. Elements of geology : a text-book for colleges and for the general reader. Geology. Fig. 753.—Right lower jaw of Diplocynodon victor (after MarstO. outside view. Twice natural size: a, canine; b, condyle; c, coronoid process; d, angle. line advanced westward on the land. During the Jura-Trias the shore-line to the -north was still beyond what it is now, for no Atlantic border deposit is visible; and along the Middle and Southern States. Fig. 754.—Left lower jaw of Ctenacodon serratus (after Marsh), inner view. Four times natural size. it was certainly beyond the bounding-line of Tertiary and
. Elements of geology : a text-book for colleges and for the general reader. Geology. Fig. 753.—Right lower jaw of Diplocynodon victor (after MarstO. outside view. Twice natural size: a, canine; b, condyle; c, coronoid process; d, angle. line advanced westward on the land. During the Jura-Trias the shore-line to the -north was still beyond what it is now, for no Atlantic border deposit is visible; and along the Middle and Southern States. Fig. 754.—Left lower jaw of Ctenacodon serratus (after Marsh), inner view. Four times natural size. it was certainly beyond the bounding-line of Tertiary and Cretaceous (see map, p. 291), for all the Atlantic deposits of this age have been covered by subsequent strata; and yet probably not much beyond, for some of these Jura-Trias patches seem to have been in tidal connection with the Atlantic Ocean. It is probable, therefore, that the shore-line was a little beyond the present New England shore-line, and a little. 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 LeConte, Joseph, 1823-1901. New York : D. Appleton and Co.
Size: 2703px × 925px
Photo credit: © Paul Fearn / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1800, bookdecade1890, booksubjectgeology, bookyear1892
