
sedimentary
Conglomerate
Conglomerative Sedimentary Rock
Hardness varies by clast type (usually 6-7 if quartz-rich); Color: Grey, brown, or multi-colored depending on clasts; Luster: Dull/Earthy matrix with variable clast luster; Crystal structure: Non-crystalline/Clastic; Specific Gravity: 2.6-2.9.
- Color
- Grey, brown, or multi-colored depending on clasts
- Luster
- Dull/Earthy matrix with variable clast luster
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Physical properties
Hardness varies by clast type (usually 6-7 if quartz-rich); Color: Grey, brown, or multi-colored depending on clasts; Luster: Dull/Earthy matrix with variable clast luster; Crystal structure: Non-crystalline/Clastic; Specific Gravity: 2.6-2.9.
Formation & geological history
Formed through the lithification of rounded gravel and boulders (clasts) larger than 2mm, usually in high-energy environments like fast-flowing rivers, alluvial fans, or glacial meltwater deposits.
Uses & applications
Primarily used as a coarse aggregate in the construction industry for concrete and road beds. Some aesthetically pleasing varieties (Puddingstone) are used for ornamental carvings or as decorative garden stones.
Geological facts
Also known as 'Puddingstone' because the rounded rocks in the matrix resemble raisins in a pudding. It is often used by geologists to determine the direction and energy of ancient river flows.
Field identification & locations
Identify in the field by looking for 'rounded' pebbles or rocks cemented naturally within a finer-grained matrix (sand or silt). Commonly found in ancient riverbeds or mountain bases globally. Collectors look for unique colors or fossil inclusions.
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