
sedimentary
Conglomerate
Conglomerate (Sedimentary Clastic Rock)
Hardness: variable (grain 6-7, matrix 3-5); Color: tan, buff, and grey; Luster: dull/earthy; Texture: coarse-grained clastic; Structure: rounded clasts (pebbles) embedded in a fine-grained matrix of silt or sand.
- Hardness
- variable (grain 6-7, matrix 3-5)
- Color
- tan, buff, and grey
- Luster
- dull/earthy
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Physical properties
Hardness: variable (grain 6-7, matrix 3-5); Color: tan, buff, and grey; Luster: dull/earthy; Texture: coarse-grained clastic; Structure: rounded clasts (pebbles) embedded in a fine-grained matrix of silt or sand.
Formation & geological history
Forms through the lithification of rounded gravel and pebbles. Typically deposited in high-energy environments like fast-flowing rivers, alluvial fans, or beaches where water movement is strong enough to round the fragments.
Uses & applications
Used as a heavy-duty aggregate in the construction industry for roads and concrete. Occasional use as decorative stone or dimension stone if it is well-cemented and takes a polish.
Geological facts
Conglomerates are essentially 'natural concrete.' They are important to geologists because they indicate a high-energy depositional environment and can help map the history of ancient river systems.
Field identification & locations
Identify by looking for rounded, pebble-sized rocks 'glued' together by a finer material. Found globally in ancient riverbeds, coastal cliffs, and sedimentary basins. Collectors look for unique inclusions or colorful clasts.
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