
sedimentary
Ferruginous Conglomerate
Conglomerate with Iron-Oxide Matrix (SiO2 + Fe2O3/FeO(OH))
Hardness: 6-7 (clasts), 4-5 (matrix); Color: Dark brown, rusty red, and grey; Luster: Dull/Earthy; Structure: Clastic (coarse-grained); Cleavage: None (breaks across grains); Specific Gravity: 2.6 - 3.2 (varies by iron content)
- Hardness
- 6-7 (clasts), 4-5 (matrix)
- Color
- Dark brown, rusty red, and grey
- Luster
- Dull/Earthy
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Physical properties
Hardness: 6-7 (clasts), 4-5 (matrix); Color: Dark brown, rusty red, and grey; Luster: Dull/Earthy; Structure: Clastic (coarse-grained); Cleavage: None (breaks across grains); Specific Gravity: 2.6 - 3.2 (varies by iron content)
Formation & geological history
Formed in high-energy fluvial environments (rivers) or alluvial fans where rounded rock fragments are deposited and later cemented together by iron-rich groundwater precipitating minerals like hematite or goethite. Age ranges from Precambrian to Cenozoic depending on the local basin.
Uses & applications
Used primarily as low-grade construction aggregate, fill material in road building, or as a decorative stone in landscaping. Historically, some high-iron variants were prospected as minor iron ores.
Geological facts
Conglomerates are often called 'puddingstone' because the rounded clasts resemble fruit in a pudding. Because the clasts are rounded, they indicate the material was transported a significant distance by water before lithification.
Field identification & locations
Identify in the field by the 'concrete-like' appearance with large, rounded pebbles embedded in a finer, rusty-colored cement. Often found in ancient riverbeds or mountain foothills. It feels heavier than standard sandstone due to iron content.
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