It involves sliding of blocks of crystal over one other
along definite crystallographic planes, called slip planes.
In physical words it is analogous to a deck of cards
when it is pushed from one end.
Slip occurs when shear stress applied exceeds a critical
value.
During slip each atom usually moves same integral number
of atomic distances along the slip plane producing a step, but the orientation
of the crystal remains the same.
Steps observable under microscope as straight lines are
called slip lines.
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