A variety of obsidian from Glass Buttes, Oregon, named for thin layers showing various colors and known as ‘fire’ obsidian, was investigated with FE-SEM, EDS, EBSD, and optical spectroscopy methods. Our study reveals that the thin layers consist of mainly concentrated nano-sized magnetite crystals. The thin layers having a thickness of 300 nm to 700 nm give rise to brilliant colors in reflection. The color is caused by thin-film interference where the thin layers have a higher calculated refractive index (n=1.495 ~1.512) than that of the host glass (n=1.484).
Fire obsidian in the host rock.
The data will be available once the paper is published
Fig 1a Fig 1b samples
Fig 2 in host rock
Fig 3a Fig 3b Fig 3c Fig3d (jpg files) visible appearance - Images are not available at this time
Fig 4 optical spectrum Fig 4 (large version)
Fig 5a Fig 5b Fig 5c Fig 5d (tif files - use 'save as') SEM images
Fig 6a (bmp file) Fig 6b (jpg file) EBSD patterns
Canadian Mineralogist 45, 551-557