
sedimentary
Puddingstone
Polymictic Conglomerate
Hardness: 6.5-7 (Mohs scale), Color: Cream or gray matrix with red, brown, or black clasts, Luster: Dull to waxy, Crystal structure: Amorphous/Microcrystalline, Specific gravity: 2.6-2.7
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Cream or gray matrix with red, brown, or black clasts, Luster: Dull to waxy, Crystal structure: Amorphous/Microcrystalline, Specific gravity: 2.6-2.7
Formation & geological history
Formed through the deposition of rounded jasper pebbles and quartz sand in high-energy river environments, subsequently lithified by silica cement roughly 2.3 billion years ago (Huronian Supergroup).
Uses & applications
Used primarily for lapidary work, jewelry, ornamental carvings, and as a popular collector's item due to its unique aesthetic appearance.
Geological facts
Famous varieties include the St. Joseph Island Puddingstone found in the Great Lakes region and the Hertfordshire Puddingstone in the UK, which was once believed to ward off evil.
Field identification & locations
Identify by looking for rounded red jasper 'raisins' embedded in a very hard, light-colored quartzite matrix. Commonly found on beaches along the North Shore of Lake Huron and throughout Michigan.
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