BH250-4

Title

BH250-4

Subject

Kyanite Quarzite

Description

Major Minerals: quartz, kyanite, muscovite, calcite, olivine
Minor Minerals: serpentine, rutile
Optics: bladed, long prismatic, perfect cleavages, cross parting with 85 degrees

BH250-4 is a kyanite quartzite, a high-grade metamorphic rock composed predominantly of quartz and bladed kyanite, with minor amounts of muscovite. The presence of kyanite indicates metamorphism under moderate to high pressure and elevated temperatures, consistent with the kyanite stability field and typical of Barrovian metamorphism. This suggests the rock was buried to mid-crustal depths.

The kyanite crystals exhibit a distinct bladed habit, often aligned with the rock’s foliation. The protolith is confidently interpreted as pelitic, originally an aluminum-rich sedimentary rock such as a mudstone or shale, which underwent recrystallization and mineralogical transformation during regional metamorphism.

Coverage

Location: Ogilby, California, USA

Creator

Bereket Haileab

Source

From the rock collection of Bereket Haileab. Sample 4. Housed at Carleton College in Minnesota.

Type

Thin section and hand sample

Relation


View on ArcGIS Online here













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Collection

Citation

Bereket Haileab, “BH250-4,” BH250 Mineralogy Teaching Collection, accessed April 25, 2026, https://bereket-haileab.geology.sites.carleton.edu/items/show/4.

Output Formats