Marl
“Where clay meets calcium”

Sedimentary
Marl is a sedimentary rock that's a natural mixture of clay and calcium carbonate (lime), typically forming in shallow marine or freshwater environments. For centuries it's been spread on agricultural fields to improve soil quality, a practice dating back to Roman times.
Composition
calcite, clay minerals, quartz, dolomite
Where Found
Champagne region (France), White Cliffs area (England), Niobrara Formation (Kansas, USA), Denmark
Mohs Hardness
2-3
Fun Fact
The famous chalky soils of the Champagne wine region are actually marl, and winemakers credit these soils with giving their sparkling wines their distinctive minerality.
Test Your Knowledge
Why was marl historically spread on agricultural fields across Europe?
Related Specimens
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