. Bulletin of the Geological Society of America. Geology. 456 OSBORN AND REEDS PREHISTORY OF MAN IN EUROPE level of the waters of the Seine—and overlaid by a series of tufa layers of a combined thickness of 15 meters, which represent not only tufa inclines (tuf de pente), but tufa of the valley bottom, local facies of the Tyrrhenian alluvium of the valley of the Seine. In the middle portion. Figure 8.—Excavations on the "high Terrace" [II] at Saint Aeheul This is known as the ancienne carriere Dupont and more recently as the carriere Battel, showing eight geologic layers, from the Up
. Bulletin of the Geological Society of America. Geology. 456 OSBORN AND REEDS PREHISTORY OF MAN IN EUROPE level of the waters of the Seine—and overlaid by a series of tufa layers of a combined thickness of 15 meters, which represent not only tufa inclines (tuf de pente), but tufa of the valley bottom, local facies of the Tyrrhenian alluvium of the valley of the Seine. In the middle portion. Figure 8.—Excavations on the "high Terrace" [II] at Saint Aeheul This is known as the ancienne carriere Dupont and more recently as the carriere Battel, showing eight geologic layers, from the Upper Paleolithic deposits of brick-earth at the top (9) down to the sub-Chellean yellow gravels (2) overlying the chalk (1) at the bottom. of the tufa there was discovered in 1893-1894 early Acheulean imple- ments, somewhat more recent than the late Ohellean coups de poing of Chelles. The section of La Celle-sous-Moret (compare Osborn, , pages 118, 166) is as follows:. 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 Geological Society of America. [New York : The Society]
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Keywords: ., bookcentury1800, bookdecade1890, booksubjectgeology, bookyear1890
