orthoclase
- noun
- /ˈɔrθəˌkleɪs/
- Specialized
- Geologists identify orthoclase by its distinct monoclinic crystal structure and light color.
Examples
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In many igneous rocks, orthoclase occurs alongside quartz and mica as a key mineral.
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The mineral orthoclase is easily identified by its light color and monoclinic crystal structure.
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The range is as follows: talc 1; gypsum 2; calcite 3; fluorite 4; apatite 5; orthoclase 6; quartz 7; topaz 8; corundum 9; and diamond 10.
Academic text (1993)
How Hard
Surface Forms
Etymology
The word orthoclase comes from Greek words orthos 'straight' and klasis 'breaking', so its name means 'straight break'. That's a helpful image because this feldspar often splits along straight planes, which is why geologists call the mineral orthoclase.