. Bulletin of the Geological Society of America. Geology. FiGUEE 1.—WyOMINGITE OF ZiRKEL MeSA The round white minerals are leneite; the rods are diopside; the large dark ones are phlo- gophite. Actual field, 1 Figure 2.—Orendite from Fifteen-mile Spring, Zirkel Mesa Round white minerals are leucite; the white rods sanidine; the small dark rods diopsidt the large dark mineral phlogophite. Actual field, 1 millimeter PHOTOMICROGRAPHS OF WYOMINGITE AND ORENDITE. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability -
. Bulletin of the Geological Society of America. Geology. FiGUEE 1.—WyOMINGITE OF ZiRKEL MeSA The round white minerals are leneite; the rods are diopside; the large dark ones are phlo- gophite. Actual field, 1 Figure 2.—Orendite from Fifteen-mile Spring, Zirkel Mesa Round white minerals are leucite; the white rods sanidine; the small dark rods diopsidt the large dark mineral phlogophite. Actual field, 1 millimeter PHOTOMICROGRAPHS OF WYOMINGITE AND ORENDITE. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Geological Society of America. [New York : The Society]
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Keywords: ., bookcentury1800, bookdecade1890, booksubjectgeology, bookyear1890
