. An old chapter of the geological record with a new interpretation, or, Rock-metamorphism (especially the methylosed kind) and its resultant imitations of organisms [microform] : with an introduction giving an annotated history of the controversy on the so-called " Eozoon canadense", and an appendix. Paleontology; Metamorphism (Geology); Paléontologie; Métamorphisme (Géologie). Fig. 3. 2 mono- 2\l often nodified jf their s of the nary of all the whose 24,°30' yields leen that tremely ;ion of ccidedly not be s render itudinal ler sueh vertical ae, pp. 90, iridote, as rtical axis. Fig
. An old chapter of the geological record with a new interpretation, or, Rock-metamorphism (especially the methylosed kind) and its resultant imitations of organisms [microform] : with an introduction giving an annotated history of the controversy on the so-called " Eozoon canadense", and an appendix. Paleontology; Metamorphism (Geology); Paléontologie; Métamorphisme (Géologie). Fig. 3. 2 mono- 2\l often nodified jf their s of the nary of all the whose 24,°30' yields leen that tremely ;ion of ccidedly not be s render itudinal ler sueh vertical ae, pp. 90, iridote, as rtical axis. Fig. 1. Diagrammatic transverse sections of a prismatic crystal of peridote. Obtuse angles 04" ; acute angles 80°. The outer dotted lines represent the form of its primary ; the inner continuous lines angular measurements of its simplest modiiication j the broken lines its rectangular cleavage. The prism is upright. Fig. 2. Diagrammatic transverse sections of a prismatic crystal of augito. Obtuse angles 92° 55'; acute angles 87° 5'. Fig. 3. Diagrammatic transverse sections of a prismatic crystal of hornblende. Obtuse angles 124° 30'; acute angles 55° 30'. The augite and hornblende prisms (Figs. 2 & 3) are inclined (mono- clinic). Their inclination to be assumed as from bottom to top of the page. When their angles are truncated down to the white lines, the resulting section is that of the usual prism. The outer dotted lines represent the form of the primary; the con- tinuous lines a secondary form,or that of the cleavage-solid; the broken lines the cleavage, which is 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 King, William, 1809-1886; Rowney, T. H. (Thomas Henry), 1817-1894. London : J. Van Voorst
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Keywords: ., bookcentury1800, bookdecade1880, booksubjectpaleontology, bookyea
