
sedimentary
Brown shale or mudstone fragment
Likely fissile claystone/shale, composed mainly of compacted clay minerals, quartz, and minor iron oxides
AI-generated identification · may be incorrectThin, layered, dull earthy-brown fragment with very fine grain and uneven/fissile breakage; estimated Mohs hardness 2–3, nonmetallic luster, negligible visible crystals, and low specific gravity around 2.2–2.7. Exact identification is limited by the photograph.
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Physical properties
Thin, layered, dull earthy-brown fragment with very fine grain and uneven/fissile breakage; estimated Mohs hardness 2–3, nonmetallic luster, negligible visible crystals, and low specific gravity around 2.2–2.7. Exact identification is limited by the photograph.
Formation & geological history
Formed when clay- and silt-sized sediment accumulated in quiet water, was compacted, and cemented during burial; age could range from very young sediment to hundreds of millions of years depending on source locality.
Uses & applications
Common shale is used for brick, cement, roofing products, and aggregate, while attractive slabs may be collected; this small fragment has essentially no commercial value.
Geological facts
Its thin layering and earthy color are typical of fine-grained sedimentary rock, though weathered slate or a clay-rich mudstone can look similar.
Field identification & locations
Look for persistent bedding, a dull surface, very fine texture, and splitting along layers; it may scratch easily with a knife and usually does not fizz with dilute hydrochloric acid. Common worldwide in former lake, floodplain, and marine basins.
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