BH250-56
Title
BH250-56
Subject
Granitic pegmatite (Biotite and hornblende)
Description
Major Minerals: hornblende, biotite, plagioclase
Minor Minerals: calcite (secondary), very large sphene (titanite), tiny isotropic mineral
Click here for a high resolution scan
Minor Minerals: calcite (secondary), very large sphene (titanite), tiny isotropic mineral
Click here for a high resolution scan
BH250-56 exhibits a pegmatitic texture with large hornblende and biotite crystals. It is a coarse-grained igneous rock, typically granitic in composition, formed from late-stage crystallization of magma.
Mineralogy:
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Biotite and hornblende: Common in granitic pegmatites, especially in hydrous compositions; large crystals are typical.
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Sphene (titanite): Large crystals present.
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Plagioclase feldspar: Anhedral crystals observed.
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Calcite: Likely formed from late-stage hydrothermal activity or interaction with carbonate wall rocks, rather than primary igneous crystallization.
Creator
Bereket Haileab
Source
From the rock collection of Bereket Haileab. Sample BH250-56. Housed at Carleton College in Minnesota.
Type
Thin section and hand sample
Relation
Collection
Citation
Bereket Haileab, “BH250-56,” BH250 Mineralogy Teaching Collection, accessed April 25, 2026, https://bereket-haileab.geology.sites.carleton.edu/items/show/65.
