About
Crystal Forms & Aggregates
Other ID Marks
Striking Features
Environment
Varieties
✓ generally accepted · ✗ less commonly used
- Hydroxylclinohumite— Form of Clinohumite lacking fluorine it its chemical structure, containing only hydroxyl at the end of its chemical formula. Hydroxylclinohumite is also deficient in iron, which is usually present in Clinohumite. Hydroxylclinohumite was classified in 1998 and is considered an individual mineral by the IMA.
Uses
Noteworthy Localities
The best formation of Clinohumite, in the form of outstanding orange crystals with good transparency, is from Kukh-i-Lal, Pamir Mts, Tajikistan. Sharp crystals and grains of Hydroxylclinohumite of excellent quality come from Sar-e-Sang, Kokcha Valley, Badakhshan Province, Afghanistan. Clinohumite associated with contrasting dark Spinel is found in the Hunza Valley, Gilgit, Pakistan.
Gemmy Clinohumite microcrystals have been found at Monte Somma, Vesuvius, Italy; and orange crystal grains from the Málaga region, Andalusia, Spain. In the U.S., large crystal clusters, almost always associated with Spinel, were found at the Rudy farm locality, Edenville, Orange Co., New York. In Canada, large Clinohumite crystals, including rare twinned crystals, have come from a one-time find at Essonville Line, near Wilberforce, Haliburton Co.
Common Mineral Associations
Photos
Crystal forms
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