Construct · 2 fields · 2 citations
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In mineralogy, parting is the tendency of a mineral to break along planes of weakness that are not cleavage, such as twin composition planes or exsolution lamellae, and so is not a property of every specimen of a species. Wang (2025), in the Manual of Mineral Material Science, treats cleavage, fracture, and parting together as the ways a mineral breaks, distinguishing parting from true cleavage. Here parting is a mode of mineral breakage, not the split line of a mould.[1]
In casting and moulding, the parting line (or parting surface) is where the two halves of a mould meet and separate so the finished part can be removed without undercuts trapping it. Majhi, Gupta, and Janardan (1999), in Computational Geometry, give an algorithm for computing a flattest, undercut-free parting line for mould design, treating parting as a geometric constraint on manufacturability. Here parting is the split plane of a mould, not the breakage habit of a mineral.[2]
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