Below is a typical view of olivine in plane polarized light. Note the highrelief and the low-relief alteration products between grains.
Same field in crossed polars, showing the "stained glass window"appearance.
Return to Mineralogy-Petrology Index
Return to Thin-Section Index
Return to Crystals and Light Index
Return to Crystal Structures Index
Return to Mineral Identification Tables
Return to Professor Dutch's Home Page
Created 22 Sept 1997, Last Update