Rock Identifier
Kidney Stone (Renal Calculus) (Calcium oxalate monohydrate (Whewellite) / CaC2O4·H2O) — mineral
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
Identified More mineral

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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.