
sedimentary
Flint (worked into an arrowhead)
Silicon dioxide (SiO2) - Microcrystalline Quartz
Hardness: 7 on Mohs scale. Color: Dark gray to brown-black. Luster: Waxy to dull. Fracture: Conchoidal with sharp edges. Microcrystalline/cryptocrystalline structure.
- Hardness
- 7 on Mohs scale
- Color
- Dark gray to brown-black
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 on Mohs scale. Color: Dark gray to brown-black. Luster: Waxy to dull. Fracture: Conchoidal with sharp edges. Microcrystalline/cryptocrystalline structure.
Formation & geological history
Forms as nodules in sedimentary rocks, particularly chalk or limestone, from the accumulation of siliceous organism remains (like sponge spicules) in deep marine environments.
Uses & applications
Historically used for stone tools, projectile points, and fire-starting (spark generation). Modern specimens like this are often crafted for jewelry pendants, lapidary art, or replica artifacts.
Geological facts
Flint fractures with extremely sharp, predictable conchoidal edges when knapped, making it the most important material for Stone Age tools and weapons. It was heavily traded across prehistoric trade networks.
Field identification & locations
Identified by its distinctive curved, shell-like conchoidal fractures, hardness (scratches glass), and dark waxy appearance. Commonly found in chalk deposits throughout Europe, North America, and North Africa.
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