type of rocks
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8/3/2019 Type of Rocks
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Type of
Rocks
Rock Mineral
Composition
Color Parent
Material
Texture Description
Pumice Quartz
MuscoviteOrthoclase
White or
gray
-Granite -Very thin
translucentbubble wall
extrusive
igneous
rock.
-Cell, and
glassy
-Highly
composemicrovesicular
glass pyroclastic
.
-It forms when
volcanic gases
absolving from
viscous magma
nucleate bubbles
which cannot
readily decouple
from the viscous
magma prior tochilling to glass
-Mild in weight
Diorite Amphibole,
Biotite
Na Plag/
Proxene
Grey,grey
to dark
grey
Granite -Coarse-
grained
-Granular
-Diorite results
from partial
melting of mafic
rock above
subduction zone.
It commonly
produces in
volcanic arcs,
and incordilleran
mountain
building.
-Extrusive
Igneous
Rock
Gabbro Pyroxene
Olivine
Ca Plag
Black or
greenish
dark
color
Basalt -Coarse-
grained
-Granular
-plutonic which
form when
molten magma
is trapped
beneath the
earth.
Andesite Amphibole,
BiotiteNa Plag
Black or
dark incolor
Basalt Fine -
grained
-Volcanic rock
-Can be found atAndes Mountain
Rhyolite Quartz
Muscovite
Orthoclase
White,
light
yellow,
brown or
red
Basalt Fine-
grained
-extrusive rock
-High content of
silica, low iron,
and magnesium,
rhyolite will
melt highly
polymerized and
form viscous
lavas.
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Sandstone Quartz and
Feldspar
Brown,
yellow,
red, pink,
white
Cemented
sand
-Fine-
grained
-Rock formation
that are
primarily
composed of
sandstone
usually allow
percolation ofwater and other
fluids and are
porous enough
to store large
qualities ,
making them
valuable aquifers
and petroleumreservoirs.
Coal Consists of
Carbon
Dark grey Form
from the
compres-sion of
plant
material
Soft ,brittle,
lightweight,
porousmaterial
-Usually
produced by
slow pyrolysis,the heating of
wood or other
substance in the
absence of
oxygen.
Conglomerate Clastic rock Grey or
yellowish
Cemented
roundedgravels
and
pebbles
-Coarse-
grained-Angular
Individual clasts
within a finer-grained matrix
that have
become
cemented
together.Sedimentary
Rock
Shale Quartz and
Calcite
Clay mineral
Red,
brown,
green,
yellow
Compac-
ted mud
-Fine
grained
The ratio of clay
to other minerals
is visible.
Breccia Clastic rocks White ,
dark grey
Variety of
the origin
Coarse
Angular tosubangular
Collapse
breccias formswhere there has
been a collapse
of rock, typically
in karst
landscape.
Siltstone Clay mineral Redyellowish
or
greenish
Mud Grain sizein the silt
range
Intermediatecomposition
between
sandstone and
shale.
Mudstone Clay mineral Dark grey mud Fine
grained
A nonfissile
mud shale.
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Fossiliferous - - - Coarse Placement of
fossil in
sedimentary
rocks
Schist Mica,
Chlorite ,
talc,hornblende,
granite
Grey,
dark
yellowish
By paral-
lelism of
more than50% of
minerals
Coarse Schist contains
more than 50%
platy andelongated
minerals, often
finely
interleaved with
quartz andfeldspar.
Metamorphic
Rock
Phyllite Quartz, Mica
,Chlorite
Grey or
white
Shale or
pellite
-Coarse
-Phyllitic
texture
Has good
fissility and
form under low
grade
metamorphic
condition.Batu
Loh(Slate)
Clay or
volcanic ash
Quartz,
muscovite ,Biotite,
Chlorite,
hematite.
Grey and
dull
Shale and
other fine
grained
rock.
Fine-
grained
The slaty
cleavage result
from the paralle
alignment ofnumerous fine
phyllosilicate
(platy) minerals
(e.g muscovite
and chlorite)
Gneiss Biotite,
Albite,
chlorite
Granite,
grano -
diorite,shale,
rhyolite,
diorite,
slate,&
schist
Medium to
course-
foliated
Mineral
composition is
variable butfeldspar is
especially
abundant.
Marble Calcite and
Dolomite
Grey Carbonate
rocks such
as
limestone
or
dolomite.
Silt Metamorphism
causes variable
recrystallization
of the original
carbonate
mineral grains.
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Rock Component
Minerals
Elemental Composition Plant Essential
Elements
Pumice Quartz Si,O -
Muscovite K,Al,O,Si K
Orthoclase K,Al,Si,O K
Diorite Amphibole Fe,Mg,Ca,Si,O Fe,Mg,Ca
Biotite K,Al,Mg,Fe,Si,O,OH K,Mg,Fe
Pyroxene Ca,Na,Fe,Mg,Zn,Al,Si,O,Li,,Cr,Sc,Ti,V Ca,Fe,Mg,Zn,
Gabbro Pyroxene Ca,Na,Fe,Mg,Zn,Al,Si,O,Li,,Cr,Sc,Ti,V Ca,Fe,Mg,Zn,
Olivine Mg,Fe,Si,O Mg,Fe
Ca Plag Ca Ca
Andesite Amphibole, Fe,Mg,Ca,Si,O Fe,Mg,Ca
Biotite K,Al,Mg,Fe,Si,O,OH K,Mg,Fe
Na Plag Na -
Rhyolite Quartz Si,O -
Muscovite K,Al,Si,O K
Orthoclase K,Al,Si,O K
Sandstone Quartz Si,O -
Feldspar K,Al,Si,O,Na,Ca K,Ca
Coal - C CConglomerate Quartz Si,O -
Silicate Si,O -
Shale Quartz Si,O -
Calcite Ca,C,O Ca,C
Clay mineral Al,Si,O -
Breccia Quartz Si,O -
Silicate Si,O -
Siltstone Clay Mineral Al,Si,O -
Mudstone Clay Mineral Al,Si,O -
Schist Mica K,Na,Ca,Al,Mg,Fe,Si,F,OH K,Ca,Mg,Fe
Chlorite Cl,O Cl
Talc Mg,Si,O,OH Mg
Quartz Si,O -
Orthoclase K,Al,Si,O K
Muscovite K,Al,Si,O K
Amphibole Fe,Mg,Ca,Si,O Fe,Mg,Ca
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Phyllite Quartz Si,O -
Mica K,Na,Ca,Al,Mg,Fe,Si,F,OH K,Ca,Mg,Fe
Chlorite Cl,O Cl
Batu Loh(Slate) Quartz Si,O -
Muscovite K,Al,Si,O K
Biotite K,Al,Mg,Fe,Si,O,OH K,Mg,Fe
Chlorite Cl,O Cl
Hematite Fe,O Fe
Gneiss Biotite K,Al,Mg,Fe,Si,O,OH K,Mg,Fe
Chlorite Cl,O Cl
Albite Na,Al,Si,O -
Marble Calcite Ca,C,O Ca,C
Dolomite Ca,Mg,C,O Ca,Mg,C