Shape (ideal) Cleavage Relief Colour (natural) Interference Colour Twinning Other features
Olivine One (poor) high colourless intermediate - Irregular fractures, often associated with alteration to serpentine (+ opaque Fe oxides)
Orthopyroxene Two (90° ) high colourless or v. pale grey low - Most sections show 1 cleavage and straight extinction. May exsolve augite
Augite high pale grey-brown intermediate occasional (simple or multiple) Most sections show 1 cleavage and oblique extinction
Hornblende Two (60/120°) high green / brown pleochroic intermediate occasional (simple or multiple) Most sections show 1 cleavage and oblique extinction. May be altered to chlorite
Biotite One mod brown pleochroic intermediate - Sections showing cleavage have straight extinction. Speckled appearance close to extinction. Biotite alters to chlorite
Muscovite mod colourless intermediate -
Quartz - low colourless low - Always unaltered. Deformation may cause patchy extinction
Feldspar Two (~90°) low colourless low common Typically some degree of alteration to clay minerals (fine particles) and small flakes of secondary muscovite (sericite)
(Plagioclase) " " " " multiple (mainly 1 direction) ± simple (same direction) Alteration as above but may also produce small grains of epidote
(K-Feldspar - Sanidine) " " " " simple Often unaltered and easily confused with quartz. Look for cleavage and twinning.
Orthoclase) " " " " simple Often shows exsolution of Na-rich feldspar = perthite
Microcline) " " " " multiple in 2 directions (~90°) on fine scale
Garnet - high colourless (grey) or pale brown isotropic -

Common Opaque Minerals

Haematite - deep red in thin flakes

Magnetite - equant grains

Chromite - equant grains

Ilmenite - elongate crystals

Calcite Three (not 90°) low colourless high multiple
Apatite - mod colourless low -
Zircon - v. high colourless (grey) intermediate -
Sphene Two v. high pale brown high simple