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Richard Willis

Soil (dirt, hubris, mud, etc.; in contrast to rock and sand) more or less rich in clay particles. Clay earths — including the feldspars, feldspathoids and feldspathics — account for well over 60% of the Earth’s crust, ranging from the very “pure” deposits of kaolin to the very “impure” deposits of marl. see soils

Out Bound Links

By Tony Hansen

XML for Import into INSIGHT

<?xml version="1.0" encoding="UTF-8"?> <material name="CLAY EARTH" descrip="" searchkey="" loi="0.00" casnumber="70694-09-6"> </material>

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