Roger Weller, geology instructor
[email protected] copyright 2016-R.Weller
labradorite-plagioclase twinning
If this piece of labradorite is turned to
just right to the correct angle of a light
source, light is reflected off of a series of narrow strips on a cleavage surface. This
phenomenon, which is common for plagioclase feldspars, is called "plagioclase
twinning" or "polysynthetic twinning". The cleavage surface consists of two slightly
different crystal orientations which formed as the plagioclase cooled. Light is being
reflected off one set of microcleavage surfaces of one of the crystalline orientations.
If the crystal is tipped again slightly with respect to the light source, the other set of
reflecting cleavage surfaces will
reflect light. The reflections are very sharp lines.
feldspar
Photo is copyright free for
non-commercial educational uses.
Just credit photo to R.Weller/Cochise College.