Quantitative and qualitative studies of the shape characteristics of both natural and artificially prepared particles combine with evidence from diverse other sources to suggest strongly that the quartz of granitic rocks and gneisses is repeatedly fractured and healed in an intricate manner before being presented at the Earth's surface and that, in the zone of weathering, this quartz is parted along some of the resulting incipient fractures. The quartz fractures are thought to originate when granitic rocks pass through a state wherein their quartz is brittle while the surrounding feldspar is still ductile. Experimental evidence supports the view that the pattern of fractures affecting granitic quartz is characteristic of the breakage of particles of a brittle solid embedded in a ductile, deforming matrix. This process produces particles that are often remarkably equant and rounded for breakage products.