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Lithology |
Description |
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Rock |
Includes unconsolidated material |
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Metamorphic rock |
A rock derived from pre-existing rocks by
mineralogical, chemical, and/or structural changes, essentially in the
solid state, in response to marked changes in temperature, pressure,
shearing stress, and chemical environment, generally at depth in the
earth’s crust. |
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Amphibolite |
A crystalloblastic rock consisting mainly of
amphibole and plagioclase with little or no quartz. |
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Calc-silicate rock |
A metamorphic rock consisting mainly of
calcium-bearing silicates such as diopside and wollastonite, and formed by
metamorphism of impure limestone or dolomite. |
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Eclogite |
A granular rock composed essentially of garnet
(almandine-pyrope) and sodic pyroxene (omphacite). |
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Gneiss |
A foliated rock formed by regional metamorphism,
in which bands or lenticles of granular minerals alternate with bands or
lenticles in which minerals having flaky or elongate prismatic habits
predominate. Generally less than 50% of the minerals show preferred
orientation. |
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Felsic gneiss |
A gneissic rock dominated by light-colored
minerals, commonly quartz and feldspar[] |
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Granitic gneiss |
A gneissic rock with a general granitoid
composition[] |
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Biotite gneiss |
A granitic gneiss in which the dominant mafic
mineral is biotite[] |
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Mafic gneiss |
A gneissic rock dominated by dark-colored
minerals, commonly biotite and hornblende[] |
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Migmatite |
A composite “mixed rock” composed of igneous or
igneous-appearing and metamorphic portions[] |
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Orthogneiss |
A gneissic rock formed from an igneous
parent[] |
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Paragneiss |
A gneissic rock formed from a sedimentary
parent[] |
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Granofels |
A medium- to coarse-grained granoblastic
metamorphic rock with little or no foliation or lineation. |
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Granulite |
A metamorphic rock consisting of even-sized,
interlocking mineral grains less than 10% of which have any obvious
preferred orientation. |
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Greisen |
A pneumatolytically altered granitic rock
composed largely of quartz, mica, and topaz. |
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Hornfels |
A fine-grained rock composed of a mosaic of
equidimensional grains without preferred orientation and typically formed
by contact metamorphism. |
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Metasedimentary rock |
A sedimentary rock that shows evidence of having
been subjected to metamorphism. |
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Marble |
A metamorphic rock consisting predominantly of
fine- to coarse-grained recrystallized calcite and/or dolomite, usually
with a granoblastic, saccharoidal texture. |
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Meta-argillite |
An argillite that has been
metamorphosed. |
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Meta-conglomerate |
A metamorphic rock formed by recrystallization
of a conglomerate. |
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Quartzite |
A granoblastic metamorphic rock consisting
mainly of quartz and formed by recrystallization of sandstone or chert by
either regional or thermal metamorphism. |
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Slate |
A compact, fine-grained metamorphic rock that
possesses slaty cleavage and hence can be split into slabs and thin
plates |
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Metavolcanic rock |
A volcanic rock that shows evidence of having
been subjected to metamorphism. |
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Felsic metavolcanic rock
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A metavolcanic rock having abundant
light-colored minerals, typically quartz and feldspar[] |
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Keratophyre |
…all salic extrusive and hypabyssal rocks
characterized by the presence of albite or albite-oligoclase and chlorite,
epidote, and calcite, generally of secondary order. |
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Meta-rhyolite |
A low-grade, felsic metavolcanic rock with
preserved evidence of its original rhyolitic character[] |
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Intermediate metavolcanic rock
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A metavolcanic rock having approximately equal
light- and dark-colored minerals in its mode[] |
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Mafic metavolcanic rock
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A metavolcanic rock having abundant dark-colored
minerals, typically feldspar, amphibole, and/or pyroxene[] |
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Greenstone |
A field term applied to any compact, dark-green,
altered or metamorphosed basic igneous rock (e.g. spilite, basalt, gabbro,
diabase) that owes its color to the presence of chlorite, actinolite, or
epidote. |
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Meta-basalt |
A low-grade, mafic metavolcanic rock with
preserved evidence of its original basaltic character[] |
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Spilite |
An altered basalt, characteristically
amygdaloidal or vesicular, in which the feldspar has been albitized and is
typically accompanied by chlorite, calcite, epidote, chalcedony, prehnite,
or other low-temperature hydrous crystallization products characteristic
of a greenstone. |
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Phyllite |
A metamorphosed rock, intermediate in grade
between slate and mica schist. Minute crystals of graphite, sericite, or
chlorite impart a silky sheen to the surfaces of cleavage (or
schistosity). |
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Schist |
A strongly foliated crystalline rock, formed by
dynamic metamorphism, that can be readily split into thin flakes or slabs
due to the well developed parallelism of more than 50% of the minerals
present, particularly those of the lamellar or elongate prismatic habit,
e.g. mica and hornblende. |
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Amphibole schist |
A schist whose essential constituent is
amphibole with lesser amounts of feldspar, quartz, and/or
mica[] |
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Blueschist |
A schistose metamorphic rock with a blue color
owing to the presence of sodic amphibole, glaucophane, or crossite, and
commonly mottled bluish-gray lawsonite; characteristic of metamorphism in
areas of unusually low thermal gradient, such as subduction
zones[] |
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Calc-silicate schist |
A metamorphosed calcareous rock, commonly
derived from argillaceous limestone or calcareous mudstone, containing
calcium-bearing silicates such as diopside and wollastonite, with a
schistose structure produced by parallelism of platy
minerals[] |
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Greenschist |
A schistose metamorphic rock whose green color
is due to the presence of chlorite, epidote, or actinolite; a common
product of low-grade regional metamorphism of pelitic or basic igneous
rocks[] |
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Mica schist |
A schist whose essential constituents are mica
and quartz, and whose schistosity is mainly due to the parallel
arrangement of mica flakes. |
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Pelitic schist |
A schistose metamorphic rock derived by
metamorphism of an argillaceous or a fine-grained alluminous
sediment. |
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Quartz-feldspar schist |
A schist whose essential constituents are quartz
and feldspar and having lesser amounts of mica and/or
hornblende[] |
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Serpentinite |
A rock consisting almost wholly of
serpentine-group minerals derived from the hydration of ferromagnesian
silicate minerals such as olivine and pyroxene. |
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Skarn (tactite) |
A rock of complex mineralogic composition formed
by contact metamorphism and metasomatism of carbonate rocks. It is
typically coarse-grained and rich in garnet, iron-rich pyroxene, epidote,
wollastonite, and scapolite. |
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Plutonic rock (phaneritic) |
A rock formed at considerable depth by
crystallization of magma and/or by chemical alteration. It is
characteristically medium- to coarse-grained, of granitoid
texture. |
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Alkalic intrusive rock |
A plutonic rock that contains more sodium and/or
potassium than is required to form feldspar with the available
silica. |
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Nepheline syenite |
A plutonic rock defined in the QAPF diagram as
having F/(F+A+P) between 10 an 60%, and P/(P+A) < 50%; composed
essentially of alkali feldspar and nepheline…[] |
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Aplite |
A light-colored igneous rock characterized by a
fine-grained allotriomorphic-granular (i.e. aplitic) texture. |
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Gabbroid |
A plutonic rock with Q < 20% or F < 10%,
P/(A+P) > 65%, and pl/(pl+px+ol) between 10 and 90%. |
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Anorthosite |
A plutonic rock defined in the QAPF diagram as
having Q between 0 and 5, P/(A+P) greater than 90, and M less than 10.
A group of monomineralogic plutonic igneous rocks composed almost
entirely of plagioclase feldspar… |
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Gabbro |
A plutonic rock defined in the QAPF diagram as
having Q between 0 and 5% or F/(F+A+P) < 10%, P/(A+P) greater than 90%
and plagioclase more calcic than An50[] |
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Norite |
A plutonic rock satisfying the definition of
gabbro, in which pl/(pl+px+ol) is between 10 and 90% and opx/(opx+cpx) is
greater than 95%. |
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Troctolite |
A plutonic rock satisfying the definition of
gabbro, in which pl/(pl+px+ol) is between 10 and 90% and px/(pl+px+ol) is
less than 5%. |
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Monzogabbro |
A plutonic rock defined in the QAPF diagram as
having Q < 5% or F/(F+A+P) < 10%, and P/(A+P) between 65 and 90%,
and plagioclase more calcic than An50 [] |
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Quartz gabbro |
A plutonic rock defined in the QAPF diagram as
having Q between 5 and 20%, P/(A+P) > 90%, and plagioclase more calcic
than An50[] |
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Quartz monzogabbro |
A plutonic rock defined in the QAPF diagram as
having Q between 5 and 20% and P/(A+P) between 65 and 90%, and plagioclase
more calcic than An50 [] |
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Granitoid |
A general term for all phaneritic igneous rocks
dominated by quartz and feldspars. |
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Alkali-granite (alaskite) |
A plutonic rock defined in the QAPF diagram as
having Q between 20 and 60% and P/(A+P) < 10%[] |
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Alkali syenite |
A plutonic rock defined in the QAPF diagram as
having Q/(Q+A+P) < 20% or F/(F+A+P) < 10%, and P/(P+A) <
10%…[] |
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Diorite |
A plutonic rock defined in the QAPF diagram as
having Q between 0 and 5% or F/(F+A+P) < 10%, P/(A+P) greater than 90%
and plagioclase more sodic than An50[] |
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Diabase |
A plutonic rock whose main components are
labradorite and pyroxene and which is characterized by ophitic
texture. |
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Granite |
A plutonic rock defined in the QAPF diagram as
having Q between 20 and 60% and P/(A+P) between 10 and 65%[] |
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Metaluminous granite |
A granite with aluminum oxide > sodium oxide
+ potassium oxide, but with aluminum oxide < sodium oxide + potassium
oxide + calcium oxide; typical accessories include: hornblende, epidote,
melilite, or biotite + pyroxene[] |
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Peralkaline granite |
A granite with aluminum oxide < sodium oxide
+ potassium oxide; typical accessories include: soda pyroxene and soda
amphibole[] |
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Peraluminous granite |
A granite with aluminum oxide > sodium oxide
+ potassium oxide + calcium oxide; typical accessories include: muscovite,
biotite, corundum, topaz, garnet[] |
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Subaluminous granite |
A granite with aluminum oxide approximately
equal to sodium oxide + potassium oxide; typical accessories include:
olivine, orthopyroxene, clinopyroxene[] |
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Granodiorite |
A plutonic rock defined in the QAPF diagram as
having Q between 20 and 60% and P/(A+P) between 65 and 90%[] |
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Monzodiorite |
A plutonic rock defined in the QAPF diagram as
having Q < 5% or F/(F+A+P) < 10%, and P/(A+P) between 65 and 90%,
and plagioclase more sodic than An50 [] |
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Monzonite |
A plutonic rock defined in the QAPF diagram as
having Q < 5% or F/(F+A+P) < 10%, and P/(A+P) between 35 and
65%[] |
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Quartz diorite |
A plutonic rock defined in the QAPF diagram as
having Q between 5 and 20%, P/(A+P) > 90%, and plagioclase more sodic
than An50[] |
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Quartz monzodiorite |
A plutonic rock defined in the QAPF diagram as
having Q between 5 and 20% and P/(A+P) between 65 and 90%, and plagioclase
more sodic than An50 [] |
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Quartz monzonite |
A plutonic rock defined in the QAPF diagram as
having Q between 5 and 20% and P/(A+P) between 35 and 65%[] |
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Quartz syenite |
A plutonic rock defined in the QAPF diagram as
having Q between 5 and 20% and P/(A+P) between 10 and 35%[] |
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Syenite |
A plutonic rock defined in the QAPF diagram as
having Q < 5% or F/(F+A+P) < 10%, and P/(A+P) between 10 and
35%[] |
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Tonalite |
A plutonic rock defined in the QAPF diagram as
having Q between 20 and 60% and P/(A+P) > 90%[] |
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Trondhjemite |
A tonalite with color index (M) less than 15;
composed essentially of sodic plagioclase, quartz, sparse biotite, and
little or no alkali feldspar[] |
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Intrusive Carbonatite |
A plutonic rock composed of at least 50%
carbonate minerals. |
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Pegmatite |
An exceptionally coarse-grained igneous rock,
with interlocking crystals, usually found as irregular dikes, lenses, or
veins, esp. at the margins of batholiths. |
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Porphyry |
An igneous rock of any composition that contains
conspicuous phenocrysts in a fine-grained groundmass. |
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Lamprophyre |
A group of porphyritic igneous rocks in which
mafic minerals form the phenocrysts; feldspars, if present, are restricted
to the groundmass. |
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Ultramafic intrusive rock |
A general name for plutonic rock with color
index (M) greater than or equal to 90… |
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Hornblendite |
A plutonic rock with M equal to or greater than
90 and hbl/(hbl+px+ol) greater than 90%. |
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Peridotite |
A plutonic rock with M equal to or greater than
90 and ol/(ol+opx+cpx) greater than 40%[] |
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Dunite |
A plutonic rock with M equal to or greater than
90 and ol/(ol+opx+cpx) greater than 90%[] |
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Kimberlite |
A porphyritic alkalic peridotite containing
abundant phenocrysts of olivine and phlogopite, and possibly geikielite
and chromian pyrope, in a fine-grained groundmass of calcite and
second-generation olivine and phlogopite… |
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Pyroxenite |
A plutonic rock with M equal to or greater than
90 and ol/(ol+opx+cpx) less than 40%. |
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Sedimentary rock |
A rock resulting from the consolidation of loose
sediment that has accumulated in layers… |
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Carbonate |
A sedimentary rock composed of more than 50% by
weight carbonate minerals. |
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Dolostone (dolomite) |
A carbonate sedimentary rock of which more than
50% by weight or by areal percentages under the microscope consists of the
mineral dolomite. |
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Limestone |
A sedimentary rock consisting chiefly (more than
50% by weight or by areal percentages under the microscope) of calcium
carbonate, primarily in the form of the mineral calcite… |
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Chemical |
A sedimentary rock composed primarily of
material formed directly by precipitation from solution or colloidal
suspension or by the deposition of insoluble precipitates. |
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Chert |
A hard, extremely dense or compact, dull to
semivitreous, microcrystalline or cryptocrystalline sedimentary rock,
consisting dominantly of interlocking crystals of quartz less than 30 µm
in diameter… |
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Evaporite |
A nonclastic sedimentary rock composed primarily
of minerals produced from a saline solution as a result of extensive or
total evaporation of the solvent. |
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Exhalite |
A chemical sedimentary rock, usually containing
oxide, carbonate, or sulfide as anions, and iron, magnesium, base metals,
and gold as cations, formed by the issuance of volcanically derived fluids
onto the sea floor or into the sea. |
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Iron formation |
A chemical sedimentary rock, typically
thin-bedded and/or finely laminated, containing at least 15% iron of
sedimentary origin, and commonly but not necessarily containing layers of
chert |
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Novaculite |
A dense, hard, even-textured, light-colored,
cryptocrystalline siliceous sedimentary rock, similar to chert but
characterized by dominance of microcrystalline quartz over
chalcedony. |
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Clastic |
A composed principally of broken fragments that
are derived from preexisting rocks or minerals and that have been
transported some distance from their place of origin. |
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Coarse-grained mixed clastic |
A mixture of clastic sedimentary rocks varying
from siltstone to conglomerate, dominated by rocks containing coarse
sand-sized or gravel-sized particles. |
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Conglomerate |
A coarse-grained clastic sedimentary rock,
composed of rounded to subangular fragments larger than 2 mm in diameter
typically containing fine-grained particles in the interstices, and
commonly cemented by calcium carbonate, iron oxide, silica, or hardened
clay… |
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Fine-grained mixed clastic |
A mixture of clastic sedimentary rocks varying
from mudstone to sandstone, dominated by rocks containing clay-sized or
silt-sized particles[] |
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Medium-grained mixed clastic |
A mixture of clastic sedimentary rocks varying
from siltstone to conglomerate, dominated by rocks containing sand-sized
particles[] |
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Mudstone |
A general term that includes claystone,
siltstone, shale, and argillite, and that should be used only when the
amounts of clay-sized and silt-sized particles are not known or specified,
or cannot be precisely identified… |
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Argillite |
A compact rock derived either from mudstone or
shale, that has undergone a somewhat higher degree of induration than
mudstone or shale but is less clearly laminated than shale and without its
fissility, and that lacks the cleavage distinctive of slate. |
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Claystone |
An indurated rock having more than 67%
clay-sized minerals. |
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Bentonite |
A soft, plastic, porous, light-colored rock
composed essentially of clay minerals of the montmorillonite (smectite)
group plus colloidal silica, and produced by devitrification and
accompanying chemical alteration of a glassy igneous material, usually a
tuff or volcanic ash. |
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Shale |
A laminated, indurated rock having more than 67%
clay-sized minerals. |
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Black Shale |
A dark, thinly laminated carbonaceous shale,
exceptionally rich in organic matter (5% or more carbon content) and
sulfide (esp. iron sulfide, usually pyrite), and often containing unusual
concentrations of certain trace elements (U, V, Cu, Ni). |
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Oil Shale |
A kerogen-bearing, finely laminated brown or
black sedimentary rock that will yield liquid or gaseous hydrocarbon on
distillation. |
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Siltstone |
An indurated silt having the texture and
composition of shale but lacking its fine lamination or fissility; a
massive mudstone in which silt-sized particles predominate over clay-sized
particles. |
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Olistostrome |
A sedimentary deposit consisting of a chaotic
mass of intimately mixed heterogeneous materials (such as blocks and muds)
that accumulated as a semi-fluid body by submarine gravity sliding or
slumping of unconsolidated sediments. |
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Mélange |
A body of rock characterized by a lack of
internal continuity of contacts or strata and by the inclusion of
fragments and blocks of all sizes, both exotic and native, embedded in a
fragmental matrix of finer-grained material. |
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Sandstone |
A medium-grained clastic sedimentary rock
composed of abundant sand-sized fragments, which may have a finer-grained
matrix (silt or clay), and which is more or less indurated by a cementing
material…[] |
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Arenite |
A “clean” sandstone that is well-sorted,
contains little or no matrix material, and has a relatively simple
mineralogic composition; specif. a pure or nearly pure, chemically
cemented sandstone containing less than 10% argillaceous
matrix. |
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Calcarenite |
A clastic sedimentary rock that is made up
predominantly of recycled carbonate particles of sand size; a consolidated
calcareous sand[] |
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Orthoquartzite |
A clastic sedimentary rock that is made up
almost exclusively of quartz sand (with or without chert), that is
relatively free of or lacks a fine-grained matrix; a quartzite of
sedimentary origin, or a “pure quartz sandstone”. |
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Arkose |
A feldspar-rich sandstone, commonly
coarse-grained and pink or reddish, that is typically composed of angular
to subangular grains that may be either poorly or moderately well sorted…
Quartz is usually the dominant mineral, with feldspars constituting at
least 25%. |
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Wacke |
A “dirty” sandstone that consists of a mixed
variety of unsorted or poorly sorted mineral and rock fragments and of an
abundant matrix of clay and fine silt; specif. an impure sandstone
containing more than 10% argillaceous matrix. |
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Graywacke |
…a dark gray, firmly indurated, coarse-grained
sandstone that consists of poorly sorted angular to subangular grains of
quartz and feldspar, with a variety of dark rock and mineral fragments
embedded in a compact clayey matrix having the general composition of
slate and containing an abundance of very fine-grained illite, sericite,
and chloritic minerals. |
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Sedimentary breccia |
A breccia (coarse-grained clastic rock composed
of angular broken rock fragments held together by a mineral cement or a
fine-grained matrix) formed by sedimentary processes[] |
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Coal |
A readily combustible rock containing more than
50% by weight and more than 70% by volume carbonaceous material, formed by
compaction and induration of variously altered plant remains… |
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Mixed clastic/carbonate |
An undivided mixture of clastic and carbonate
sedimentary rocks. |
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Mixed clastic/coal |
An undivided mixture of clastic sedimentary rock
and coal. |
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Mixed clastic/volcanic |
An undivided mixture of clastic sedimentary rock
and volcanic rock. |
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Phosphorite |
A sedimentary rock with a high enough content of
phosphate minerals to be of economic interest. |
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Tectonite |
A rock whose fabric reflects the history of its
deformation. |
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Augen gneiss |
Gneissic rock containing augen (large lenticular
mineral grains or mineral aggregates having the shape of an eye in cross
section) |
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Cataclasite |
A fine-grained, cohesive cataclastic rock,
normally lacking a penetrative foliation or microfabric, formed during
fault movement. |
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Flaser gneiss |
A dynamically metamorphosed rock in which lenses
or layers of original or relatively unaltered granular materials are
surrounded by a matrix of highly sheared and crushed material, giving the
appearance of a crude flow structure[] |
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Mylonite |
A compact, chert-like rock without cleavage, but
with a streaky or banded structure, produced by the extreme granulation
and shearing of rocks that have been pulverized and rolled during
overthrusting or intense dynamic metamorphism. |
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Phyllonite |
A rock that macroscopically resembles phyllite
but that is formed by mechanical degradation (mylonitization) of initially
coarser rocks… |
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Tectonic breccia |
A breccia formed as a result of crustal
movements, usually developed from brittle rocks. |
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Tectonic mélange |
A mélange produced by tectonic
processes. |
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Unconsolidated deposit |
A sediment that is loosely arranged or
unstratified, or whose particles are not cemented together, found either
at the surface or at depth. |
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Alluvium |
A general term for clay, silt, sand, gravel or
similar unconsolidated detrital material, deposited during comparatively
recent geologic time by a stream or other body of running water, as a
sorted or semi-sorted sediment… |
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Alluvial fan |
A low, outspread, relatively flat to gently
sloping mass of loose rock material, shaped like an open fan or a segment
of a cone, deposited by a stream (esp. in a semiarid region) at the place
where it issues from a narrow mountain valley upon a plain or broad
valley… |
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Alluvial terrace |
A stream terrace composed of unconsolidated
alluvium (including gravel), produced by renewed downcutting of the flood
plain or valley floor… |
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Delta |
The low, nearly flat, alluvial tract of land at
or near the mouth of a river, commonly forming a triangular or fan-shaped
plain of considerable area… |
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Flood plain |
Unconsolidated sediment deposited adjacent to a
river channel, constructed by the present river in its existing regimen
and covered with water when the river overflows its banks. |
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Levee |
A long broad low ridge or embankment of sand and
coarse silt, built by a stream on its flood plain and along both banks of
its channel, esp. in time of flood when water overflowing the normal banks
is forced to deposit the coarsest part of its load. |
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Biogenic sediment |
An organic sediment produced directly by the
physiologic activities of organisms, either plant or animal[] |
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Coral |
A hard calcareous substance consisting of the
continuous skeleton secreted by coral polyps for their support and
habitation and found in single specimens growing plant-like on the sea
bottom or in extensive, solidified accumulations (coral
reefs). |
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Peat |
An unconsolidated deposit of semicarbonized
plant remains in a water saturated environment, such as a bog or fen, and
of persistently high moisture content (at least 75%). |
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Clay or mud |
A loose, earthy, extremely fine-grained, natural
sediment composed primarily of clay-size or colloidal particles and
characterized by high plasticity and by a considerable content of clay
minerals… |
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Eolian |
Sediments such as loess or sand deposited by the
action of the wind[] |
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Dune sand |
A type of blown sand that has been piled up by
the wind into a sand dune, usually consisting of rounded mineral grains,
commonly quartz, having diameters ranging from 0.1 to 1 mm. |
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Loess |
A widespread, homogeneous, commonly
nonstratified, porous, friable, slightly coherent, usually highly
calcareous, fine-grained blanket deposit, consisting predominantly of silt
with subordinate grain sizes ranging from clay to fine sand. |
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Sand sheet |
A large irregularly shaped plain of eolian sand,
lacking the discernible slip faces that are common on dunes. |
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Glacial drift |
A general term applied to all rock material
(clay, silt, sand, gravel, boulders) transported by a glacier and
deposited directly by or from the ice, or by running water emanating from
a glacier. |
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Stratified glacial sediment |
Stratified glacial drift deposited by, or
reworked by running water, or deposited in standing water.[] |
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Glacial-marine |
Deposits of glacially eroded, terrestrially
derived sediment in the marine environment. |
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Glaciolacustrine |
Deposits and landforms composed of suspended
material brought by meltwater streams flowing into lakes bordering the
glacier, such as deltas, kame deltas, and varved sediments. |
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Outwash |
Stratified detritus (chiefly sand and gravel)
removed or “washed out” from a glacier by meltwater streams and deposited
in front of or behind the end moraine or the margin of an active
glacier. |
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Sub- and supra-glacial
sediment |
A variety of irregularly stratified sand and
gravel deposits, such as eskers, kames, etc., that were deposited by a
subglacial or supra-glacial stream or pond and were left behind when the
ice melted[] |
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Till |
Dominantly unsorted and unstratified drift,
generally unconsolidated, deposited directly by and underneath a glacier
without subsequent reworking by meltwater… |
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Moraine |
A mound, ridge, or other distinct accumulation
of unsorted, unstratified glacial drift, predominantly till, deposited
chiefly by direct action of glacial ice… |
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Gravel |
A loose accumulation of rock fragments composed
predominantly of more or less rounded pebbles and small
stones[] |
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Lake or marine deposit
(non-glacial) |
A sedimentary deposit laid down conformably on
the floor of, or along the shore of, a lake, sea, or ocean, usually
consisting of coarse material near the shore and sometimes passing into
clay and limestone in deeper water… |
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Beach sand |
A loose aggregate of unlithified mineral or rock
particles of sand size forming a beach (the relatively thick and temporary
accumulation of loose water-borne material that is in active transit
along, or deposited on, the shore zone between the limits of low water and
high water)[] |
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