sedimentary

Conglomerate

Clastic Sedimentary Rock (Conglomerate)

Hardness: 6-7 (depending on clast types), Color: Tan to brown with white/grey quartz inclusions, Luster: Dull/Earthy matrix with waxy/vitreous clasts, Structure: Clastic with rounded fragments larger than 2mm, Cleavage: None

Identified May 14, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed through the lithification of rounded gravel and boulders. These usually accumulate in high-energy environments like fast-moving rivers, alluvial fans, or shorelines where water action rounds the stones over time.

Uses & applications

Used in the construction industry as coarse aggregate for concrete and road fill. Occasionally used as decorative dimension stone if the colors are striking.

Geological facts

Conglomerates are often referred to as 'puddingstone' because the rounded stones in the matrix resemble raisins or fruit in a pudding. They are key indicators of past aqueous environments on Earth and even Mars.

Field identification & locations

Identify by looking for rounded rock fragments (clasts) cemented within a finer-grained matrix. Often found in riverbeds or near mountain fronts. Collectors look for unique 'puddingstone' varieties with contrasting colors.

Other sedimentary specimens

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Sandstone or Siltstone

Arenite (if sandstone)

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Cone-in-cone structure (Limestone)

Cone-in-cone structure (Secondary Sedimentary Structure)

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Chert Breccia

Brecciated Chert (Microcrystalline Silica)

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Sandstone Grain

Clastic Sedimentary Rock Grain (SiO2 dominated)

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Shale or Slaty Mudstone

Argillaceous sedimentary rock

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Sandstone

Arenite (primarily SiO2)

sedimentary