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Gneiss with pencil structure

This gneiss was caught in a deep, hot part of a fault zone between rocks moving in opposite directions. The movement stretched the mineral grains into long ribbons. You can see the grains that form the ribbons by viewing the end of the rock.

Group: Metamorphic
Image Number: 98-27011
Catalog Number: 115158
Locality: Kutna Hora , Czech Republic

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Smithsonian National Museum of Natural History Geology, Gems, and Minerals Subject Guide Credits