sedimentary

Chalk

Micrite (primarily Calcium Carbonate, CaCO3)

AI-generated identification · may be incorrect

Hardness: 1-3 (Mohs scale); Color: White to light grey; Luster: Dull/Earthy; Structure: Fine-grained, porous; Cleavage: None; Specific Gravity: 2.4-2.6

Hardness: 1-3 (Mohs scale)
Color: White to light grey
Luster: Dull/Earthy

Identified April 17, 2026More sedimentary →

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Physical properties

Hardness: 1-3 (Mohs scale); Color: White to light grey; Luster: Dull/Earthy; Structure: Fine-grained, porous; Cleavage: None; Specific Gravity: 2.4-2.6

Formation & geological history

Formed in deep marine conditions from the accumulation of microscopic skeletal remains of calcareous algae (coccoliths) and plankton. Primarily associated with the Cretaceous period.

Uses & applications

Used in the manufacturing of portland cement, lime, and bricks. Formerly used extensively as a writing medium on blackboards. Used in agriculture to treat acidic soils and in sports for better grip.

Geological facts

The famous White Cliffs of Dover in England are composed primarily of chalk. Most modern 'blackboard chalk' is actually made of gypsum, though historically it was made from natural chalk.

Field identification & locations

Identify in the field by its soft, powdery texture that easily rubs off on fingers and its vigorous reaction (effervescence) when touched with dilute hydrochloric acid. Commonly found in coastal areas or former seabed deposits.