. Elements of geology. Geology. Orapliic granite. Fig. 108. Section parallel to the laminae. Fig. 109. Section transverse to the laminse. appear to have been first formed, leaving between them the space now occupied by the darker coloured quartz. This mineral, when a section is made at right angles to the alternate plates of. 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 Lyell, Charles, Sir, 1797-1875; Gibbes, Lewis Reeve
. Elements of geology. Geology. Orapliic granite. Fig. 108. Section parallel to the laminae. Fig. 109. Section transverse to the laminse. appear to have been first formed, leaving between them the space now occupied by the darker coloured quartz. This mineral, when a section is made at right angles to the alternate plates of. 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 Lyell, Charles, Sir, 1797-1875; Gibbes, Lewis Reeve, 1810-1894, former owner. DSI; Merrill, George P. (George Perkins), 1854-1929, former owner. DSI. Philadelphia : James Kay, Jun. and Brother ; Pittsburgh : C. H. Kay & Co.
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Keywords: ., bookauthorlyellcharlessir17, bookcentury1800, booksubjectgeology
