Diatomite, also called diatomaceous earth, is a soft, siliceous sedimentary rock made of the fossilized silica remains of diatoms, microscopic single-celled algae that settled in lakes and seas. It crumbles to a fine white to off-white powder and has a low density because it is so porous. Marine deposits are worked in the Sisquoc Formation near Lompoc, California, and freshwater lake deposits occur in Nevada, Oregon, Washington and California, usually associated with volcanic rock. It is used to filter water, beer and wine and as an insecticide.
Is this diatomite?
3-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Read the textureLook at a fresh break with a hand lens. Texture: Soft, porous rock that crumbles to a fine powder. Grain size: typically 10 to 200 micrometres.
- 2Pick out the mineralsComposition: Fossilized diatom remains: 80 to 90 percent silica, mainly amorphous (opal), with minor clay and iron oxide. Identify the two or three most abundant grains.
- 3Match the color rangeCompare against the expected color range: white.
All properties
- Colors
- Uses
- Industrial
- Host rock
- Lake and marine sediments; lake deposits are almost always associated with volcanic rock
- Texture
- Soft, porous rock that crumbles to a fine powder
- Grain size
- typically 10 to 200 micrometres
- Composition
- Fossilized diatom remains: 80 to 90 percent silica, mainly amorphous (opal), with minor clay and iron oxide
Where rockhounds find diatomite
Classic worldwide localities
- Sisquoc Formation near Lompoc, California (marine)
- Nevada, Oregon, Washington and California (freshwater lake deposits)
- Maryland and Virginia (marine)
- Fur and Mors, Denmark (moler)
Field-hunting tip
Where it forms: Lake and marine sediments; lake deposits are almost always associated with volcanic rock.
