its chemical formula is written using special notation that tells us about its composition
shows the chemical formulas of the pure compounds at the two ends of the “range of composition” that the solid solution can have (ie. the diff possibilities for the formula)
pure compounds = the 2 or more compounds that, when mixed together in varying proportions, give rise to the solid solution
present in smaller amounts
commonly replace major elements
sometimes part of chemical formula
found in very small amounts
can either replace a major element or occupy “holes” in the structure
mostly not included in written chem. formulas
allows for substitution of elements, which affects the mineral's properties
especially important for gemstones, where minor and trace elements can substitute for major elements in a mineral
caused by light absorption/refraction of certain wavelengths from:
foreign atom (trace element) presence
absence of atom/ionic radial typically present (called vacancy; result is a “color center”)
mineral structure
appearance of mineral’s surface in reflected light, with 2 types:
metallic
untarnished metal surface, opaque to light
non-metallic
lighter colour, degree of transparency (even if only on thin edges)
described w multiple terms: vitreous, adamantine, resinous, pearly, greasy, silky, satin, earthy
color of powder produced when drawn across a surface, useful for diagnosis bc:
mineral’s streak is more consistent than color (on unweathered surface)
can distinguish between similar minerals
ability of mineral to break along flat, planar surfaces + occurs at weakest points of atom bonding.
surface is generally smooth, evenly reflect light
consistent property; useful for diagnosis
described by direction re: crystal faces (cubic, prismatic, basal) + how easy its produced (perfect = clvg easily produces smooth/lustrous surfaces)
can have multiple directions or not be present at all
ease or difficulty that a mineral can be scratched
important diagnostic property
measured by Mohs scale (1-10)
more hydrous minerals = soft, anhydrous/silicate = hard (>5)
unrelated to toughness/strength
measurement of change of velocity + direction when light passes through trans(parent/lucent) mineral
ref. index = ratio of velocity of light in air, to its velocity in the crystal
high index = light disperses into its component colors (gives “fire”)
identified (by noobs) w special liquids or inexpensive equipment
measure of the density of a substance, using ratio of (substance mass) to (mass of equal volume of water)
ie. mineral w SG 2 = 2x heavy as water of same volume
found by using special balances OR liquids that allow minerals of below certain SG to float
when minerals emit coloured visible light under UV radiation
found by using UV light
inconsistent; less reliable diagnostic indicator
triclinic: no perpendicular axes, the three axes are of unequal length.
monoclinic: one axis perpendicular to a plane of two other axes of unequal length.
orthorhombic: three perpendicular axes of unequal length.
tetragonal: one axis perpendicular to a plane of two other axes of equal length.
hexagonal: three axes of equal length in a horizontal plane and a fourth axis perpendicular to the plane.
cubic (isometric): three axes of equal length that intersect at right angles.
involves using polyhedral shapes to visualize how different elements interact in 3D to create crystals
tetrahedra, octahedra, cubes
central cation is surrounded by a number of anions, and faces are drawn between the outside anions to form the polyhedral shape.