Rock Identifier
Dolomite on Prehnite (Saddle-shaped Dolomite) (Dolomite [CaMg(CO3)2] on Prehnite [Ca2Al(AlSi3O10)(OH)2]) — mineral
mineral

Dolomite on Prehnite (Saddle-shaped Dolomite)

Dolomite [CaMg(CO3)2] on Prehnite [Ca2Al(AlSi3O10)(OH)2]

Hardness: 3.5-4 (Dolomite) and 6-6.5 (Prehnite). Color: Pearly white to cream crystals on a pale green/yellow matrix. Luster: Vitreous to pearly. Crystal structure: Trigonal (rhombohedral) for Dolomite, Orthorhombic for Prehnite. Cleavage: Perfect rhombohedral.

Hardness
3
Color
Pearly white to cream crystals on a pale green/yellow matrix
Luster
Vitreous to pearly
Identified More mineral

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Physical properties

Hardness: 3.5-4 (Dolomite) and 6-6.5 (Prehnite). Color: Pearly white to cream crystals on a pale green/yellow matrix. Luster: Vitreous to pearly. Crystal structure: Trigonal (rhombohedral) for Dolomite, Orthorhombic for Prehnite. Cleavage: Perfect rhombohedral.

Formation & geological history

Formed through hydrothermal processes where magnesium-rich fluids react with limestone or are precipitated in cavities. Often found in basaltic vugs or sedimentary basins. This specific 'saddle' shape is caused by crystal lattice distortion during growth.

Uses & applications

Primarily a collector's mineral specimen. Industrial dolomite is used in cement, as a source of magnesium, and as a flux in steel making. Prehnite is sometimes used as a minor gemstone or ornamental stone.

Geological facts

The characteristic curved 'saddle' shape of the dolomite crystals is a classic feature highly prized by mineralogists. Fine combinations of white dolomite on mint-green prehnite are most famously sourced from the Kayes Region of Mali.

Field identification & locations

Identify in the field by the curved rhombohedral crystals and the reaction to warm dilute hydrochloric acid (effervescence). Common locations include Mali, Morocco, and various trap rock quarries in New Jersey, USA. Collectors look for undamaged crystal 'saddles' and contrasting matrix colors.