Lesson 3 Minerals and Rocks Flashcards
(53 cards)
naturally occurring not man made
inorganic
solid
definite chemical composition
ordered internal structure
mineral
quality and intensity of reflected light exhibited by the mineral
luster
generally opaque and exhibit a resplendent shine similar to a polished metal
metallic
vitreous (glassy) adamantine (diamond like) resinous, silky, pearl, dull, greasy
non metallic
measure of resistance of a mineral to abrasion or scratch
hardness
unique identifying property of minerals and maybe a poor indicator
color
color of mineral in powdered form
streak
golden color black or dark gray streak
pyrite
the ability of mineral to break along planes of weak bonding
cleavage
some minerals may not have cleavages but may exhibit broken surfaces that are irregular and non planar
fracture
it is the ratio of the weight of a mineral to the weight of an equal volume of water
specific gravity
silicon 28% and oxygen 47% over 90% of the rock forming minerals belong to this group
silicates
minerals containing oxygen anion (-O2) combined with one or more metal ions
oxides
minerals containing sulfur and oxygen anon (S04) combined with other ions
sulfates
contains sulfur anion (S2) combined with one or more ions
sulfides
contains carbonate anion (C03) 2- combined with other elements
carbonates
contains halogen elements combined with one or more elements
halides
minerals that form as individual elements
native elements
minerals with high thermal and electrical conductivity, typically with metallic luster, low hardness
metals and inter metals
more fragile than metals and have lower conductivity
semi metals
formed when magma or lava cool to a solid form, either glass or masses of tightly inter grown mineral crystals
igneous
formed from magma and tends to take a long time to solidify into rock has phaneretic textures
intrusive or plutonic
formed from lava and tends to solidify quickly common textures include aphanitic and porphyritic
extrusive or volcanic
fine grained, not visible to the naked eye, relatively fast rates of cooling/solidification prevent the formation of large crystals
aphanitic