sedimentary

Conglomerate

Clastic Conglomerate (Lithic-rich)

AI-generated identification · may be incorrect

Hardness: 3-7 (variable based on clasts); Color: Reddish-brown matrix with maroon/grey rounded clasts; Luster: Dull/Earthy; Structure: Clastic with rounded pebbles (>2mm); Specific Gravity: 2.6-2.8.

Hardness: 3-7 (variable based on clasts)
Color: Reddish-brown matrix with maroon/grey rounded clasts
Luster: Dull/Earthy

Identified April 25, 2026More sedimentary →

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Physical properties

Hardness: 3-7 (variable based on clasts); Color: Reddish-brown matrix with maroon/grey rounded clasts; Luster: Dull/Earthy; Structure: Clastic with rounded pebbles (>2mm); Specific Gravity: 2.6-2.8.

Formation & geological history

Formed through the lithification of rounded gravel and pebbles, typically in high-energy environments such as riverbeds, alluvial fans, or beaches. The reddish hue indicates an iron-rich (hematite) cementing matrix, common in terrestrial deposition environments.

Uses & applications

Used primarily as low-grade construction aggregate, fill material, and decorative landscaping stones. Exceptional specimens are sometimes used as architectural stone or for lapidary rough.

Geological facts

Conglomerates are known as 'puddingstones' because they resemble fruit in a pudding. They are key indicators of ancient water flow and have even been discovered on Mars by the Curiosity rover, proving past water movement there.

Field identification & locations

Identify in the field by looking for rounded, water-worn pebbles cemented within a finer-grained matrix. It is commonly found in sedimentary basins and eroded mountain foothills. Collectors should look for 'matrix-supported' vs 'clast-supported' structures.