Lab Proponent Flashcards
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Peridotite, Phaneritic, ultra mafic, green rock made at high tempretures
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Talc, slippery surface, sillicate, irregular fracture, hardness 2
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Dolomite, no reaction with HCL unless powdered, harness 4, rhobohedral cleavage, carbonate, CaMg(CO3)2
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Chalcopyrite, distinguished by their hardness. Chalcopyrite is a soft mineral that can be scratched by a nail, while pyrite is hard enough that a nail cannot dig into its surface, CuFeS2, Sulfide
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Scoria, Rusty red ground mass with an aphanitic and vesicular texture, forms as an extrusion of cooling high temp lava
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Sphalerite, browninsh orange streak, 6 cleavage planes, sulphide, ZnS
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Shale, dull, reddish- brown, very fine grains (smooth to the touch), breaks easily. If an edge is dipped in water and drawn along a surface, shale will leave a muddy streak.
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Galena,Its perfect cubic cleavage, metallic luster, lead-gray color, and relative softness readily distinguish galena from most other metallic minerals. Perhaps its most distinctive feature though, is its very high density, PbS, Sulfide
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Quartz sandstone, coarse grained quartz sand with cross bedding, mycrocrystaline texture
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Diorite, mainly made of amphibole, phaneritic and intermediate rock made from slow cooling of intermediate magma at a depth
Nonferrromagnesian silicates
Muscovite, K-Feldspar, Quartz
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Biotite mica, hardness 2, basal cleavage, dark in colour, silicate
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Lithic sandstone, Sandy texture, well sorted grains and grain size pretty uniform
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Soap stone, Soapstone is soft and can be scratched with a fingernail. Polished and unpolished soapstone both offer a waxy, soap-like feel and a pearly or silky luster.
Metamorphic rocks
1)Slate
2)Gneiss
3)Quartzite
4)Marble
5)Schist
6)Soap stone
7)Phyllite
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Rhyolite,Light pink/reddish ground mass, aphanitic and flesic. Forms from low temperature lava extrusions or shallow intrusions
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Muscovite, hardness 2, basal cleavage, white or light in colour
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Marble, Coarse texture, made of limestone and fizzles under acid, formed from both contact and regional metamorphisim
Sulphates
Gypsum, anhydrite
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Arkose sandstone, coarse-grained enough that feldspar grains (which are usually rather angular) can be easily seen with the unaided eye, poorly sorted
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Chert, the waxy luster, a conchoidal (shell-shaped) fracture of the silica mineral chalcedony that composes it, a hardness of seven on the Mohs scale, and a smooth (non-clastic) sedimentary texture.
Igneous rocks
1)Granite
2)Granodiorite
3)Basalt
4)Dacite
5)Rhyolite
6)Diorite
7)Peridotite
8)Scoria
9)Gabbro
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Gneiss, Foliated, medium to coarse grain made of schist or phylite and formed from regional metamorphisim
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Magnetite, heavy, magnetic, fracture, hardness 5.5-.5, black streak, oxide,Fe3O4
Carbonates
Calcite, dolomite
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Phyllite has a marked fissility (a tendency to split into sheets or slabs) due to the parallel alignment of platy minerals; it may have a sheen on its surfaces due to tiny plates of micas. Its grain size is larger than that of slate but smaller than that of schist.
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Pyrite, brassy metallic luster, black streak, brittle fracture, hardness greater than that of glass, absence of cleavage and it is nonmagnetic Fe2S, Sulfide
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Chalk, Chalky texture, made of calcite, Carbonate mineral and will react with acid
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Quartz, Hardness 7, fracture, SiO2, Non metallic
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K feldspar, lack striations, 2 cleavage, 6-6.5 hardness,silicate,potassium feldspars commonly have pink to reddish hues
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Dacite, porphrytic texture, grey ground mass with ampibole crystals, felsic and formed from low temp lava
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Obsidian, volcanic glass formed from extremly quick cooling of lava
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Granodiorite, contains quarts, coarse grained and flesic, granodiorite contains more plagioclase (calcium and sodium) feldspar than potassium feldspar and has more dark minerals in it. Formed from slow cooling at low tempreture
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Pumice, comprised of tiny shards of volcanic glass, it is light weight and rough to the touch
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Oolithic sandstone, Well sorted, reacts with acid, a type of sedimentary rock, usually limestone, made up of ooids cemented together. An ooid is a small spherical grain that forms when a particle of sand or other nucleus is coated with concentric layers of calcite or other minerals. Ooids most often form in shallow, wave-agitated marine water.
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Micrite, Dense, uniform, fine grained rock with conchoidal fracture. Reacts with acid and is made of calcite.
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Halite,its distinctive taste, combined with its perfect cubic cleavage, low hardness, and the ease with which small fragments dissolve in water should make it easy to identify. NaCl, Halide
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Basalt, Fine grained dark mineral, mafic, formed from fast cooling of high temp lava
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Coal, is blocky and appears shiny and smooth when you first see it, but look closer and you might see it has thin, alternating, shiny and dull layers
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Granite, Felsic, contains quartz,feldspar, and biotite, coarse grained, formed from slow cooling at a low temp
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Fluorite, 4 cleavage planes, hardness 4,octahedral cleavage, halide, CaF2
Sulfides
Galena, pyrite
Halides
Halite, fluorite
Ferromagnesian silicates
Biotite, olivine, pyroxene
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Schist, Foliated, made of mudstone,shale,slate or phyllite, black colour with garnets embedded, formed from regional metamorphsim
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Calcite, Rhombohedral cleavage, white streak, hardness 3, fizzles under acid, Carbonate, CaCo3
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Quartzite, NF, sandy texture, hardness 7, DOES NOT REACT WITH ACID, regional metamorphic and contact metamorphic
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Horneblend, hardness 5-6,black,. It tends to form slender prismatic to bladed crystals, diamond-shaped in cross section, or is present as irregular grains or fibrous masses.
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Pyroxene, pyroxenes have two cleavages at roughly 90,hardness between 5 and 7
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Conglomerate, Rock fragments that are gravel sized and poorly sorted
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Na feldspar, Striations, 2 cleavage, silicate
Steps in identifying Minerals
1)Lustre
2)Streak
3)Hardness
4)Cleavage
5)MISC properties
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Porphyritic garbbo, phanertiic texture, mafic rock formed at a depth, larger grains than basalt
Steps in identifying sedimentary rocks
1)Grain size
2)Composition
Steps in identifying igneous rocks
1)Ground mass colour
2)Identifyiable minerals
3)Texture
4)Felsic, intermediate,mafic, ultra mafic
Sedimentary rocks
1)Congolmerate
2)Quartz sandstone
3)Arkose sandstone
4)Lithic sandstone
5)Shale
7)Chalk
8)Oolitic limestone
9)Micrite
10)Coal
11)Chert
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Slate, fine grained, slaty cleavage, made of mudstone or shale, layered with a smooth texture and forms from regional metamorphisim
Oxides
Hematite, magnetite, ice
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Gypsum, white earthy masses or as clear crystals. In crystal form, its softness and single perfect cleavage with two less well-developed cleavage directions usually serve to distinguish gypsum from other similar-looking minerals. Hardness 2, CaSO4, Sulphate
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Ca feldspar,possible striations, dark colour
Steps in identifying metamorphic rocks
1)Foliated or nonfoliated
2)Grain size
3)Distinguishing charachteristics
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Hematite, When hematite is scratched on a rough surface, it leaves a reddish-brown streak,Fe2O3, Oxide
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Olivine, green and gemmy quality with small crystals, silicate, hardness 7. (Mg,Fe) 2SiO 4
Quartz chemical formula
SiO2
Calcite chemical formula
CaCo3
Magnetite chemical formula
Fe3O4
Olivine Chemical formula
Fe2SiO4
Dolomite chemical formula
CaMg(Co3)2
Sphalelite Chemical formula
ZnS
Flourite Chemical formula
CaF2
Galena Chemical formula
PbS
Pyrite Chemical formula
FeS2
Chalacopyrite Chemical formula
CuFeS2
Gypsum Chemical formula
CaSO4