Rock Identifier
Calcilutite (Fine-grained limestone (calcium carbonate, CaCO3))
sedimentary

Calcilutite

Fine-grained limestone (calcium carbonate, CaCO3)

A very fine-grained, mud-sized limestone formed from carbonate mud, smooth and dense with conchoidal fracture.

Mohs hardness
3
Color
white, cream, gray to buff
Type
sedimentary

Got a rock like this?

Identify any rock from a photo, free.

Overview

Calcilutite is a textural term for a limestone made of mud-sized carbonate grains (finer than about 1/16 mm). The name parallels the siliciclastic term "lutite" (mudstone) but applies to calcium carbonate sediment. It overlaps closely with micrite and lime mudstone.

These rocks are dense, smooth, and homogeneous, often breaking with a conchoidal or splintery fracture. Because the grains are so fine, individual particles are invisible to the naked eye, giving the rock a uniform, porcelain-like appearance.

Calcilutite records quiet-water carbonate environments and is common in deeper or sheltered marine settings.

Formation & geology

Calcilutite forms from the accumulation of fine carbonate mud ("micrite") in low-energy marine environments where currents are too weak to winnow away fine particles. Sources of the mud include the breakdown of calcareous algae, fine skeletal debris, and direct chemical precipitation of aragonite and calcite.

Typical settings include lagoons, deep shelf and basin floors, and protected back-reef areas. Over time the carbonate mud is compacted and recrystallized into solid fine-grained limestone.

Famous fine-grained limestones such as the lithographic limestones of Solnhofen are calcilutites, valued for preserving exquisite fossils because of their quiet, fine-grained deposition.

How to identify it

Look for a dense, very fine-grained, light-colored rock — white, cream, gray, or buff — with a smooth feel and no visible grains. It typically breaks with a smooth conchoidal or splintery fracture.

The decisive field test is its vigorous fizzing in dilute hydrochloric acid, confirming it is carbonate. Its softness (about 3 on the Mohs scale, scratchable by a knife) separates it from fine chert and porcellanite, which are silica, much harder, and do not react with acid.

Compared with chalk it is denser and less powdery. Fossils, if present, are usually fine and well preserved.

Uses & significance

Fine-grained calcilutite has many of the uses of other limestones: it is quarried for building and dimension stone, crushed aggregate, cement and lime production, and agricultural lime. Its uniform, fine texture makes it excellent for carving and for taking a polish.

Historically, the finest, most even-grained varieties were famous as lithographic limestone used in printing, and as a medium for detailed sculpture. Fossil-rich calcilutites are scientifically valuable.

It has no gem or metaphysical role, but its workability and fine grain give it long-standing value to builders, sculptors, and printers.

Frequently asked questions

What does calcilutite mean?

It is a textural term for a limestone made of mud-sized (very fine) carbonate grains, the carbonate equivalent of a siliciclastic mudstone.

Is calcilutite the same as micrite?

They overlap closely. Micrite refers specifically to fine carbonate mud matrix, while calcilutite is the grain-size term for a rock dominated by that mud-sized carbonate.

How do I confirm it is limestone?

It fizzes vigorously in dilute hydrochloric acid and is soft enough to scratch with a knife, which separates it from hard, non-reactive silica rocks like chert.

Why are fine limestones good for fossils?

They form in quiet water from fine mud, which gently buries organisms and preserves delicate detail, as in the famous Solnhofen lithographic limestone.

What is calcilutite used for?

It is used for building stone, crushed aggregate, cement and lime, agricultural lime, carving, and historically for lithographic printing.