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Quartz breaks with a conchoidal fracture rather than cleaving because its structure is a

  • A.framework of tetrahedra bonded equally in all directions
  • B.sheet structure with weak bonding between layers
  • C.chain structure with weak bonding between chains
  • D.structure of isolated tetrahedra held together by cations alone

Answer: A

Correct answer: framework of tetrahedra bonded equally in all directions

Cleavage requires planes of weaker bonding, and in quartz every oxygen is shared between two tetrahedra so the silicon-oxygen bonds run in all directions with equal strength. There is no weak plane for a break to follow, so a fracture takes the shell-like conchoidal form instead - the same reason flint and glass break as they do.

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