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The formula for the reorder point without safety stock is:
Cleavage
In geology, this refers to the tendency of crystalline materials to split along definite crystalline boundaries, often parallel to planes of weakness in their structure.
Cleavage Planes
Natural planes of weakness along which minerals preferentially break, reflecting their crystallographic structure.
Asbestos
A general name for the fibrous varieties of a number of silicate minerals whose common characteristic is that they tend to form fibers.
Silicate Structure
The arrangement of silicon and oxygen atoms that forms the backbone of most minerals in the Earth's crust.
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