How gypsum is quarried
Gypsum is a mineral so soft you can scratch it with a fingernail, and it holds water inside its crystals.
- stations
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- things downstream
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The short version
Gypsum is a soft calcium sulfate mineral that forms thick beds when seawater or salty lakes dry up. It is dug from open quarries or underground mines, crushed and sorted. Heating it later drives off the water locked in its crystals, leaving the powder called plaster of Paris.
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Quarry the evaporite bed
Gypsum forms thick, extensive beds in sedimentary rock where water evaporated long ago. Quarries drill and blast the beds, or underground mines follow them.
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Crush to chips
Quarried rock is crushed and screened. Because gypsum is soft, it breaks down without much effort.
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Sort for the plant
Material is graded by purity and size. Most of it goes to a plant that heats it to make plaster, or sets it into wallboard, and some goes to farms as a soil amendment.
Worth repeating
- Heating gypsum drives off water and leaves plaster of Paris, named for the quarries of the Montmartre district of Paris.
- Gypsum crystals called selenite can grow up to 12 m long, among the largest crystals found in nature.
- At White Sands National Park in New Mexico, 710 square kilometers of the dunes are made of gypsum sand.
Where it goes next
Gypsum feeds 5 lines directly and reaches 10 things in total.
Further down the line
Keep walking
Sources
Cite this page: "How gypsum is quarried." Assembly Line, 2026-11-03. https://assemblyline.org/make/gypsum