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Feldspar (Orthoclase)

The Rock-Forming Minerals

Feldspars are a group of closely related silicate minerals that together make up the majority of the Earth's crust. This is orthoclase. (more below)
Top mineral in the whole crust
Photo (c) 2007 Andrew Alden, licensed to About.com (fair use policy)
The compositions of the various feldspars all blend together smoothly. If the feldspars can be considered a single, variable mineral, then feldspar is the most common mineral on Earth. All feldspars have a hardness of 6 on the Mohs scale, so any glassy mineral that's slightly softer than quartz is very likely to be a feldspar. A thorough knowledge of the feldspars is what separates geologists from the rest of us.

Learn more about the feldspar minerals.

See the other feldspar minerals in the Feldspars Gallery.

Other Primary Minerals
Other Metamorphic Minerals
Other Hydrothermal Vein Minerals

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