Cordierite-biotite-gneiss
Wall Art and Photo Gifts from Mary Evans Picture Library
Cordierite-biotite-gneiss
Geological specimen collected by Scotts British Antarctic Expedition 1910-1913, also known as the Terra Nova expedition. It had a broad scientific programme and collected thousands of geological and zoological specimens. The banding of a gneiss is caused by minerals growing under huge pressures deep in the Earths crust
Media ID 8623392
© Mary Evans / Natural History Museum
Cordierite Cyclosilicate Iolite Metamorphic Mica Mineral Phyllosilicate Scott Scott Expedition Silicate Silicate Mineral Sunstone Terra Nova Terra Nova Expedition
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