Geological Ages and Biblical Interpretations of Fire Obsidian Formation
This specimen is an exceptional piece of Fire Obsidian from Lake County, Oregon, measuring 73x31x9 mm. Fire Obsidian is a rare type of naturally occurring volcanic glass distinguished by its intense, vibrant, iridescent, non-metallic sheen, which displays a rainbow of colors like red, orange, yellow, green, and blue. This striking iridescence is an optical effect caused by the thin, aligned layers of nanocrystals of magnetite within the glass, which interfere with light. Obsidian, a silica-rich igneous rock, forms when felsic lava cools very rapidly, preventing the diffusion of atoms necessary for crystal growth. Fire obsidian specifically is found in rhyolitic flows, where the lava's high viscosity and quick cooling create the glass structure, and subsequent geothermal activity or weathering can create the conditions for the thin magnetite layers. The source region, often associated with Glass Buttes in Lake County, Oregon, is geologically significant. The volcanic act...