| Mineral class: | Tectosilicate |
| Composition: | Feldspars are aluminum silicates with varying proportions of potassium (K), sodium (Na) or calcium (Ca). There are two broad categories of feldspars:
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| Hardness: | 6 |
| Color: | White, pink, grey, green |
| Streak: | White |
| Cleavage: | 2 directions at 90 degree angles. Orthoclase cleavage surfaces are striated; plagioclase surfaces are not striated. |
| Environment: | Feldspars account for 60 percent of the continental crust, but are virtually absent from ocean beds. Common in stream gravel. |
| Comments: | Scratched by quartz but not by knife.
At the surface of the Earth, particularly in warm, humid environments, feldspars weather (by hydrolysis) to form Kaolin, a fine-grained, white clay which is the main ingredient of Kaopectate. The large positive ions of the feldspars (K+, Na+, Ca2+) are replaced by hydrogen ions (H+) from water, yielding Al2Si2O5(OH)4. Kaolin is found as bedded masses in soils and sedimentary rocks. It is soft (Mohs 2.5 or less) and has an earthy odor, particularly if moistened. |