pikkade, valandi või valuploki keskosani ulatuvate läbipõimunud sammaskristallide tsooni moodustumine; on iseloomulik tugevalt ülekuumutatud metalli, eelkõge mitteraudmetallide, tardumisel (kristalliseerumisel)
typical feature in ingot macrostructure; formed by dendrite growing in nearly the same direction
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