Where is Clay found?
Hydrous phyllosilicates
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Open the appClay occurs in specific geological environments. Knowing where to look, and in what kind of rock, is the difference between going home empty-handed and finding a great specimen.
Where to find Clay
Mississippi River Delta, USA
Extensive deposits of Holocene clays and silts due to fluvial deposition.
Amazon Basin, South America
Vast areas covered by clay-rich sediments from weathering and fluvial transport.
Weald Basin, UK
Significant Jurassic and Cretaceous clay formations (e.g., Weald Clay, Gault Clay).
Kaolin deposits in Georgia, USA
World-renowned deposits of high-purity kaolinite formed from the weathering of feldspar-rich rocks.
Bentonite deposits in Wyoming, USA
Large deposits of smectite-rich clay (bentonite) formed from the alteration of volcanic ash.
Collecting tips
- Look for fine-grained sediments. Clay is typically found in areas with low-energy depositional environments, such as river floodplains, lakebeds, and marine environments. Look for fine-grained, soft, and often layered sediments.
- Check for plasticity. A key characteristic of clay is its plasticity when wet. Take a small sample, moisten it, and try to roll it into a 'worm' or shape it. If it holds its shape without crumbling, it likely contains a significant amount of clay.
- Observe color and texture. While variable, many clays have a dull, earthy luster and a smooth, non-gritty feel when dry. Red, brown, gray, and white are common colors. A gritty feel indicates the presence of silt or sand.
- Examine geological maps. Geological maps often delineate areas with clay-rich formations (e.g., shale, mudstone, claystone units), which can guide your search.
Quick Check
- Color:
- Variable (white, gray, black, red, brown, yellow, green)
- Luster:
- Dull to earthy (dry), waxy/greasy (wet)
- Streak:
- White to light-colored, depending on impurities
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