
sedimentary
Conglomerate
Conglomerate (clastic sedimentary rock)
Composed of rounded gravel-sized clasts (>2mm) held together by a matrix of sand/silt and mineral cement; Hardness: variable (3-7 Mohs) based on clasts; Color: multi-colored/mottled; Luster: earthy/dull; Structure: clastic/fragmental.
- Hardness
- variable (3-7 Mohs) based on clasts
- Color
- multi-colored/mottled
- Luster
- earthy/dull
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Physical properties
Composed of rounded gravel-sized clasts (>2mm) held together by a matrix of sand/silt and mineral cement; Hardness: variable (3-7 Mohs) based on clasts; Color: multi-colored/mottled; Luster: earthy/dull; Structure: clastic/fragmental.
Formation & geological history
Formed in high-energy environments like riverbeds, alluvial fans, or beaches where water current is strong enough to transport and round large stones. Over millions of years, these deposits are buried and lithified through pressure and mineral precipitation.
Uses & applications
Used primarily in the construction industry as coarse aggregate for concrete and roadbeds; sometimes used as architectural stone or for interior decoration if it contains high-contrast colorful clasts.
Geological facts
Conglomerates are often referred to as 'puddingstone' because they resemble a fruit pudding; they indicate a specific paleoenvironment where ancient high-velocity water once flowed, helping geologists map ancient river systems.
Field identification & locations
Identify in the field by looking for 'stones within a stone'—specifically rounded pebbles or cobbles embedded in a finer-grained matrix. Found globally in ancient sedimentary basins, river valleys, and mountain foothills.
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