. Acadian geology : the geological structure, organic remains, and mineral resources of Nova Scotia, New Brunswick, and Prince Edward Island. Geology -- New Brunswick; Geology -- Nova Scotia; Geology -- Prince Edward Island; Paleontology -- New Brunswick; Paleontology -- Nova Scotia; Paleontology -- Prince Edward Island. 194 THE CARBONIFEROUS SYSTEM. have been broken off without any decrease of their diameter. In one place twelve stems were counted in eight feet measured along the face of the cliff. From the base of the cliff to low-water mark, they could everywhere be seen abundantly along th
. Acadian geology : the geological structure, organic remains, and mineral resources of Nova Scotia, New Brunswick, and Prince Edward Island. Geology -- New Brunswick; Geology -- Nova Scotia; Geology -- Prince Edward Island; Paleontology -- New Brunswick; Paleontology -- Nova Scotia; Paleontology -- Prince Edward Island. 194 THE CARBONIFEROUS SYSTEM. have been broken off without any decrease of their diameter. In one place twelve stems were counted in eight feet measured along the face of the cliff. From the base of the cliff to low-water mark, they could everywhere be seen abundantly along the continuation of the ledge of sandstone. This bed and others of similar character at the Joggins,. have given us much information respecting the nature and mode of growth of these plants, which I may pause here to notice in detail. The Calamites were tall cylindrical stems, with a hard outer bark, and were either hollow or filled with cellular matter. The stems were regularly marked with longitudinal strise or furrows and cross joints, sometimes showing the marks of the attachment of the leaves, which were verticillate, or in whorls around the stem, and long and needle-like (Figs. 37 and 38). The general habit of growth thus Fig. 38.—Leaves of Calamites [C. Cistii) Fig. 37. -Erect Calamites {C. Voltzii), imtli 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. London : Macmillan
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