Ball clays are
kaolinitic sedimentary clays, that commonly consist of 20-80%
kaolinite, 10-25%
mica, 6-65%
quartz. Localized
seam in the same deposit have variations in composition, including the quantity of the major
minerals, accessory minerals and
carbonaceous materials such as
lignite. They are fine-grained and plastic in nature.
Ball clays are relatively scarce deposits due to the combination of geological factors needed for their formation and preservation. They are
mine in parts of the Eastern United States and from three sitesThe
Bovey Basin in South Devon, the Petrockstowe Basin in North Devon and the Wareham Basin in South Dorset. in
Devon and
Dorset in South West
England. They are commonly used in the construction of many ceramic articles, where their primary role is to either to impart plasticity or to aid stability during the shaping processes.
History
The name "ball clay" is believed to derive from the time when the clay was mined by hand. It was cut into 15 to 17-kilogram cubes and during transport the corners of the cubes became rounded off leaving "balls".
The
ceramic use of ball clays in
Britain dates back to at least the
Roman era. More recent trade began when a clay was needed to construct
tobacco pipes in the 16th and 17th century. In 1771 ...
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