Final answer:
Silicate groups can be classified based on how many oxygen atoms are shared by each silicon-oxygen tetrahedron with a neighboring tetrahedron. The classifications include isolated or nesosilicates, ring silicates, sheet silicates, and framework silicates.
Step-by-step explanation:
Silicate groups can be classified based on how many oxygen atoms are shared by each silicon-oxygen tetrahedron with a neighboring silicon-oxygen tetrahedron. The different classifications are:
- Isolated or Nesosilicates: Each silicon-oxygen tetrahedron is independent and not connected to any other tetrahedron. Examples include garnet and olivine.
- Ring Silicates: Silicon-oxygen tetrahedra are linked together in rings, with oxygen atoms being shared between the tetrahedra. Beryl and tourmaline are examples of ring silicates.
- Sheet Silicates: The tetrahedra form sheets or layers, with oxygen atoms being shared between adjacent tetrahedra. Micas and clays belong to the sheet silicates group.
- Framework Silicates: The tetrahedra are connected in a three-dimensional network, with all oxygen atoms being shared between neighboring tetrahedra. Quartz and feldspar are examples of framework silicates.