Rockby LogoRockby

How to identify Septarian Nodule

Septarian Nodule (calcite-filled concretions)

Got a photo? Identify rocks instantly with the Rockby app

Open the app

To correctly identify Septarian Nodule (Septarian Nodule (calcite-filled concretions)), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.

Step-by-step identification

  1. 1

    Color

    Overall color and any zoning or banding

    Exterior: Dull brown, gray, or yellowish-brown. Interior: Dark brown to gray matrix with bright yellow, orange, or white calcite veins; sometimes dark brown aragonite or black pyrite.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Exterior: Dull, earthy. Interior (calcite): Vitreous to pearly. Interior (aragonite): Vitreous. Interior (pyrite): Metallic.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Exterior: Rough, bumpy, often resembling a potato or turtle shell. Interior: Smooth to crystalline within the septa.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    The calcite within the septa typically forms dogtooth spar crystals (scalenohedral) or rhombohedral crystals. Aragonite may form acicular or radiating crystals. The overall nodule is spherical to ovoid.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Calcite: Perfect rhombohedral cleavage in three directions (1011). Aragonite: Distinct cleavage in one direction (010) and imperfect in two others (110, 011).

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found embedded in marine sedimentary rocks, particularly shales, mudstones, and marls, often associated with ancient sea beds where organic matter was abundant.

Key Facts

Hardness
Matrix: 3-4 (depending on composition). Calcite: 3 on Mohs scale. Aragonite: 3.5-4 on Mohs scale. Pyrite: 6-6.5 on Mohs scale.
Specific Gravity
2.6-2.9 (variable depending on mineral infill and matrix density). Calcite: 2.71. Aragonite: 2.95.
Crystal System
Calcite: Trigonal. Aragonite: Orthorhombic. The nodule itself is amorphous in overall shape but contains crystalline infillings.
Color
Exterior: Brown, gray, yellowish-brown. Interior: Dark gray/brown matrix, yellow/orange/white calcite, sometimes dark brown aragonite or black pyrite.
Luster
Earthy (exterior), Vitreous to Pearly (calcite), Vitreous (aragonite), Metallic (pyrite).
Transparency
Opaque (matrix), Translucent to Transparent (calcite/aragonite crystals).
Fracture
Conchoidal to uneven (calcite), Subconchoidal (aragonite), Irregular (matrix).
Cleavage
Calcite: Perfect rhombohedral (3 directions). Aragonite: Distinct (1 direction), imperfect (2 directions).
Composition
Primarily a clay-rich or mudstone matrix (silicates, aluminosilicates) with secondary mineral infillings of calcium carbonate (calcite, aragonite), sometimes barium sulfate (barite), or iron sulfide (pyrite).

Physical characteristics

  • Crystal Habit: Nodular to ovoid external form. Internal calcite often forms scalenohedral (dogtooth spar) or rhombohedral crystals. Aragonite can be acicular or radiating.
  • Cleavage Type: Calcite: Perfect rhombohedral. Aragonite: Distinct to imperfect.
  • Fracture Type: Conchoidal to uneven for crystalline infillings; irregular for the matrix.
  • Tenacity: Brittle.
  • Luster Type: Earthy (exterior), Vitreous to Pearly (calcite), Vitreous (aragonite), Metallic (pyrite).

Explore Septarian Nodule

Identify rocks anywhere

Free on iOS, Android, and Web. Photo identification, full database, and your personal collection.

Open in app