. Bulletin of the Department of Geology. Geology. 1917] Stock: Structure of the Pes in Mylodon harlawi 26! > detail the astragalus and navicular of M. harlani from Rock Creek, Texas, and they need not be considered further at this time. In M. robustus the cuboid is apparently longer anteroposterior^ than wide, while in M. harlani the reverse is true, the cuboid being wider transversely than long. The outer (lower) surface of the cuboid. Fig. 1. Mylodon harlani Owen. Left pes, outer view, X V±- Unguals slightly foreshortened. Bancho La Brea beds. Fig. 2. Mylodon robustus Owen. Left pes, X %.

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. Bulletin of the Department of Geology. Geology. 1917] Stock: Structure of the Pes in Mylodon harlawi 26! > detail the astragalus and navicular of M. harlani from Rock Creek, Texas, and they need not be considered further at this time. In M. robustus the cuboid is apparently longer anteroposterior^ than wide, while in M. harlani the reverse is true, the cuboid being wider transversely than long. The outer (lower) surface of the cuboid. Fig. 1. Mylodon harlani Owen. Left pes, outer view, X V±- Unguals slightly foreshortened. Bancho La Brea beds. Fig. 2. Mylodon robustus Owen. Left pes, X %. After Owen. Pampean Pleistocene beds, South America. articulates with a greater portion of metatarsal 5 and with a corre- sponding lesser portion of metatarsal 4 than in M. robustus. In the latter species there is a much smaller articulation of the posterior face with the calcaneum. This difference may also be more apparent than 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 University of California, Berkeley. Dept. of Geology. Berkeley : The University Press

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Keywords: ., bookcentury1900, bookdecade1900, booksubjectgeology, bookyear1902