. The geological history of plants. Paleobotany; 1888. THE BRIAN OR DEVONIAN FORESTS. 79 folk Island pine, than that of the modern yews. These trees are chiefly known to us by their mineralised trunks, which are often found like drift-wood on modern sand- banks embedded in the Erian sandstones or limestones. It often shows its structure in the most perfect man- ner in specimens penetrated by calcite or silica, or by pyrite, and in which the original woody matter has. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - col
. The geological history of plants. Paleobotany; 1888. THE BRIAN OR DEVONIAN FORESTS. 79 folk Island pine, than that of the modern yews. These trees are chiefly known to us by their mineralised trunks, which are often found like drift-wood on modern sand- banks embedded in the Erian sandstones or limestones. It often shows its structure in the most perfect man- ner in specimens penetrated by calcite or silica, or by pyrite, and in which the original woody matter has. 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 Dawson, John William, Sir, 1820-1899. New York, D. Appleton and Company
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Keywords: ., bookauthordawsonjo, bookcentury1800, bookdecade1880, bookyear1888
