Concept:
Feldspar is the most abundant group of minerals in the earth's crust and acts as the primary flux (melting agent) in high-fire ceramic glazes and clay bodies.
Step 1:
In ceramics, feldspars are used to introduce alkaline earth metals that lower the melting point of silica, allowing glass to form at achievable kiln temperatures.
Step 2:
There are three primary types of feldspar categorized by their dominant alkali element:
• Potash Feldspar (Orthoclase): Rich in Potassium ($K_{2}O$). Melts smoothly and is highly favored in stoneware glazes.
• Soda Feldspar (Albite): Rich in Sodium ($Na_{2}O$). Melts at a slightly lower temperature and is often used in casting slips and brighter glazes.
• Lime Feldspar (Anorthite): Rich in Calcium ($CaO$). While less common as a standalone pure ingredient than the other two, it completes the standard feldspar triad.
Step 3:
While studio potters most frequently toggle between Potash and Soda feldspars, ceramic science and industrial preparation formally recognize the three fundamental types (Potash, Soda, and Lime) as the building blocks for bodies and glazes.
Step 4:
Because there are three main mineralogical categories utilized in ceramic formulation, the correct answer is 3 types.
\[
\boxed{\text{(2) 3 types}}
\]