermediate %
53-66%
mafic %
46-52%
ultramafic %
38-45
felsic flow is _____ viscous because of the
more viscous
because of the silica
mafic flow is ______ viscous because of the
less viscous
because less silica
how does a melt become a rock (how does it freeze)
volatiles leave
reaches the surface
temp or pressure change
types of intrusions
(which is parallel)
dike (perpendicular)
sills (parallel)
what is a pluton
a magma chamber that solidified
what is a batholith
a bunch of plutons together
how does partial melting and crystal refractionalizatoion work
rock begins to melt
felsic melts earlier
resulting magma is more felsic
as mafic rocks stay solid, the felsic minerals migrate away
when it cools the opposite happens the mafic rocks solidify first
the whole mantle is one type of rock (what is it)
peroditite
aphanitic def
fine grained, cooled fast, crystals couldn’t grow much
phaneritic def
coarse grained, cooled slow, crystals grew more
porphyritic def
two cooling stages, slow to fast
aphanitic probably cooled where
underground
phaneritic probably cooled where
above ground