Schists are strongly foliated, and look like a stack of paper. Some of the best places to see schist are among the spires at Gunnison Point or Kneeling Camel View. The Great Pillars, seen here, are among the largest examples of schist in the canyon. The main difference between schist and gneiss is the thickness of their internal layers, known as lamellae (pronounced "la MEL lee"). Gneiss has thick lamellae and schist have very thin, fine layers.
There are two kinds of schists found in the canyon, either a mica-rich schist, that has a lot of biotite and muscovite mica, or a schist rich in hornblende, a type of mineral called amphibole. A zone of schist crosses the canyon between Gunnison Point and Pulpit Rock Overlook. Rare minerals such as garnets, sillimanite, staurolite or andalusite can be common in places.
Plagioclase is a whole family of minerals that make up what is called a solid solution series. That means there are two ends of a scale with "pure" members at each end, with blended members of the family in between. "Pure" yellow is at one end and "pure" green is at the other with many shades between them. If you mix a few other elements in you find white, reddish-gray or black colors as well, making this hard mineral an important part of most metamorphic (and igneous) rocks, and is one of the most common rock-forming minerals you will find.
- The most common variety in Black Canyon is Albite. It is rich in sodium.
- Albite is used as a gemstone, also known as "moonstone," but gem quality finds are rare in the United States.
- Is used commercially in the ceramics industry as well.
- The name albite comes from the Latin "albus" or white.
- Albite is found in schists, gneisses and quartz monzonite.