6 March 2010
Glittery!
Posted by Callan Bentley
The Manhattan Schist with its well-developed alignment of muscovite mica:
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About Callan
Callan Bentley is Associate Professor of Geology at Piedmont Virginia Community College in Charlottesville, Virginia. He is a Fellow of the Geological Society of America. For his work on this blog, the National Association of Geoscience Teachers recognized him with the James Shea Award. He has also won the Outstanding Faculty Award from the State Council on Higher Education in Virginia, and the Biggs Award for Excellence in Geoscience Teaching from the Geoscience Education Division of the Geological Society of America. In previous years, Callan served as a contributing editor at EARTH magazine, President of the Geological Society of Washington and President the Geo2YC division of NAGT.
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Callan,
Nice shots but hey, you’re in NYC; show us some cool building stone. Rumor has it that there is some there.
Just a thought.
David
Oh my! I can’t believe you said “glittery”! You should know better than to say that! Manhattan schist isn’t glittery but has that appearance owing to muscovite’s vitreous luster.