Roger Weller, geology instructor
[email protected]
copyright
2010-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 micro cleavage 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.
labradorite
4
Photo is copyright free for
non-commercial educational uses.
Just credit photo to R.Weller/Cochise College.