Identification of Minerals Flashcards
Observations during PPL
Opacity
Habit, Form, mode of aggregation
Color
Pleochroism
Cleavage
Observations during XPL
Isotropic vs Anisotropic
Habit
Cleavage
Interference color
Sign of elongation
Extinction and ext angles
Twinning, zoning
Function of the wavelength transmitted by the mineral
Color
Color is best observed in?
PPL
the ability of a mineral to absorb different wavelengths of transmitted light depending upon its crystallographic orientation.
Pleochroism
Pleochroic hexagonal and tetragonal minerals
twofold pleochroism; dichroic
exhibit varying degrees of absorption
Biaxial minerals
Exhibit three different colors
trichroic
darkest at long axis oriented perpendicular to polarizer
“normal” pleochroism
darkest at long axis oriented parallel to polarizer
“reverse” pleochroism
The degree to which mineral grains stand out from the mounting medium, have sharp boundaries, show fractures and cleavages well
Relief
without regular crystal faces
anhedral
has well-formed crystal faces
euhedral
elongate needlelike grains
acicular
elongate, slender
bladed
shaped like a column
columnar
equidimensional grains
equant
individual grains are long slender fibers
fibrous
flat elongate grains
lathlike
the dominant faces are those of a prism
prismatic
shaped like a book
tabular
more or less parallel tabular or platy grains; flaky
foliated
equant grains, all about the same size
granular
elongate grains in a random pattern
matted