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Richard Willis

Geophysically hardened clay. Claystone is normally classified by geologists as a sedimentary rock composed primarily of clay-sized particles of less than 1/256 millimeter in diameter and which is not laminated or easily split into thin layers, such rocks that show cleavage roughly parallel to the bedding plane often are classed as “clay shales”. Massive and blocky claystones are sometimes called mudstones, but some geologists class as mudstones only the partly hardened muds that slake when wetted, reserving the term 'claystone' for fully hardened matter.

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By Tony Hansen

XML for Import into INSIGHT

<?xml version="1.0" encoding="UTF-8"?> <material name="CLAYSTONE" descrip="" searchkey="" loi="0.00" casnumber=""> </material>

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