
mineral
Kidney Stone (Renal Calculus)
Calcium oxalate monohydrate (Whewellite) / CaC2O4·H2O
Hardness: Approx 2.5-3 (Mohs). Color: Brown, tan, or grey. Luster: Dull to earthy. Crystal structure: Monoclinic. Cleavage: Poor. Specific gravity: Approx 2.2.
- Hardness
- Approx 2
- Color
- Brown, tan, or grey
- Luster
- Dull to earthy
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Physical properties
Hardness: Approx 2.5-3 (Mohs). Color: Brown, tan, or grey. Luster: Dull to earthy. Crystal structure: Monoclinic. Cleavage: Poor. Specific gravity: Approx 2.2.
Formation & geological history
Formed through the precipitation and crystallization of minerals (usually calcium oxalate) within the human kidney over months or years, often due to dehydration or metabolic imbalances.
Uses & applications
Medical diagnostic value; primarily analyzed in clinical laboratories to determine physiological causes of stone formation.
Geological facts
Kidney stones are biological minerals. While they are not formed in mother Earth, they are chemically and structurally identical to geological whewellite crystals found in carbonaceous veins.
Field identification & locations
Identify by its irregular, often jagged 'burr' shape and granular surface. Common in individuals with high dietary oxalate intake or low fluid intake.
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