Sometimes it's hard to tell whether a well-formed mineral crystal is displaying crystal habit (i.e., it grew that way), or whether it's a broken piece of a mineral with cleavage (i.e., it broke into a particular shape because of a specific pattern of weaknesses in its atomic structure).
The image shows two samples for each of two minerals. Three of the samples are pieces broken from a bigger crystal. Can you figure out which of the larger samples (A or B) is also a broken piece?